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ASX : PCL
PANCONTINENTAL OIL & GAS NLPANCONTINENTAL OIL & GAS NLKENYA PROJECTS
March2012March 2012
AUSTRALIAAUSTRALIACANNING BASIN• EP 104 / R1• L15NAMIBIA
WALVIS BASIN• EL 0037
AUSTRALIACARNARVON BASIN
EP 424
KENYALAMU BASIN• L6• L8• L10A
EL 0037
• EP 424• EP 110
• L10A• L10B
DisclaimerThese materials are strictly confidential and are being supplied to you solely for your information and should not be reproduced in any form,redistributed or pass on, directly or indirectly, to any other person or published, in whole or part, by any medium or for any purpose. Failure tocomply this restriction may constitute a violation of applicable securities laws.
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The distribution of these materials in other jurisdictions may also be restricted by law, and persons into whose possession these materials comeshould inform themselves about, and observe, any such restrictions.
This presentation includes forward-looking statements that reflect the company’s intentions, beliefs or current expectations. Forward lookingstatements involve all matters that are not historical fact. Such statements are made on the basis of assumptions and expectations that theCompany currently believes are reasonable, but could prove to be wrong. Such forward looking statements are subject to risks, uncertainties andassumptions and other factors that could cause the Company’s actual results of operations, financial condition, liquidity, performance, prospects oropportunities, as well as those of the markets it serves or intends to serve, to differ materially from those expressed in, or suggested by, theseforward-looking statements. Important factors that could cause those differences include, but are not limited to: changing industry. Additionalfactors could cause actual results, performance or achievements to differ materially. The company and each of its directors, officers, employees andadvisors expressly disclaim any obligation or undertaking to release any update of or revisions to any forward-looking statements in the presentationadvisors expressly disclaim any obligation or undertaking to release any update of or revisions to any forward looking statements in the presentationor these materials, and any change in the Company’s expectations or any change in the events, conditions or circumstances on which theseforward-looking statements are based, expected as required by applicable law or regulation.
By accepting any copy of the materials presented, you agree to be bound by foregoing limitations.
h h il d j i b d i f i il d b h hThe summary report on the oil and gas projects is based on information compiled by Mr R B Rushworth, BSc, MAAPG,MPESGB, MPESA, Chief Executive Officer of Pancontinental Oil & Gas NL. Mr Rushworth has the relevant degree ingeology and has been practising petroleum geology for more than 30 years.Mr Rushworth is a Director of Pancontinental Oil & Gas NL and has consented in writing to the inclusion of theinformation stated in the form and context in which it appears.
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Pancontinental Snapshot
• Pancontinental Oil & Gas is listed on theAustralian Securities Exchange (ASX) undercode PCLcode PCL
• Market Capitalisation of about A$ 170 million
P j i KENYA (18 000 k ) NAMIBIA• Projects in KENYA (18,000 sq km), NAMIBIA(17,000 sq km) and AUSTRALIA
• Growing Portfolio of East & Southwest African• Growing Portfolio of East & Southwest AfricanAssets
• Recognised Partners with Successful AfricangTrack Record
• Defined & Funded Work Programme
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Pancontinental
KENYA is a very favourable country for oil and gas projects-projects
• No indigenous oil or gas production--- hence a strong need for local energy productionstrong need for local energy production
• Transparent and encouraging legislation and fiscal regimeregime
• Enthusiastic and supportive Ministry and national il (NOCK)oil company (NOCK)
• Physical exploration opportunities in exciting geology
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PANCONTINENTALApache, Tullow, Origin KENYA
Anadarko, TotalFAR
OphirCove
ShellBG Group, Premier
Ophir
Petrobras
Shell
Ophir
