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58th British Sedimentological Research Group Annual General Meeting Egham Surrey UK 13- 17 December 2019 (AGM: 14 th and 15 th December) 3rd Circular @BSRG19 58 th BSRG Annual General Meeting [email protected]

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Page 1: 58th British SedimentologicalResearch Group Annual General ... Circular_58BSRG.pdf · •Ross Ferguson, Spatial and temporal ... •P3.HaryaNugraha, Lateral variation of submarine

58th British Sedimentological Research Group Annual General Meeting

Egham Surrey UK 13- 17 December 2019(AGM: 14th and 15th December)

3rd Circular

@BSRG19

58th BSRG Annual General Meeting

[email protected]

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58th British Sedimentological Research Group Annual General Meeting

1. INTRODUCTION

When: 13th - 17th December 2019Where: Royal Holloway, University of London, TW20 0EX Egham, UK

Egham Surrey UK 13th – 17th December 2019(AGM: 14th and 15th)

BSRG @brit_seds

You are cordially invited to participate next December for the 58th BSRG Annual General Meeting. We aimto provide a scientifically stimulating and socially enjoyable forum to meet and discuss results and ideasrelated to Sedimentology. The meeting should be of interest to both academic and industry participants.Students and early career researchers are especially welcome, and an attractive timetable of workshops,field trips, and outreach activities has been planned for them.

.

We look forward to welcoming you to Royal Holloway, University of London!

The British Sedimentological Research Group (BSRG) Annual General Meeting (AGM) is the mostimportant event in the BSRG calendar and is the focus of much of BSRG's activities. The meeting features anextensive academic and social program which includes pre-conference workshops, talk and poster sessions,and a conference dinner. The meeting provides a chance to meet other researchers, your peers, industrycontacts and perhaps even a future collaborator or employer. The talk and poster sessions provide anexcellent opportunity to advertise your research to a captive audience and catch up on the UKsedimentology research scene.

https://www.bsrg.org.uk-

The BSRG has dynamic communication pathways to well over one thousand sedimentologists andstratigraphers in the UK, Europe, and beyond.

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2. CONFERENCE VENUEWindsor Building Conference Centre: https://www.royalholloway.ac.uk/media/8499/academic-locations_february-19.pdf

3. ORGANISATION AND SCIENTIFIC COMMITTEE

The 58 BSRG AM is organized by the Department of Earth Sciences (RHUL, UK)

Domenico Chiarella Amy Gough Dan BosenceNicola ScarselliF. Javier Hernández-Molina

with the support of the following research groups

4. PROGRAMME

Friday 13th

Saturday 14th

Sunday 15th

Monday 16th

Tuesday 17th

• Pre-meeting field trip• Pre-meeting workshops • Ice breaker party (Picture Gallery & Queen’s Building, RHUL)

• Talks & Posters• Conference dinner (Dorney Lake, Eton)

• Talks & Posters• BSRG AGM

• Post-meeting field trip (1st day)• Outreach activity, “The Ocean: a perspective from Earth Sciences”

• Post-meeting field trip (2nd day)• BOSCORF, NOC. Laboratory excursion & workshop

Dece

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6. FINAL SCIENTIFIC SESSIONS

5. KEYNOTES• Amanda Owen (Univ. Glasgow, UK); Fluvial stratigraphic response to a hyperthermal event

• Dave Hodgson (Univ. Leeds, UK); Laterally Offset Bulbous Elements, and other deep-water acronyms (Perce Allen Award 2018)

• Karyna Rodriguez (Spectrum, UK); Source rocks characterization using seismic reflection data

• Susanne Gier (Univ Vienna); Clays and mudstones in the hydrocarbon century and beyond (CMG sponsored)

Oral and Posters• Sessions 1, 8 and 15. DEEP WATER PROCESSES • Sessions 2 and 11. TECTONICS AND SEDIMENTATION• Session 3. NUMERICAL REPRESENTATIONS OF SEDIMENTARY ENVIRONMENTS• Session 4. TIGHT SANDSTONES AND MUDROCKS• Session 5. CONTOURITES AND REWORKED TURBIDITES• Sessions 6 and 16. SOURCE TO SINK• Session 7. RESERVOIR QUALITY OF CLASTIC AND CARBONATE ROCKS• Session 9. SALT-SEDIMENT INTERACTIONS• Session 10. GLACIOGENEIC AND GLACIALLY RELATED SEDIMENTS AND LANDFORMS• Session 12. SHALLOW MARINE• Session 13. ICHNOLOGY• Session 14. LACUSTRINE AND DEEP LACUSTRINE• Session 17. SEDIMENTOLOGY AND SOCIETY• Session 18 MICROPLASTICS AND POLLUTANTS: THE HUMAN FOOTPRINT IN THE SEDIMENTARY RECORD• Session 19. OBLIQUE RIFTING AND VOLCANIC PROCESSES CONTROLLING RESERVOIR DISTRIBUTION ALONG

THE NORTHERN ATLANTIC MARGIN• Session 20. EXPLORING AND CHARACTERISING DEEP WATER STRATIGRAPHY AND RESERVOIRS FROM

WESTERN EUROPE AND BEYOND: FROM CLASSIC SUBMARINE FANS TO INJECTITES• Session 21. FINE-GRAINED SEDIMENTARY ROCKS IN ENERGY DECARBONISATION• Session 22. SEDIMENTOLOGY

Posters• Session 23. CONTINENTAL SEDIMENTOLOGY• Session 24. MIXED SILICICLASTIC-CARBONATES• Session 25. GEOLOGY AS A TOOL TO AID IN CLIMATE CHANGE

Harold Reading (1924-2019): A tribute from his studentsJoseph A. Cartwright (Univ. Oxford, UK)

The life and achievements of one of the founding fathers of sedimentology,Dr Harold G. Reading, will be celebrated on the first day of the 58th BSRGAnnual Meeting.

Professor Joseph A. Cartwright, a former student,will lead the BSRG community in acknowledging thepivotal role that Harold played in establishing theconcepts of facies analysis and in makingsedimentology a mainsteam geological subject.

His achievements and legacy rundeep in our subject, including ‘thebook’ (Sedimentary Environmentsand Facies), the IAS and the BSRG,all of which were driven by Haroldin his modest, determined anddeeply enduring style.

Please join us in celebratingthe life of an exceptionalman who devoted hisworking life tosedimentology.

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8. TITLES OF PRESENTATIONS BY SESSION

SESSION: DEEP WATER PROCESSESOral (Day 1-14th December, 2019). Session 1Co-chairs: Megan Baker and Mike ClareWindsor Auditorium• Ben Tindal, Localised carbonate deposition above the Gaskiers diamictite - implications for Neoproterozoic cap

carbonates?• Daniela Vendettuoli, How grainsize controls a turbidity current structure? A compilation of a successful decade of

seafloor monitoring.• Arne Fuhrmann, Bottom current modification of turbidite lobe complexes• Hannah Brooks, Quantifying lateral and distal variability in clasts and matrix size within hybrid beds case studies

from Central and Northern Italy• Maria Azpiroz, Numerical simulation of multiple turbidity currents to analyse the flow-seafloor inter-relation

evolution• Laura Buehrig, A global database-informed investigation of submarine-canyon formation and evolution in a

source-to-sink context• Jefferey Peakall, Magical geology! When submarine fans vanish...

