2. evidence of former depositional environments deep marine black shales pelagic muds/oozes...

25

Upload: tariq-lambson

Post on 16-Dec-2015

219 views

Category:

Documents


3 download

TRANSCRIPT

Page 1: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 2: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

2. Evidence of Former Depositional Environments

Page 3: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Deep Marine

•Black Shales

•Pelagic Muds/Oozes

•Greywackes

•Mature

•Immature

•Laminations

•Graded Bedding ( some evidence of cross bedding & ripple marks)

•Sole Marks

•Graptolites

•Slow build up of sediment apart from turbidites

Page 4: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 5: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 6: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 7: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 8: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 9: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 10: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 11: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Carboniferous 360 – 290 MYA

Carboniferous Limestone

Brachiopods

Crinoids

Ammonoids

Colonial coral

Page 12: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Upper Carboniferous

limestonemudstone

sandstone

Delta top / swamp

Fluvial channel fill

Delta front

Prodelta

Offshore

Page 13: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Upper Carboniferous

Delta top / swamp

Fluvial channel fill

Delta front

Prodelta

Offshore

Turbidity currents

Page 14: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Upper Carboniferous

Carboniferous Limestone

Brachiopods

Crinoids

Ammonoids

Colonial coral

Millstone Grit (ssts)

Medium-grained Arkose

Quartz

FeldsparWeak cross bedding

Mudstones

Shales

Page 15: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Suggest the environment of deposition of the sediments shown in Fig. 1c and give evidence for your conclusion. (5)Environment:

Deltaic (1)

Evidence:

Coal swamp/rootlets/complete fossil plants (1)Coarsening up sequence (1)Cross-bedded sands (1)Marine sediments/bivalves (1)Marine to freshwater (1)Shallowing of water (1)

Page 16: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 17: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

363 Ma

290 Ma

325 Ma

315 Ma

Page 18: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Devonian 409 – 360 MYA

Sandstones & conglomerates

Limestones & Marine fossils

Page 19: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Devonian - 400 mya

South of equator 10-20ºArid/desert climate – similar to SW USA (New Mexico/Texas)Old Red Sandstone (ORS) ContinentRapid erosion of Caledonian mountains (Caledonian orogeny)Rivers & lakes in basins between mountainsTropical ocean to south (Rheic Ocean)

Desert sandstones – lack of fossilsAlluvial sandstones – river depositsLimestones – brachiopodsShales – lake deposits, primitive fish, land plants, insects on land & first winged insects

Page 20: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Alluvial Environments (meandering rivers)Lithology:

Texture:

Mineralogy:

Structures:

Fossils:

Page 21: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

• conglomerates

• well-sorted red sandstones

• desiccation cracks & calcrete

• cross bedding

• repeated cycles

• alluvial fan deposits formed at edge of Caledonian mountain area

Old Red Sandstone Deposits

Page 22: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

1 cm

ORS sandstone, Orkney

Medium to fine grained red sandstone with cross bedding

Page 23: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

50 cm

ORS conglomerate, Aberdeen

Boulder sized clasts of quartzite, granite, rhyolite & andesite

Page 24: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some
Page 25: 2. Evidence of Former Depositional Environments Deep Marine Black Shales Pelagic Muds/Oozes Greywackes Mature Immature Laminations Graded Bedding ( some

Devonian Marine Deposits