PetrobrasTANZANIA
BG Group, Ophir Statoil, ExxonMobil
TANZANIA
PANCONTINENTAL OIL & GAS
Anadarko, Mitsui, Bharat Videocon ENH
ENIPANCONTINENTAL OIL & GASEAST AFRICAMAIN OFFSHORE OIL & GAS PLAYERS*February 2012 Bharat, Videocon, ENH
CoveMOZAMBIQUE
y*Not definitive, not complete
Pancontinental Offshore KenyaPANCONTINENTAL OFFSHORE KENYA• Four blocks totalling >18,000 sq km
• Significant long term holdings in prime areas
Ethiopia
Somalia
• Major partners with successful African track records
• Very large prospect potential (> 1 Billion Bbls)
Somalia
KENYA
L6 - 3,100km2
FAR 60%Pancontinental 40%
L8 5 123km2
KENYA
L6Pemba Island Oil Seep
Pate 1 Wet Gas Flow
L8 – 5,123km2
Apache 50%Origin 20%Pancontinental 15%Tullow 15%
L8TanzaniaGas Discoveries
Songo Songo Gas Field
Oil d G Di
Mnazi Bay Gas FieldGas Discoveries
Pemba Island Oil Seep
L10A – 4,962km2
BG 40%Cove 25%Premier 20%P i l 15%
0 Km 400
Tanzania
L10A
L10B
0 Km 100 -------------
Mozambique
Oil and Gas Discovery Pancontinental 15%
L10B – 5,585km2
BG 45%Premier 25%
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0 Km 400 ---------- Pancontinental 15%
Cove 15%
Offshore Kenya- BathymetrySediment and Nutrient (Source Rocks)Input by Tana River
Why is Pancontinental in Kenya’s offshore L B i ?Lamu Basin?A simple beginning-----BATHYMETRY
NE – SW Prevailing Currents imply …….CounterclockwiseCounterclockwise Oceanic Circulation
KENYA
Tana River Delta progrades to the SSE • Bulge in bathymetric contours off
southern Kenya suggests a delta
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southern Kenya suggests a delta prograding to the south• Interpreted NNE- SSW predominant current direction during delta formation
Why is Pancontinental offshore in Kenya’s Lamu
Palaeocene Depth & Residual Gravity
offshore in Kenya s Lamu Basin?A simple beginning----
Tana River Sediment and Nutrient input
GRAVITY DATA Basement Trough Axis L6
Basement Davie Ridge-
Basement High
g L6
L8Trough AxisBasement HighL8
KENYA
Mbawa Trend -Tertiary
Inversion AxisL10A
Gravity data supports location of oil “kitchen” troughs, shown in Dark Blue
Pemba – Simba
L10A
e ba S baRidge-
Basement HighPANCONTINENTAL
Offshore Kenya- Exploration Model Sediment and Nutrients (Source Rocks)Input by Tana Riverp y
NE – SW Prevailing Currents imply …….Conterclockwise
L6
KENYA
Conterclockwise Oceanic Circulation
Mbawa Trend
L8
L10AL10A
L10B
Tana River Delta progrades to the SSE
Pancontinental exploration areas optimally located in delta , over generating troughs and on Mbawa inversion trend
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M. Jurassic Plate TectonicReconstruction - Close-up
Plate Tectonics- PANCONTINENTAL
PancontinentalArea of Interest
Restricted seaway during continental separation- Good for hydrocarbon source rock deposition and preservationsince ?Early Jurassic
Late Cretaceous Plate Tectonic Reconstruction
Plate Tectonics-Reconstruction
Madagascar India Separation
PANCONTINENTAL
g p
WB
SAUDIARABIA
AFRICA
NEOTETHYS OCEAN
WB
RestrictedCirculation Enclosed seaway continues into Late
Cretaceous
OCEANIC CRUST, DEEP
SR
MGR
PNGRestrictedCirculation
INDIAN OCEAN
Cretaceous
OCEANIC CRUST, DEEP
DISTAL SHELF/BASIN
DELTAIC- NEARSHORE-SHELF
GIN
PROXIMAL SHELF
ANTARCTICA
Circulation
AUSTRALIA
CO
NTI
NEN
TAL
MA
RG
LIMESTONE NEARSHORE- SHELF
EVAPORITES
NON-MARINEACTIVE CONTINENTAL MARGIN
ACTIVE SPREADING RIDGE
ANTARCTICA
C
SIGNIFICANT EROSION, MOUNTAINS
NON-DEPOSITION
MAXIMUM GLACIATIONPRESENT DAY COASTLINE/BLOCK BOUNDARY
SEDIMENT INPUT
COMPRESSION/COLLISION
WBWESTERN BURMA
SourceKitchensandMigrationKENYA L6, L8, L10A & L10B
Source Kitchens and Migration• Recent & Tertiary Regional Isopach Map –
• Tertiarydepocentres;sourcekitchens;andTertiary depocentres; source kitchens; and generalised migration pathways
• Thick Tertiary loading means relatively recently KENYAy g y ymaturity and generation
Oceanic current organic matter
S
Sgdilution (poor Source Rock quality)
Ponded lower delta Source Rock TANZANIA
S
areas (excellent Source Rock quality)S
Nutrient Rich Delta S
Main Migration Pathway
PANCONTINENTAL
Pancontinental
De-risking The Concept
(i) Depositional model(ii) Oil Seeps(iii) Fluid Inclusions(iii) Fluid Inclusions(iv) Seismic –
CharacterStructuresStructuresDepositional featuresFlat spots, AVO’sP !Prospects!