Oral (Day 2-15th December, 2019). Sessions 8 and 15Co-chairs: Maria Azpiroz (session 9) and Peter Haughton (session 16)Windsor Auditorium• Ashley Ayckbourne, Mechanisms of mass transport emplacement accommodation generation and infill in

creeping slope successions (Eocene Ainsa Basin Spain)• Jaco H. Baas, First evidence of flow-type driven sole marks and their distribution in a mixed sand-mud submarine

system• Patricia Buffon, Contribution of turbidity currents triggered by jets to sediment management in water reservoirs • Maarten Heijen, Infrequent large events versus frequent small events: importance for submarine channel

evolution• Chi Li, Influence of Thermal Fluid on Sandstone Carbonate Cement Quality: the Baiyun Sag Study Case (Northern

South China Sea)• Minru Zhao, Lithological Classification and Oil-Bearing Capability of Tight Reservoir in Permian Lucaogou

Formation Santanghu Basin Xinjiang China• Euan Soutter, What controls sediment delivery to deep-marine basins? An isotopic investigation of the Eocene-

Oligocene Alpine foreland basin• Adriana Crisostomo-Figueroa, Numerical modelling of equilibrium conditions for turbidity currents: examples using

submarine channels of the East Coast Basin New Zealand• Ross Ferguson, Spatial and temporal variability in the stratigraphic evolution of muddy and unstable continental

slopes: an example from the Shannon Basin western Ireland• Megan Baker, Can sand promote the cohesive forces in high-density clay-laden sediment gravity flows?• Joris Eggenhuisen, A critical appraisal of the Rouse equation as a simplified model for particle suspension in

turbidity currents.• Zoe Cumberpatch, Evolution of a mixed siliciclastic-carbonate system on an unstable margin: the Cretaceous of

the Eastern Greater Caucasus Azerbaijan

Posters (Day 1 & 2)• P1. Benjamin Couvin, A new model of deposition for the Tuaheni Landslide Complex, Hikurangi Margin, New

Zealand• P2. Muhamad Zulkifli, What are the dominant controls on submarine channel evolution? Detailed insights from

thirteen years of repeat mapping in Knight Inlet, British Colombia.• P3. Harya Nugraha, Lateral variation of submarine landslide frontal emplacement: a case study from Makassar

Strait, offshore Indonesia• P4. Arne Fuhrmann, Hybrid turbidite-drift channel complexes - an integrated multi-scale model• P5. Jonathan Wilkin, New insights into the internal structure of turbidite deposits from physical modelling of

relevant erosional and depositional processes• P6. Sojiro Fukuda, Flow Power of Turbidity Currents and Fluvial Rivers• P7. Apiradee Suwannathong, Thin-bedded turbidites, West Crocker Formation, Malaysia: Facies, microstructure

and porosity-permeability characteristics

Oral and Poster presentations and chairs for each scientific session including the first author, day, session number, poster number (PX) and location are listed next

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SESSION: TECTONICS AND SEDIMENTATIONOral (Day 1-14th December, 2019). Session 2Co-chairs: Tim Cullen, Nicola Scarselli and Chris JacksonRoom 0-02 and 0-03

• Jon Noad, The Guinness Book of Sedimentology: your guide to the world's largest EVER sedimentary features• Tim Cullen, Structural and palaeoclimatic controls on deep-water syn-rift depositional systems• James Hunt, Characteristics of the catastrophic December 22nd 2018 Anak Krakatau flank collapse and tsunami• Donald Christie, Simulation of Stratal Architecture in Deep Marine Mini-basins: Making it Realistic is Easy -

Making it Exactly Right is not• Miquel Poyatos-More, Multi-scale influence of topography on depositional architecture of long-term

transgressive successions (Jurassic Neuquén Basin, Argentina)• Andrew Procter, Deep-water lacustrine channel analysis as an aid to understanding fold growth history within

the South Caspian Sea Basin• Chris Elders, Middle Jurassic - syn-rift sedimentary systems in the Northern Carnarvon and Roebuck Basins of the

NW Shelf of Australia

Oral (Day 2-15th December, 2019). Session 11Co-chairs: Andy Emery and Janet RichardsonWindsor Auditorium• Peter Wooldridge, Quantifying Sediment Distribution in Fluvial-Deltaic Foreland Basins• Marco Pizzi, A statistical approach to quantify the structural controls on the distribution of deep-water slope

channels• William Mitchell, Quantifying the Structural Control on Submarine Channel Stacking Patterns: Case Studies from

the Niger Delta• Bernard Guest, Sandstone provenance and tectonics using detrital zircon metamorphic rim U-Pb dating• Marcus Duffy, Evolution of sandstone reservoir quality due to mineral alteration in proximity to igneous

intrusions• Alastair Robertson, Development of the Cambrian-Cretaceous pre-rift multi-stage rift passive margin and

emplacement Southern Neotethys: new evidence from the Antalya Complex in the Alanya Window (S Turkey)

Posters (Day 1 & 2)• P8. Mohamed Elouali, Geological study of detrital red formations in the central High Atlas (Morocco):

stratigraphic and paleoenvironnement implications• P9. Louis Howell, The influence of local low-density basement anomalies on the distribution of fluvio-deltaic

sediment in rift basins: the early Carboniferous Fell Sandstone Formation northern England• P10. Laura Sinclair, Patterns of erosion and subsidence associated with the mid-Aptian unconformity in the

Jeanne d’Arc Basin, offshore Newfoundland• P11. Elizabeth Balmer, Sedimentation of the remnant Tethys in the easternmost Mediterranean region: new

evidence from western Cyprus • P12. Xinong Xie, Stratigraphic architectures and break-up unconformity system in Zhujiangkou rifted margin

during the seafloor spreading of South China Sea• P13. Ivan Antonov, Geometry, kinematics and mechanics of inversion- fault reactivation and mechanical

stratigraphy: a case study on the Neuquén Basin, Argentina• P14. Chris Elders, A revised structural elements map of the North West Shelf• P15. Chris Elders, What does the evolution of sedimentary basins on the North West Shelf of Australia tell us

about Gondwana break-up?