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Satellite Synthetic Aperture R d (SAR)Radar (SAR) KENYA L6 & L8
•Interpreted natural oil sea surface slicks. •L6, L8 - best areas for slicks offshoreL6, L8 best areas for slicks offshore Kenya from available data•Natural oil seep on Pemba Island, south of L10B
L6
L8PANCONTINENTALPANCONTINENTAL
KENYA L6 & L8
L8Mbawa Jurassic prospect outline (2D) ~ 500+ SQ KM
Mbawa sea surface slicks interpreted as light oil or condensate
Mbawa Base Tertiary prospect outline (2D)~180 SQ KM
SEA-SURFACE SLICKS OVER MBAWA PROSPECTPANCONTINENTAL OVER MBAWA PROSPECTPANCONTINENTAL
SEA FLOOR 3D OBLIQUE VIEW
KENYA L8 – MBAWA SEA FLOOR POCKMARKS AND SEA SURFACE SLICKS
SEA FLOOR POCK MARKS
POCK MARKS= EXPULSION CRATERS
SLICKS
BASE TERTIARY PROSPECT OUTLINE
Mbawa Prospect slicks coincide with interpreted sea-floor expulsion craters -consistent with pminor natural leakage on N flank of Prospect
PANCONTINENTAL
Maridadi Fluid Inclusion Oil•Oil inclusionsoccur in twosamples inMaridadi
KENYA L6 & L8
•Oil inclusions occur in two samples in Maridadi1B exploration oil well
–The 4,190 m sample with a GOI value of 3.2% is interpreted to have moderately good evidence for palaeo-oil zone.
–The 4,110 m sample is interpreted to reflect the presence of oil in trace amounts in water or gas saturated reservoir at the Flourescing oil inclusions from Maridadi 1Bin water or gas saturated reservoir at the time fluid inclusions formed.
Evidence of Upper Cretaceous or younger oil
•MCI analysis shows the Maridadi-1B FIoil is likely
Evidence of Upper Cretaceous or younger oil from fluid inclusions in Maridadi 1
y yto be derived from Upper Cretaceous or younger calcareous source rocks
•This is an important finding as some geologists thought that only Jurassic or older rocks were viable oil source rocks
The pristane/ phytane ratio assesses the redoxconditions within the depositional environment.