SESSION: NUMERICAL REPRESENTATIONS OF SEDIMENTARY ENVIRONMENTSOral (Day 1-14th December, 2019). Session 3Co-chairs: Andrew Mitten and James MullinsWindsor Auditorium• Eoin O’Donnell, Testing the impact of fault growth models on syn-rift stratigraphy using forward stratigraphic

modelling• James Mullins, Deciphering reservoir complexity of ice-contact deltas using surface analoguesPoster (Day 1 & 2)• P16. Salim Ayomaya, Digital outcrop characterisation and forward modelling of the Calcarenite di Gravina

Formation exposed at Matera, Italy: better understanding of seismic sequence stratigraphy

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SESSION: TIGHT SANDSTONES AND MUDROCKSOral (Day 1-14th December, 2019). Session 4Co-chairs: Garrett Fowler and Jon RotzienRoom 0-05

• Sophie Behrendsen, Sedimentological controls on fluid flow in deeply buried aeolian gas reservoirs• Xinyu Zhong, Permeability Change Caused by Stress Damage of Tight Sandstone Reservoir in the Ordos Basin;

China• Jie He, Reservoir Characteristics and Evaluation of Tight Sandstone of Chang 8 Member in Zhenbei Oil Field Ordos

Basin• Enrica Battara, Carbonate depositional environments and their impact on reservoir properties: examples from

Central Mediterranean hydrocarbon fields• Ziyuan Meng, Basic to Acid Pyroclasts Deposited in A Sediment-hosted Geothermal System in A Permian

Lacustrine Rift Basin: Implications for Ancient Hydrovolcanic Sedimentation

Posters (Day 1 & 2)• P17. Kieran Blacker, Assessing the suitability of infrared hyperspectral imaging to characterise organic-rich

mudstones: an example from the Carboniferous Bowland-Hodder shales of the UK• P18. Shuwei Ma, Pore Structures and Occurrence Characteristics of Movable Fluid of Tight Sandstone Oil

Reservoir in Huachi area Ordos Basin China• P19. Jingyue Hao, Impacts of early diagenesis of organic-rich mudstones: an example from the Morridge

Formation the Widmerpool Gulf UK.• P20. Muhammad Sabiu Jibrin, Investigating microbial degradation of dissolved organic matter leachates from

marine black shale• P21. Catherine Russell, An Analysis of Facies and Architectural Elements in the Lower Cretaceous Wessex

Formation Wealden Group, Isle of Wight

SESSION: CONTOURITES AND REWORKED TURBIDITESOral (Day 1-14th December, 2019). Session 5Co-chairs: Adam Kirby, Alex Mason, Antoine Thieblemont, Debora Duarte, Niamh McGovern, Oswaldo Mantilla, Sandra de Castro, Sara Rodrigues, Wouter de Weger, Zhi Lin NgWindsor Auditorium

• F Javier Hernandez Molina, Depositional and erosional contourites features in the Morondava Basin offshore Madagascar

• William Bailey, Distribution of contourite drifts on convergent margins: examples from the Hikurangi subduction margin of NZ

• Zhi Lin Ng, Latest Miocene Mediterranean-Atlantic gateway restriction: The Atlantic's side of the story• Dorrik Stow, Contourite reservoir characteristics: Porosity grain size and a new sortable silt method• Wouter de Weger, Ancient contourite channels and their sedimentological criteria - case study from Upper

Miocene deposits in the southern Rifian Corridor Morocco

Posters (Day 1 & 2)• P22. William Bailey, Distribution of contourite drifts on convergent margins: examples from the Hikurangi

subduction margin of NZ• P23. Sandra De Castro Santos, New sedimentary model for Bottom Current Reworked Sands; IODP U1389 and

U1388 sites, Gulf of Cadiz• P24. F Javier Hernandez-Molina, Deep-water bottom current deposits from Cyprus• P25. F Javier Hernandez-Molina, Contourite features from the northern South China Sea• P26. Wei Zhou, Early Miocene to Quaternary unidirectionally migrating canyons in the northern slope of the

South China Sea continental margin• P27. Estefania Llave, Distribution of the Southern Contourite Channel (SE Gulf of Cadiz) after the opening of the

Strait of Gibraltar• P28. Jiawei Pan, Contourite facies and cyclicity: new update of geostatistical approach• P29. Adam Kirby, Distal sediment waves on the Argentine passive continental margin: characterization and

implications• P30. Oswaldo Mantilla, Contourite depositional systems in the Exmouth Plateau (North West Shelf Australia)

during the Mesozoic the Cenozoic• P31. Jiawei Pan, Contourite Facies and Cyclicity: A Geostatistical Approach• P32. Marga Garcia Garcia, Structural control on the downslope-alongslope sedimentary processes in the Cadiz

upper slope

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• P33. Sara Rodrigues, Late Cretaceous hybrid (turbidite-contourite) system offshore Argentina: morphology, evolution and paleoceanographic implications

• P34. David R Pedreros Bastidas, Seismic reflection data reveal Mesozoic-to-Recent bottom current activity in the Browse Basin offshore NW Australia

• P35. Niamh McGovern, Sedimentological characteristics and evolution of the deep-water system in the Porcupine Basin: conceptual and economic implications

• P36. Zeinab Smillie, Microbial Role in Deep-Marine Dolomite Formation within the Gulf of Cadiz Contourite Depositional System

SESSION: SOURCE TO SINKOral (Day 1-14th December, 2019). Session 6Co-chairs: Jon Rotzien, Laura Fielding, Mike BlumRoom 0-02 and 0-03

• Mike Blum, Tibetan and Himalayan Signals in the Detrital Zircon U-Pb Record of the Neogene and Quaternary Bengal Fan

• Jonathon Rotzien, Late Miocene sediment routing patterns and reservoir-scale architecture of deep-water slope base-of-slope and basin-floor fan depositional environments in the Taranaki Basin

• Dimitrios Charlaftis, Quantification of grain coatings in sandstone reservoirs• Conor McMillan, Sedimentary provenance and depositional environments from the Oligocene formations in the

north of the Salin sub-basin onshore Myanmar• Kimberley Johnson, Sediment Provenance and Routing Pathways of the Miocene Formations of the Salin Sub-

Basin Central Myanmar• Ikenna Okwara, Mass-balance analysis of the Middle Jurassic Brent Delta sediment routing system Northern

North Sea offshore UK and Norway

Oral (Day 2-15th December, 2019). Session 16Co-chairs: Jon Rotzien, Laura Fielding, Mike BlumRoom 0-02 and 0-03

• Kaja Fenn, The provenance of loess-palaeosol sequences along the Middle and Lower Danube• Eugene Szymanski, Paleoenvironments and Sediment Routing Along the Equatorial Atlantic Cretaceous Margin:

New Insights from DSDP/ODP/IODP Borehole Data Offshore Suriname Cote d'Ivoire and Ghana• Wiktor Luzinski, Textural development of sand grains in natural fluidisation• Chris Brewer, Grain size fractionation and sediment mass balance: The keys to unlocking the stratigraphic

archive in Source-to-Sink systems• Gavin Anthony, Source to sink history of the Neogene sedimentary rocks of the Miri Zone in Sarawak NW

Borneo using provenance tools.• Pieter Vermeesch, Is Geology Normal? The peculiar mathematics of sedimentary provenance data.

Posters (Day 1 & 2)• P37. Max Webb, Sedimentary provenance of the Nicobar Fan - Raman spectroscopy heavy mineral analysis

reveals more than zircons alone• P38. Laura Fielding, A Source to Sink and Reservoir-Quality Prediction Workflow: The Offshore Nile Delta• P39. Habibah Hanan Mat Yusoff, Identifying a source-to-sink framework of modern and palaeo-rivers: A case

study from the offshore Central Luconia Shelf and onshore Sarawak, Malaysia• P40. David Buchs, Detrital pyroxenes to characterise source to sink processes in volcano-sedimentary

environments: 3 examples with global relevance

SESSION: RESERVOIR QUALITY OF CLASTIC AND CARBONATE ROCKSOral (Day 1-14th December, 2019). Session 7Co-chairs: Luke Wooldridge and Joshua GriffithsRoom 0-05• Laura Fielding, Diagenetic control on mineralogical suites in sand silt and mud (Cenozoic Nile Delta): Implications

for reservoir quality• Robert Waltham, Spatial net-to-gross variability of a saucer shaped sandstone intrusion• Jian Shi, Diagenetic Features and Porosity Dense Evolution of Chang 8 Tight Sandstone Reservoir in Hujianshan

Area; Ordos Basin• Laura Bastianini, What causes carbonates to form shrubby morphologies? An Anthropocene limestone case

study.• Luke Wooldridge, The Digital Rock revolution of reservoir quality; understanding clay mineral morphology and

distribution in three dimensions• Valentin Zuchuat, CO2 containment and monitoring techniques along Little Grand Wash Fault east-central Utah

USA

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SESSION: SALT-SEDIMENT INTERACTIONSOral (Day 2-15th December, 2019). Session 9Co-chairs: Zoe Cumberpatch, Leonardo Muniz Pichel, and Charlotte RibesRoom: 0-02 and 0-03

• Zoe Cumberpatch, Halokinetic modulation of allogenic sedimentation; insights from numerical models and outcrop and subsurface analogues

• Alja Sassnowski, Constraints on caprock lithofacies and stratigraphy by application of a multi-method approach• Mareike Henneberg, Sedimentary and mineralogical features of evaporitic red bed sediments from Permian

diapir structures North Germany - a comparison• Ian Davison, Some Remarks on Unconformities around Salt Bodies• Frank Peel, Mud diapirism and catastrophic fluidization triggered by MTC collapse down a salt scarp: What

happens when a hundred billion tonnes of mud falls down a 1km-high slope?• Gillian Apps, Sediment transport over complex salt topography: fill & spill revisited

Posters (Day 1 & 2)• P41. Xing Pan, Differences in diagenesis of delta plain sandstone from the Yanéan Formation in the Yinjiacheng

area and its effect on reservoir classification• P42. Debora Duarte, Diapirism in the Betic Foreland: salt-sediment interaction during the late Miocene-

Quaternary evolution of the SW Iberian Margin

SESSION: GLACIOGENIC AND GLACIALLY-RELATED SEDIMENTS AND LANDFORMSOral (Day 2-15th December, 2019). Session 10Co-chairs: Bartosz Kurjanski, Thomas Vandyk, and Christoph KettlerRoom: 0-05

• Dan Le Heron, Complex development of a 300-million-year old subglacial unconformity in southern Namibia• Xiaoshuai Chen, Subglacial landforms formed by an Ediacaran ice sheet in west Henan North China• Christoph Kettler, Palaeo-ice streams and meltwater channels formed during the decay of a Late Palaeozoic ice

sheet in eastern Chad• Kieran Blacker, The consolidation properties of the glacial sediments of the Dogger Bank Tranche A - evidence for

multiple ice-sheet advance and retreat.• Bartosz Kurjanski, Ice-contact deltas investigation using sedimentology electrical resistivity tomography (ERT)

and ground penetrating radar (GPR) Salpausselka I and II near Lahti Finland• Stephen Davison, Dropstones slime and ice; re-advancing glacigenic interpretation in the Proterozoic Stoer

Group (Torridonian) of NW Scotland.

Posters (Day 1 & 2)• P43. Bethan Davies, Glacier processes and landscape evolution in a rapidly deglaciating Austrian valley glacier:

Gepatschferner Kaunertal Austria• P44. Marie Busfield, Fantastic flutes and where to find them: a 444 Ma subglacial pavement in South Africa• P45. Thomas Vandyk, Temperate glaciation on a Snowball Earth: Glaciological and palaeogeographic insights

from the Cryogenian Yuermeinak Formation of NW China• P46. Sinead Birks, Determining past ice flow direction and ice thickness in Eglwyseg and Glyn Ceiriog, North

Wales

SESSION: SHALLOW MARINE

Oral (Day 2-15th December, 2019). Session 12Chair: Domenico ChiarellaRoom: 0-02 and 0-03

• Kelvin Ikenna Chima, Pliocene and Pleistocene stratigraphic evolution of the western Niger Delta: A record of glacioeustatic and autogenic forcing.

• Richmal Paxton, Hot and late: clumped isotopes in Middle Jurassic calcite-cemented concretions from Skye• Matthew Watkinson, Extrinsic vs intrinsic controls on the architecture of shallow-water deltas: lessons from

mixed systems in a tectonically active basin

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SESSION: ICHNOLOGY

Oral (Day 2-15th December, 2019). Session 13Co-chairs: Francisco Rodrigues-Tovar and Javier DoradorRoom: 0-02 and 0-03

• Javier Dorador, Core bottom currents affecting ichnological signature within a muddy contourite drift: a case study from the NW Iberian Margin

• Francisco Rodriguez-Tovar, Ichnological analysis: a tool for characterize deep-marine systems

SESSION: LACUSTRINE AND DEEP LACUSTRINEOral (Day 2-15th December, 2019). Session 14Co-chairs: Tom Dodd, Stephen Andrews and Amy RegisRoom: 0-05

• Dan Bosence, Bumps in the Bay; Did carbonate mounds form the large circular sea-floor structures in Weymouth Bay Dorset UK?

• Tom Dodd, A depositional model for deep-lacustrine turbidite fans: examples from the North Falkland Basin• Pang Jungang, Recognition criteria of ancient deep lake line of depressed-type lacustrine basin: An Insight from

Triassic Yanchang Formation Ordos Basin China• Guilherme Bozetti, Field evidence of deep-lacustrine slope channels in the Triassic Yanchang Formation, Ordos

Basin, Northern China• Stamatina Makri, Late Glacial-Holocene high resolution records of productivity and meromixis from varved lake

sediments across Europe: methods and applications

Posters (Day 1 & 2)• P47. Shauna-kay Rainford, Temporal high-resolution recording of land use and fire dynamics from the Iron Age to

the Early Middle Ages at Lake Murten• P48. Connor Doyle, Microbe-mineral interactions in Modern and Ancient Saline-Alkaline Lakes of the Iberian

Peninsula: Early Findings from Laguna de Chiprana• P49. Amy Regis, Changes in depositional environments across an arid continental lacustrine system: Insights

from the Moenave Formation western USA

SESSION: SEDIMENTOLOGY AND SOCIETYOral (Day 2-15th December, 2019). Session 17Co-chairs: Andy Emery and Janet RichardsonRoom: 0-02 and 0-03

• Andy Emery, Sedimentary and stratigraphic archives of Late Pleistocene terrestrial drainage network evolution at Dogger Bank

• Ian Kane, Microplastics across global environments - a challenge for sedimentologists