The ratio is < 1 for oils of marine origin related to sapropelic plankton organic matter, while it Is > 1 for oils of coastal marine or continental origin
PANCONTINENTAL
Kenya L6 & L8 Slicks
KENYA L6 & L8
• L6 + L8 Total 8,200km2
• Water depths 0 to 1300m & onshore
• Major Cretaceous / Tertiary geologicaltrough thought to be oil generating
L6• Prospects associated with slicks in
both areas –supporting concept of oilgeneration
Slicks
L8• Variety of large Prospects• Slicks associated with Prospects
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• Slicks associated with Prospects support Pancontinental oil concepts
800m WATER DEPTH
0 Km (approx) 2
KENYA L8Thick Tertiary deposition (>4,000m) “cooked up” mature oil source rocks in the adjacent Trough
MBAWA PROSPECT
( pp )
PANCONTINENTAL
POSSIBLE TERTIARY “FLAT SPOTS”
TERTIARY / CRETACEOUS “FLAT SPOT”-Possible Gas-over –Oil interface
POSSIBLE LOWER “FLAT
MAIN DRILLING TARGETPossible thick Oil column
SPOT”- Possible Oil-over-Water interface
JURASSIC CHANNEL SANDS
Dual Seismic Flat Spots in Mbawa Inversion “popped up” good channel and turbidite sands in central Mbawa- Best reservoir rocks should be in the crestal zone
Kenya L8
KENYA L8• PCL 15%• 5,100 Km2
• Water depth 0 to 1,300m• Mbawa drilling planned mid / Q3 2012 –
PCL free carried by Tullow• Farmins by Apache and Tullow 2011SLICKS Farmins by Apache and Tullow 2011• New operator Apache looking at rig
availability• Slicks coincide with sea floor expulsion
craters
SLICKS
SLICKS
L8MBAWA POTENTIAL *MBAWA POTENTIAL *Tertiary / Cretaceous (P10):• 4.9 Billion Barrels oil in place
plus-• 284 Billion Cubic Feet gas in
* NOTE - Potential volumes arePancontinental projections and donot necessarily reflect those of otherjoint venture participants and may
t il t b t i
284 Billion Cubic Feet gas inplace plus-
Jurassic (P10)• 323 Million Barrels oil in place or• 525 Bcf in place gas cap plus--
• Mbawa potential approx5 Billion Bbls oil in place(P10)
• Mbawa drilling planned
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not necessarily prove to be correct inthe future.
Tertiary has further potential• Mbawa drilling plannedmid / Q3 2012
Kenya L8 – Mbawa MBAWA DRILLING
• One Mbawa well to 3,500m will test multipletargets
Water depth of approximately 800m easilySea
• Water depth of approximately 800m - easilyaccessible with modern equipment
• Main target- Lower Tertiary / Upper Cretaceous
• Secondary targets- Upper Jurassic & shallower
Sea floor – 800m
1,000m Lamu Limestone
Secondary targets Upper Jurassic & shallowerTertiary Simba Shale
Kipini ShaleTertiary
*EARLY PALAEOGENE BASIN FLOOR TURBIDITE ‘FAN’ SANDS (Kipini Sands)
2 000m
Cretaceous
**
LATE CRETACEOUS BASIN FLOOR TURBIDITE ‘FAN’ SANDS (Kofia Sands)
Kipini Sands
Kofia SandsKofia Shale
Primary Targets1,800m – 2,200m
2,000m
2,140m
Walu Shale
CARBONATES Jurassic
*
*JURASSIC SANDSTONES & / OR CARBONATES (Mb o / Isalo II Sands
EARLY CRETACEOUS DELTAIC SANDS (Ewaso Sands) 2,800m
3,000m
Walu ShaleEwasu Sands
?
*
SANDSTONE
SHALE
EXPLORATION TARGET
JurassicCARBONATES (Mbuo / Isalo II Sands, Amboni Limestone)
Secondary Targets2,700m – 3,400m
• Mbawa potential approx 5Billion Bbls oil in place (P10)
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* EXPLORATION TARGETp ( )
• Mbawa drilling planned mid/ Q3 2012
Why is Pancontinental offshore in Kenya’s Lamu
Palaeocene Depth & Residual Gravity
offshore in Kenya s Lamu Basin?A simple beginning----
GRAVITY DATA- Basement Trough Axis L6
Followed-up with L10A & L10 Projects in 2011
Basement Davie Ridge-
Basement High
g L6
L8Trough AxisBasement HighL8
•Gravity data supports location of oil “kitchen” troughs•Play concept followed up with new
L10A
•Play concept followed up with new L10A & L10B projects- 2011
Mbawa Trend -Tertiary
Inversion AxisPemba – Simba
L10A
e ba S baRidge-
Basement HighPANCONTINENTAL
Kenya L10A & L10B – Leads
Extension of Mbawa TrendSimba Trend
KENYA L10A & L10B• Pancontinental 15%• 5 Play Types
KENYAChannel Trend
5 Play Types• > 10 Leads• 3D & 2D late 2011• 2 wells 2013 -2014
A d d M 2011Mombasa L10A