Posters (Day 1 & 2)• P50. Octria Adi Prasojo, Backwater Hydraulic Geometry of Lowland Deltas

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SESSION: MICROPLASTICS AND POLLUTANTS: THE HUMAN FOOTPRINT IN THE SEDIMENTARY RECORDOral (Day 2-15th December, 2019). Session 18Co-chairs: Catherine Russell, Florian Pohl and Daniel BellRoom: 0-02 and 0-03

• Luyao Tu, Historical eutrophication history and long-term phosphorus fractions retention from sediments in Lake Burgschi (Switzerland) since the early 1900s

• Michael Clare, Deep-sea circulation creates seafloor microplastic hotspots• Yasmin Yonan, Controls on microplastic vertical distribution in an urban environment in the River Thames London

UK• Florian Pohl, Turbidity current transport deposition and burial of microplastics

Posters (Day 1 & 2)• P51. Giorgia Beffa, Exploring prehistoric vegetational and agricultural dynamics using an annually laminated

sediment record from Lago di Mezzano in Latium, Italy• P52. Connor Burchell, Investigating transport processes of macroplastic in fluvial environments• P53. Jack Lacey, Understanding human-driven ecosystem change in a tropical Southeast Asian wetland• P54. Edward Keavney, Transfer of microplastics from terrestrial to marine environments: Tracking transport

from the River Mersey to Liverpool Bay

SESSION: OBLIQUE RIFTING AND VOLCANIC PROCESSES CONTROLLING RESERVOIR DISTRIBUTION ALONG THE NORTHERN ATLANTIC MARGIN

Oral (Day 2-15th December, 2019). Session 19Chair: Nicola ScarselliRoom: 0-04

• Bent Erlend Kjolhamar, Pre-Cretaceous highs controlling fairways for gravity-driven sedimentation in the Norwegian Sea

• Sverre Planke, The influence of voluminous magmatism on Paleogene sedimentary systems in the West of Shetland and outer Møre and Vøring basins

SESSION: EXPLORING AND CHARACTERISING DEEP WATER STRATIGRAPHY AND RESERVOIRS FROM WESTERN EUROPE AND BEYOND: FROM CLASSIC SUBMARINE FANS TO INJECTITESOral (Day 2-15th December, 2019). Session 20Co-chairs: Andrew Hurst, Rob Butler, Grant Wach, and Jon RotzienWindsor Auditorium

• Mario Andres Gutierrez, Process Stratigraphy of Deepwater Depositional Systems: Bedform Recognition Criteria & Applications

• Michael Steventon, Laminar and transitional sediment gravity deposits as baffles and barriers to fluid flow: a case study from the Magnus Field northern North Sea

• Timothy Wigan, Sub-seismic heterogeneity in early post-rift deep-water lobes; insights from the Angel Formation NW Shelf Australia

• Grant Wach, Outcrop analogues for petroleum system characterization of the Central and North Atlantic margins

• Jonathon Rotzien, The range and variability in sediment gravity flow deposits and petroleum reservoirs

Posters (Day 1 & 2)• P55. Lauren Clarehugh, Controls on the geometry extent and reservoir quality of sand injectites: combining

worked industry datasets (Norwegian Continental Shelf) with outcrop analogue studies (Vocontian Basin, Southern France)

• P56. Benjamin Panting, A Review of Thin Bedded Pay Determination and Produceability• P57. Junia Casagrande, Architectural variability in a stepped-slope fan system - implications for reservoir

connectivity

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SESSION: FINE-GRAINED SEDIMENTARY ROCKS IN ENERGY DECARBONISATION

Oral (Day 2-15th December, 2019). Session 21Co-chairs: Joe Emmings, Mark Wilkinson, and Patrick DoweyRoom: 0-02 and 0-03

• Joe Emmings, Investigating the sedimentary rock record using text mining• Mark Wilkinson, 10 Things We Don't Know About Clay Minerals• Andrew Wiseall, The role of physical properties in storage and disposal in the subsurface

SESSION: SEDIMENTOLOGY

Oral (Day 2-15th December, 2019). Session 22Chair: Charlotte PriddyRoom: 0-05

• Charlotte Priddy, Ephemeral fluvial-aeolian interactions: from outcrop studies to core analysis• Jonathan Scafidi, Hydrogen storage in porous rocks: the storage capacity of the UK continental shelf

SESSION: CONTINENTAL SEDIMENTOLOGYPosters (Day 1 & 2). Session 23

• P58. Hazel Beaumont, Is it possible to work out the lateral migration of preserved fluvial systems through outcrop?

• P59. Jon Noad, Oranges and Phenoms: deconstructing a Cretaceous meandering channel in southern Alberta• P60. Chloe Griffin, Localised rotational effects on granular temperature in granular flows• P61. Elena Bellizia, Intra-point bar grain-size variability: an example from the Holocene alluvial succession of the

Venetian Plain (Italy)• P62. Marta Cosma, Piracy-controlled geometry of tidal point bars: examples from modern and ancient channel

networks• P63. Daniela Fontana, Sedimentary structures and textures in sand injectites. Insights from dikes and sand blows

of Holocene fluvial sediments (Emilia Italy)• P64. Sinead Lyster, Palaeohydrology of Late Cretaceous sediment routing systems, Utah, USA in space and time.

SESSION: MIXED SILICICLASTIC-CARBONATESPosters (Day 1 & 2). Session 24

• P65. Yu-Chun Chang, The Characteristics of Submarine Landslides in Active Volcanic Settings: Cohesion from Slope Stability Analysis, the Central Azores Islands

• P66. Massimiliano Ghinassi, Reading tidal processes where their signature is criptic: the Maastrictianmeandering channel deposits of the Tremp Formation (southern Pyrenees Spain)

• P67. Domenico Chiarella, Scales and heterogeneities in mixed siliciclastic-carbonate deposits

SESSION: GEOLOGY AS A TOOL TO AID IN CLIMATE CHANGE

Posters (Day 1 & 2). Session 25

• P68. Andrew Bond, Quantifying marine redox; using non-traditional geochemical techniques on late Triassic sediments

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9. WORKSHOPS

USES OF A CARBONATE-EVAPORITE CORE AND HOW TO LOG ONETrevor Burchette (CRG Ltd./ RHUL)

Duration; ~3:30 h lectures + 3 h Core logging exercise Minimum / Maximum participants= 5 / 25

F. Javier Rodríguez-Tovar (Univ. Granada, Spain) & Javier Dorador (RHUL)

APPLICATION OF ICHNOLOGY IN SEDIMENTARY BASIN RESEARCH

Duration; ~4h lectures + 2 h practical sessions Minimum / Maximum participants= 5 / 25

In the petroleum and other industries, borehole corerepresents the only real ground truth against which to calibratemany sorts of theoretical models and more remote physicalobservations. These include conceptual geological models basedon seismic and regional data, petrophysical models concerningreservoir quality and fluid saturations, as well as aspects of rock-typing and reservoir heterogeneity, all of which allow optimumdevelopment of an asset. However, cores really form only one-dimensional samples of the formations being investigated and alarge degree of interpretation and not a little imaginationfounded on geological knowledge are required for theirinterpretation. The workshop is intended for geosciencestudents who have no experience of logging borehole cores, butwho wish to gain some insight into how cores and the datagained from them are used in the petroleum industry.

This workshop focuses on the application of ichnology in sedimentarybasin research with special attention to palaeoecological anddepositional interpretations, and the influence of biogenic structures tosediment features (i.e., porosity & permeability). Main objectives of thecourse will be, to introduce the conceptual framework of ichnology; tolearn about the two main paradigms ichnology as the ichnofabricapproach and the ichnofacies model, and to explore the use of tracefossils in palaeoecological and depositional interpretations, with specialattention to oil exploration and reservoir characterisation.

PRE-MEETING WORKSHOPS

F.J. Hernández-Molina (RHUL), Domenico Chiarella (RHUL) & Jon Rotzien (Basin Dynamics, USA)MARINE SEDIMENTARY PROCESSES & PRODUCTS

Duration; ~3h lectures + 3 h exercises + 1 h general discussion Minimum / Maximum participants= 5 / 25

In the last decades, our knowledge andunderstanding of processes & products in marineenvironments have grown very fast. Both scientific,economic and environmental endeavours haveincreased exploration in marine basins. Thisworkshop considers some of these findings and theirimplication at geological scale, being divided intothree parts; shallow marine; gravitational andbottom currents. So, new perspectives in marinesedimentation and their integration in currentmodels (e.g., source to sink) will be discussed withimplications for academia and industry.

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INTRODUCTION TO SEDIMENT CORE DESCRIPTIVE LOGGING

Suzanne Maclachlan & BOSCORF staff (NOC, UK)

Duration; 1 Day Minimum / Maximum participants= 10 / 30

Sedimentary logging is the graphical method for describing a succession of sediments and crucially forms thefoundation of most sediment core analyses. The workshop is intended for geoscience students who have noexperience of logging soft sediment cores, but who wish to gain some insight into how sediment core descriptions canbe used to interpret environmental settings. This is a laboratory-based introductory workshop to sedimentologicalcore logging, smear slide analysis and data visualisation, using examples from the BOSCORF collection to cover a rangeof environments. Included in the day course will be a tour of BOSCORF and NOC.

Logistics: Participants will independently travel to Southampton, to meet at NOC reception 9 am. A light lunch will beprovided (included in the course fee).

POST-MEETING WORKSHOPS

17th December 2019. BOSCORF, National Oceanography Centre SouthamptonLaboratory excursion & workshop (17th)

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10. FIELD TRIPS

Pre-meeting field trip (13th December 2019)PORTISHEAD (UK); A journey from continental to marine in clastic sedimentology.

Leader: Dan Le Heron (Univ. Vienna, Austria) & Amy Gough (RHUL)

Duration= 1 dayMinimum / Maximum participants= 10 / 30

Morning:Portishead

Afternoon: Aust Cliff

Lunch in pub

AimsTo study (i) some excellent outcrops of Late Carboniferous to early Devonian age (Portishead) in the morning and

(ii) Middle to Late Triassic and Jurassic deposits (in Aust Cliff, Gloucestershire- time permitting) in the afternoon.

ItineraryMorning: a traverse from Battery Point to Woodhill Bay, Portishead. Carbonates occur at the Battery Point sections

and include a rich variety of marine fossils, among which crinoids, brachiopods, bivalves, fish scales,eurypterids and a number of different types of ichnofossils occur. Stratigraphically above, and along the coastto the south, an excellent section of cross-bedded sandstones and conglomerates crop out both as tabularbeds and lenticular geometries separated by mudstone beds. Our aim is to study both the carbonates and thesiliciclastic rocks in this classic location. It is hoped that the mix of lithologies and environments will keepeveryone happy, and we can consider the nature of the contact between the two.

Lunch: and ensuing interpretative disagreements, will be at one of the local pubs within short walking distance fromthe outcrops. Lunch at the participants’ own cost.

Afternoon: Time permitting, we will visit the famous Aust Cliff section near the Severn Bridge, which is famous for itsreptile, teeth and fish remains in certain Triassic levels. In spite of the short days in December in Bristol(sunset 16.01 on 13th December) expect to have some good time to visit this section after lunch, providedthat no-one orders 3 course dinners. The Aust Cliff has excellent fossil hunting potential.

LogisticsBus leaves from The Hub, Royal Holloway main campus (Founder’s tennis court), at 8.00 am. Bus to arrive back at

Royal Holloway @18.00 (approx.). Note for safety: We will be studying coastal sections in the vicinity of Portishead.These will be coastal sections along the Bristol Channel. We will time our arrival to be mid tide. Predicted tide timesfor Woodhill Bay on 13th December are: High tide 7.12 am; low tide 2.18 pm. Participants arriving independentlyplease meet at 10 am at the junction between Esplanade Road and Beach Road on the seafront. There should bepublic toilets available.

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Organised by the Department of Earth Sciences of the Royal Holloway, University of London and the

in collaboration with the Marine Studies Group of the Geological Society of London (UK)

• 09:30 – 10:30 The polar oceans (Robert Larter, British Antarctic Survey, UK)

• 10:30 – 11:30 The Ocean from a geological perspective (Ros Rickaby, Oxford Univ., UK)

11:30 – 12:00 Coffee break

• 12:00 – 13:00 The Ocean in changing climate (Elvira Poloczanska, Alfred Wegener Institut, Germany)

When: 16th December 2019Where: The Beatrice Shilling building auditorium, Royal Holloway, University of London, Egham, UK

58th British Sedimentological Research Group Annual General Meeting

The Oceana perspective from Earth Sciences

The talks are specifically aimed at 6thform students and those with a generalinterest in our ocean as viewed within thecontext of the Earth Sciences!

11. OUTREACH ACTIVITIES

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AimsThe non-marine carbonates of the Purbeck limestones were deposited in a shallow lake on the western margin of

the Wessex Basin during its late syn-rift phase. New research at RHUL demonstrates that an early brackish phase ischaracterised by in-situ highly porous thrombolitic microbial mounds. In cross-section, they show tabular-shapedsmall mounds (up to 50 cm high and 1 m across) that constitute large, more complex-shaped mounds (up to 4m highand 18m across). In plan-view these mounds have a circular shape up to 20 m in diameter and are surrounded andonlapped by an inter-mound packstone-grainstone facies. Together those facies are arranged in high-frequencylacustrine cycles capped by paleosols.

Itinerary1st day: Waking up so early will be difficult in a cold winter morning but the rocks we will see are worth it. On this first

day, we will visit 4 disused quarries across the Isle of Portland (2 in the morning and 2 in the afternoon).At Portland Bill we will see the transition between marine deposits of the Portland Limestone Group (oolitic

grainstone with marine bivalves) organised in massive beds and lacustrine deposits of the Purbeck LimestoneGroup (wackestone-packstone with peloids and some ostracods) organised in thin laminated beds withpaleosol intercalations.