• Awarded May 2011• 10,000 km2
• “Fast Track” explorationprogramme
• Water depth 200-1,800mp ,• Interpreted oil “kitchen”
troughs in Blocks• Notable partners-
BG GroupPremier Oil
L10B
Premier OilCove Energy
---------------0 Km 20
L10B
Jurassic TrendMiocene Reef T d
• “Fast Track” Exploration• Multiple leads and play types
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Jurassic TrendTrendp p y yp
• 3D and 2D already acquired• Drillable prospects expected Q4 ‘12
Kenya L10A & L10B – Leads
High Amplitudes +?Phase Reversal
Amplitude Shutoff
Olkaria Lead
Miocene reefMiocene reef
Tertiary / Upper C t ti li
Rollover into Fault – Amplitude Supported
Miocene Reefs
Cretaceous anticline Supported
KENYA L10A & L10B• Pancontinental 15%• 5 Diverse Play Types
Upper Jurassic reefUpper Jurassic Reef or
Mounded Basin Floor T bidit Pil
5 Diverse Play Types• > 10 Leads• 3D & 2D late 2011• 2 wells planned•Several Prospect expected to be
d t d ill b Q4 2012
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Turbidite Pile ready to drill by Q4 2012
Kenya L10B – Windjammer Look-alike
Thrust - related Antiform
Kenya L10B Lead
Undrilled
Flat events, phase reversals
Flat events, phase reversals
Flat events, phase reversals
Flat events, phase reversals
Amplitude
Windjammer / Lagosta etc –
Offshore AmplitudeCut-offsMozambique
Gas Discovery -30 to 50+ Tcf in
place
KENYA L10A & L10BA large Kenya L10B lead is similar on seismic to the
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place Windjammer gas discovery off Mozambique
Kenya L6 Kifaru ProspectKENYA L6• PCL 40%• 3,134 Km2
• Water depth 0 to 300m• Kifaru- main prospect adjacent to interpretedKifaru- main prospect adjacent to interpreted
hydrocarbon kitchen / trough• Farming out 2012• 3D over 2+ prospects 2012• Drilling 2012 / 2013
KENYA L6 EXPLORATION PLAY•Lamu Basin has >10km of sediments•Various good source rocks sampled along the East African margin.Many wells intersected good oil and gas shows; 3 wells flowed gas.•Thick Tertiary deposition brings potential source rocks into play as•Thick Tertiary deposition brings potential source rocks into play asmature oil sources. Migration pathways are short and direct.•Lamu Basin- part of a failed Late Cretaceous to Tertiary rift, withgood analogues of prolific oil prone Early Tertiary source rocks inIndia’s Bombay and Cambay basins. Cretaceous and Tertiarydepocentres in restricted marine settings between structural highs.•Eocene source rock samples range up to 11% TOC and hydrogenindices up to 688 - this interval could be an excellent oil source•L6 has a variety of structural leads- E trend has leads clustered onadjacent to Maridadi Trough.•Almost 8tcf unrisked recoverable resource identified and mapped atthe Eocene Kipini sands level Most structures are closed in the
KIFARU
the Eocene Kipini sands level. Most structures are closed in thedeeper Cretaceous where additional resource potential exists. Twoof the main leads are Kifaru and Tembo. Kifaru is old featureadjacent to interpreted generating trough.
KENYA L6
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KIFARUPROSPECT
KENYA L6• Numerous Prospects / Leads•Kifaru 3D mid 2012
Pancontinental
What’s Next ?
• Mid year / Q3 2012 - drilling Mbawa in L8, with some 5 billion barrels of oil potential in place
• In L10 Blocks - 3D and 2D results later this year and planning a• In L10 Blocks - 3D and 2D results later this year and planning a minimum of 2 wells in these blocks once we get the data
• In L6 we will be acquiring about 1000 sq km of 3D mid year
• We look forward to a very exciting year, starting with the possibility of finding the first ever commercial oil offshore Kenya in the giant Mbawa PProspect
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Pancontinental Oil & Gas NLPancontinental Oil & Gas NL
Ground Floor, 288 Stirling Street
Perth, WA 6000
Australia
Tel: +61 (8) 9227 3220
Fax: +61 (8) 9227 3211
http://www.pancon.com.au
Barry Rushworth CEO of Pancontinental Oil & GasCEO of Pancontinental Oil & Gas
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