At Tout Quarry we will have an introduction to the succession with Portland-Purbeck boundary and the basalMupe Member with Skull Cap, Lower Dirt Bed, Hard Cap, Great Dirt Bed, Soft Cap and Cypris Freestones.Overview of microbial mounds, their geometries and their relationships with inter-mound facies.

Lunch at the Lobster Pot (Portland Bill) where the famous local fresh crab sandwich is served. Lunch at theparticipants’ own cost.

At God Nore and Freshwater Bay we will see the basal part of the Purbeck Limestone Group where two sequencesillustrating the development of in-situ microbial mounds (some around tree trunks and branches) in abrackish water lake environment and capped by paleosols.

At Stonefield Quarry we will see pseudo 3-D cross-section view of mounds and architecture and relationship withinter-mound facies.

2nd day:

Lulworth Cove east side we will see plan-view of mounds and folded structures in Lulworth Bay and we will discussnewly discovered offshore circular structure imaged in Weymouth Bay seafloor by multi-beam echo sounder.

Post-meeting field trip (16th – 17th December 2019)Syn-rift lacustrine carbonates: cycles, microbial mounds & brackish-hypersaline facies. Purbeck, Wessex Basin UKLeaders: Arnaud Gallois (CGG, UK) & Dan Bosence (RHUL)

Duration: 2 days – 1 nightMinimum / Maximum participants = 7 / 18

More information at Gallois A., Bosence D., Burgess P., 2018. Brackish to hypersaline facies in lacustrine carbonates: PurbeckLimestone Group, Upper Jurassic–Lower Cretaceous, Wessex Basin, Dorset, UK. Facies, 64:12.

LogisticsBus leaves from The Hub, Royal Holloway main campus, at

6 am on Monday 16th and return at approx. 6 pm onTuesday 17th. One-night accommodation is included in thecost at The Edenhurst on Weymouth seafront. Participantneed to choose single or shared rooms.

Lulworth Cove west side to see section through thePurbeck limestones showing open and closed lakedeposits. These are organised as a succession ofclays, oolitic and shelly grainstones and fresh- tobrackish water mollusc-rich beds (coquinas of theUnio Member, Corbula Member, Broken ShellLimestone or Purbeck Marble).

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12. SOCIAL PROGRAMME

Friday 13th Ice breaker party. Picture Gallery and Queen’s Building, RHULTime: 18:00

Saturday 14th. Conference dinnerDorney Lake, https://www.dorneylake.co.uk/parties.aspxTime: 20:00Buses depart at 18:30Cost £ 75 / person (including coach)

Royal Holloway's finest geologist DJ, theone and only DJ Cyclone, spinning thedecks with only the very best of tunesand rocking all your bones on thedance floor

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Bus meeting point for the post-meeting field trip

Outreach “The Ocean”. The Beatrice Shilling building auditorium

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Next we are providing details on travelling to the Royal Holloway campus and registering for the conference

on the first day. You can download a campus map to help find your way around once on campus.

13. DELEGATE INFORMATION AND JOINING INSTRUCTIONS

a. Arriving at Royal Holloway• By TaxiFor those arriving at London airports, we strongly recommend that you do not take the expensive black cabs,

but call either Windsor Cars http://www.windsorcars.com/ (+44 1753 677677) or Gemini Cars

http://www.geminicars.co.uk/ (+44 1784 471111). Windsor Cars have a dedicated email for pre-booking

journeys: [email protected]. Most local taxi companies know the Royal Holloway campus well and

should be able to drop you at the correct area.

• By busThe timetable for bus route 441 from Staines or Egham is as follows:

https://www.surreycc.gov.uk/__data/assets/pdf_file/0006/7836/441-White-Bus-250618.pdf

For bus route 8, the timetable can be found here:

• By trainThere are frequent services from London Waterloo to Egham (35-40 minutes); Woking to Egham (35 minutes,

change at Weybridge) and Reading to Egham (40 minutes). Services at weekends, especially those on Sundays,

are less frequent than on weekdays. Train links to the rest of the country are available via the London stations

or Reading. There are usually taxis waiting outside Egham station to take you to Royal Holloway, which is

located less than a mile from the station www.southwesternrailway.com.

• By carRoyal Holloway is on the A30, 19 miles from central London and about a mile south-west of the town of

Egham. It is 2 miles from junction 13 of the M25 (London Orbital). After leaving the motorway, take the A30

west, signposted to Bagshot and Camberley (this is the Egham by-pass). At the first roundabout, take the

second exit. At the second roundabout, take the second exit and continue on the A30 up Egham Hill. Royal Holloway is on the left at the top of the hill. Free parking is available on campus. The car parks are indicated on

the car parks map. The SAT NAV post code is TW20 0EX.

Car parking arrangements

The car park map shows a variety of car parks on site. For the Windsor Building and Picture Gallery, please use

either Car Park 12 or Car Park 4.

Delegates will not need to register their vehicles in advance and therefore the car park signage requesting

visitors to register their vehicles does not apply.As car parking spaces are free of charge, they cannot be booked and are allocated on a first come, first served

basis. Please note that a penalty charge notice (PCN) will be issued for any vehicles parked in contravention of the College’s parking regulations.• Directions on campusPlease use the campus map given at registration to find your way around campus. There will be some

conference signage but this will be minimal in compliance with College policy.

The campus map will help locate the Windsor Building and Picture Gallery before arrival.

• Mobility issuesPlease ensure that any mobility issues have been forwarded to the conference organisers at least 5 working

days before arrival.

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b. Conference registrationFor delegates arriving on Friday evening for the Ice Breaker Drinks Reception on Friday 13th December, registration will take place in the Picture Gallery in our main Founder’s Building from 18.00.

Picture Gallery(Follow the entrance marked by blue arrow)

Windsor Building

For delegates arriving on Saturday morning, registration will take place in the Windsor Building Foyer.

Delegates will receive a badge which allows access to the building, participation in seminars and refreshments. Anyone without a badge will not be able to access conference workshops or events. The badge is also needed for lunches and refreshments. Please wear your conference badge at all times, as identification is required to access conference services and sessions.

c. Refreshments and lunchesProgramme fees include morning and afternoon refreshments and a self-service lunch in the Windsor Building on Saturday 14th and Sunday 15th December. Water and squash will be available throughout the day – please bring a re-fillable bottle with you if possible, to help reduce our plastic waste.

There will also be an Ice Breaker drinks reception on Friday 13th December in the Picture Gallery.

• Dietary requirementsPlease ensure that any dietary requirements which were not given during the online registration process have been forwarded to the conference organisers at least 5 working days before arrival. Most diets can be catered for if advised in advance.d. Internet accessFree WiFi access to ‘CampusNet’, our high speed wireless internet service, is available across the entire campus. Each conference is issued with a unique guest username and password which will allow you to register on the WiFi network and provide you with access for the duration of your stay. Although access is available across the campus, we do advise that you and your speakers bring any essential documents or media with you in a hard or digital copy.

To log on: • Open internet browser• Of the 2 available options, click on the ‘Guest User’ option • Terms of use - confirm acceptance• Enter username and password

ü User ID: 58bsrgü Password: 58bsrg2019

After 60 seconds, you will be asked to close down and open the browser again. You will only have to complete this registration process once for the duration of your stay. The same username and password will be required if accessing the internet in the bedrooms. Details are also provided on the reverse of your key envelope.

If for any reason the above instructions do not work, please enter the following into your browser: nac.rhul.ac.uk/ and press enter. Follow the instructions on screen and enter the above Username and Password when prompted.

You will only have to complete this process once as the code covers the duration of your stay/event.

Please note that the access provided is standard internet; organisations would need to specify any specific non-standard internet access in advance so we can support your requirements.

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e. Medical AssistanceIf you should become unwell or suffer an injury, there are several options. The nearest Accident and Emergency department is at St Peter’s Hospital in Chertsey. For first aid enquiries only, the College has its own Health Centre situated in the Founder’s Building. It is open from 9.00am – 1.00pm and 2.00 - 5.00pm Monday to Friday. An out-of-hours answer phone will provide you with details of an on-call doctor, should you need medical assistance when the centre is closed. Medicines can also be purchased in the Union Shop on Campus.

f. Shops and ATMsThe ‘Union Shop’ is located within the Davison Building in Founder’s Square. Opening hours: Monday – Sunday: 8.00am – 6.00pm. Other shops can be found in nearby Egham and Englefield Green.

There are ATMs at the Students Union Building and at the Windsor Building. Other ATMs can be found in Egham and at the BP petrol station on the A30 towards Egham.

g. SafetyIn the event of a fire or other emergency, please leave via the nearest emergency exit. Delegates should then go to the nearest Assembly Point indicated by a large Green and White sign. Each building has its own Assembly Point, which is identified by a number or letter, their location is given on the Fire Action Notices located at each Fire Alarm Call Point. A check that everyone attending the Symposium is present will then be made.

If you discover a fire you must: • Operate the nearest fire alarm • Leave the building by the nearest exit • Go to your designated Assembly Point

Fire Fighting Equipment must only be used by persons who have been trained to do so, and only after the alarm has been sounded.

Fire Evacuation procedure If the Fire Alarm sounds at any time other than a scheduled testing time (or for longer than 30 seconds on a scheduled test, as above) then you must:

1. Leave the building by the nearest exit 2. Close doors behind you 3. Report to your designated Assembly Point 4. Do not return to the building until authorised to do so 5. Do not use lifts 6. Founder’s Building only – A red light will flash at the entrances/exits to the Building when the fire

alarm has been activated and re-entry into the building will only be allowed when these lights are turned off (regardless of whether the sounders are sounding)

All gangways, passages staircases and exits must be kept clear from any obstruction at all times.

h. Local RestaurantsIndianMegnaOn the main street of Englefield Green, providing classic tasty dishes and consistently great service for reasonable prices.(2 St Jude’s Road, Englefield Green, Surrey TW20 0DB)

ChineseMagic WokAuthentic Beijing and Sichuan dishes on the Egham High Street.(17 High Street, Egham)

ThaiEat Thai Provides traditional and fusion Thai dishes conveniently situated on Egham High Street.(67 High Street, Egham)

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ItalianPrezzoA member of the familiar chain that provides simple, tasty Italian dishes.(2 Egham Hill, Egham, TW20 0AY)CaspariA gem of a local restaurant that serves traditional Italian food cooked beautifully.(4 St Jude’s Road, Englefield Green, TW20 0DB)Caffé Gondola A lively Italian restaurant that also boasts a bar, and dishes out cheap, good food and quick service.(168 High Street, Egham, TW20 9HP)

Pub foodThe PackhorseNow leased by Royal Holloway, this newly refurbished pub (formerly known as the Monkey’s Forehead) offers decent food at fair prices. Located opposite the college towards Egham.(70 Egham Hill, Egham TW20 0BQ Egham Hill, Egham)The Barley MowA historic pub situated on the green after which Englefield Green is named. (Englefield Green, Egham TW20 0NX)The Red Lion A newly renovated pub that has kept serves hearty homemade food.(52 High Street, Egham, TW20 9EW)The BeehiveA cosy pub that serves traditional pub food and German dishes as well.(34 Middle Hill, Englefield Green, TW20 0JQ)The Fox and HoundsA large, traditional English pub in Englefield Green, serving great food and wine. Located at one of the entrances to Windsor Great Park.(Bishopsgate Rd, Englefield Green, Egham TW20 0XU)

OtherBar 163For something a little fancier, this is the place to go. Delicious food, tasteful décor, and a walled garden which is perfect to enjoy your meal in on a Summer evening.(163 High Street, Egham, TW20 9HP)Hugo’s Bar and GrillHugo’s has a cocktail bar and a selection of simple, hearty dishes. Occasionally a musician will perform there, which only adds to the lively atmosphere. (72 High Street, Egham, TW20 9EY)9. AssistanceIf, in an emergency, you need to contact somebody outside of office hours with regard to the academic conference content, the following team member can be contacted:

Amy Gough / Email: [email protected]

Please feel free to contact Customer Services or call +44 (0)1784 443285 if you have queries about our facilities. Dialling 444 on internal campus landlines or +44 (0)1784 443888 will initiate an emergency response from our 24 hour security team.

E-mail: [email protected]: +44 (0) 1784 44 3604

@BSRG19

15. CONTACT US

http://bsrg.rhul.ac.uk14. WEB PAGE

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16. LOCAL INFORMATION

Local Taxi facilitiesGemini +44 (0) 1784 47 1111

AccommodationThere are many different styles of accommodation at Egham, Staines and Windsor to suit all budgets and

needs.We recommend to start to book in advance because close to Christmas can be difficult to findaccommodation in the area. For more info please check https://bsrg.rhul.ac.uk/venue.html

Family activities• Thorpe Park resorts (3.8 mi from Egham)• Legoland (6.7 mi from Egham)• National Trust- Runnymede (1.3 mi from Egham)• Windsor Great Park (9 mi from Egham)• Windsor & Windsor Castle (6 mi from Egham)• Virginia Water Lake (3 mi from Egham)

17. SPONSORS

About EghamEgham is a town in the Runnymede borough of Surrey, in the south-east of England. It is part of the

London commuter belt and has its own railway station. It adjoins, narrowly, junction 13 of the M25motorway and is situated 19 miles (31 km) WSW of London. It can be considered a university town as it hason its higher part, Egham Hill, the campus of Royal Holloway, University of London. Not far from this town,at Runnymede, the Magna Carta was sealed. More information athttps://www.visitsurrey.com/explore/egham-p196021

About Royal Holloway University of LondonRoyal Holloway, University of London (RHUL) is a public research university and a constituent college of

the federal University of London. It has three faculties, 20 academic departments and c. 10,615 studentsfrom over 100 countries. The campus is located in Egham, Surrey, 19 miles (31 km) from central London(40´by train) and just 7 miles (11.2 km) from Heathrow international airport (15-30´ by taxi). Moreinformation at https://www.royalholloway.ac.uk

If you want advice on either planning your travel, or get ideas for spending some extra days in Egham, Windsor or surrounding areas, please contact us at: [email protected]

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