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BPH ENERGY LTD Audit Report / Information 2010

Dec 21, 2010

64555_rns_2010-12-21_3bfc8e74-1bcd-4ae7-b0e7-7ca5cf8ac6a4.pdf

Audit Report / Information

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22 December 2010

Companies Announcement Office Australian Securities Exchange Limited 10th Floor, 20 Bond Street SYDNEY NSW 2000

Dear Sir,

ADVENT ENERGY PEP11 INDEPENDENT EXPERT REPORT – PERMIO TRIASSIC

MEC Resources (ASX:MMR) is pleased to provide the attached independent geological expert’s report on the Permio Triassic section commissioned by investee company Advent Energy Limited (Advent) for Advent’s PEP11 project in the offshore Sydney Basin.

The report was prepared by Mr Tim Berge of Pangean Resources LLC. Tim Berge is an internationally recognised geophysicist with over 30 years experience, including time with Exxon Ventures and Forest Oil, and is credited with a number of significant field discoveries including the multi-Tcf Ibhubesi Field in South Africa.

Of key significance is the conclusion that PEP11 has all the working components of a gas-charged hydrocarbon system and is a potential giant gas province. The mean estimate of the portfolio aggregate prospective resources has been calculated to be 15.9 Tcf recoverable.

The major shareholders of Advent are:

MEC Resources (ASX: MMR) BPH Energy (ASX: BPH) Talbot Group Investments Grandbridge (ASX: GBA)

Yours sincerely,

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David Breeze Media Enquiries: Executive Director Bill Kemmery MEC Resources Ltd Fortbridge Consulting PO Box 317 Tel: +61 2 9331 0655 North Perth WA 6906 Mobile: +61 400 122 449 Tel: +61 8 9328 8477

About MEC Resources

ASX listed MEC Resources (ASX: MMR) invests into exploration companies targeting potentially large energy and mineral resources. The Company has been registered by the Australian Federal Government as a Pooled Development Fund enabling most MEC shareholders to receive tax free capital gains on their shares and tax free dividends.

About Advent Energy

Advent Energy Ltd is an unlisted oil and gas exploration company, held by major shareholders MEC Resources (ASX: MMR), BPH Energy, Grandbridge (ASX: GBA) and Talbot Group Investments. Advent holds a strong portfolio of exploration and near-term production assets throughout Australia. Advent’s cornerstone project lies off the coast of NSW in Petroleum Exploration Permit 11 (PEP11), and comprises gas prospects of multi-Tcf capacity. Advent Energy’s wholly owned subsidiary Asset Energy Pty Ltd will increase its interest from 25% to 85% of PEP11 by drilling the first well. Bounty Oil and Gas (ASX:BUY) will thereby reduce their interest from 75% to 15%.

Notes: In accordance with ASX listing requirements, the geological information supplied in this report has been based on information provided by geologists who have had in excess of five years experience in their field of activity.

MEC is an exploration investment company and relies on the resource and ore reserve statements compiled by the companies in which it invests. All Mineral Resource and Reserve Statements have been previously published by the companies concerned. Summary data has been used. Unless otherwise stated all resource and reserve reporting complies with the relevant standards. Resources quoted in this report equal 100% of the resource and do not represent MEC’s investees’ equity share.

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MEC Resources Ltd

ACN 113 900 020 PO Box 317, North Perth, WA 6906

14 View Street, North Perth 6006, Western Australia T: +61 8 9328 8477 F: +61 8 9328 8733 [email protected] www.mecresources.com.au

INDEPENDENT EXPERT REPORT

PEP11 Block Offshore Sydney Basin Australia

Prepared by PANGEAN RESOURCES LLC T.B. Berge, P.G., TBPG#6318 November, 2010

Prepared for Advent Energy Ltd

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CONTENTS

CONTENTS
SUMMARY CONCLUSIONS 4
INTRODUCTION 5
REGIONAL GEOLOGY 6
PETROLEUM SYSTEMS ELEMENTS 11
SOURCE 11
RESERVOIR 15
SEAL 18
PROSPECTS SUMMARY 20
INDIVIDUAL PROSPECT DETAILS AND RISKS 20
KEY PARAMETERS 22
PORTFOLIO AGGREGATION 31
CONCLUSION 32
FIGURES
Figure 1, Location of Block PEP 11 offshore Australia. 5
Figure 2, Major sedimentary basins of Australia. 6
Figure 3, Global Magnetic and Gravity Field Data for SW Australian region. 7
Figure 4, Structural Model of the Sydney Basin. 8
Figure 5, Depth structure map. 9
Figure 6, General Stratigraphy of the Sydney Basin. 10
Figure 7, Seismic profile showing generation and migration pathways. 12
Figure 8, Line B19 Neural Network. 13
Figure 9, Details of seafloor mound. 14
Figure 10, Isotopic analysis of Catherine Bay seeps. 14
Figure 11, Complete log suite from Munmorah. 16
Figure 12, Log analysis of select interval from -550m to -760 m depth, Munmorah. 16
Figure 13, Log analysis of select interval from -1650m to -1870m depth, Munmorah. 17
Figure 14, Scaled correlation of Munmorah section with the Fish prospect location. 18

2

Figure 15, Log analysis of interval -1270m to -1490m, Munmorah well. 19
Figure 16, Leads Map. 20
TABLES and CHARTS
Table 1, Prospect List and 3P Reserves Summary 4
Table 2, Permeability by formation and age. 15
Table 3, Porosity values by formation and age. 15
Table 4, Prospective reserves distribution, all prospects. 21
Table 5, Individual prospect assessment and risking details. 23
Table 6, Portfolio Aggregation Plot. 31
Table 7, Table of Aggregate Portfolio values. 31
DIGITAL APPENDIX 33
BIBLIOGRAPHY 33
CONSENT LETTER 34

3

SUMMARY CONCLUSIONS

Evaluation of all available Geologic and geophysical data, summarized here, show that PEP11, which covers a majority of the Sydney Basin offshore NSW Australia, has all the working components of a gas-charged Hydrocarbon system and is a potential Giant Gas province. The Fish Prospect, confirmed through ongoing seismic data review, is a fault bounded 4-way dip-closed anticline structure estimated to comprise 11.5 Tcf (Mean) prospective recoverable gas resources. A large prospect named Baleen is located in the northern sector of the Permit in an average depth of 125m of water and is situated on the crest of the Offshore Uplift on a thrusted anticline. With a closure of over 202 km[2] (50,500 acres), the Baleen target has potential to hold 1.4 Tcf (Mean) of prospective recoverable gas resources.

Looking past any single initial test, and assuming success, we may wish to assess the possible value of the entire portfolio by a defined process known as Portfolio Aggregation. Calculating the Aggregate Sum of the Prospective Reserves, the Mean of the Portfolio Aggregate is 15.9 Tcfg recoverable. These are “Undiscovered Prospective Reserves” as defined by the SEC and SPE 2005. The equivalent classification if terms of a 3P assessment would be: (Low) P1= 410 Bcfg, P2= 4.25 Tcfg, (Best) and P3 (High)= 47 Tcfg, the equivalencies are allowed and defined specifically by the SPE (Etherington, 2005), these are also by those same definitions and guidelines considered “Undiscovered Prospective Reserves” and assume successful outcomes.

TABLE 1: Prospect List and 3P Reserves Summary

Reserves, Bcfg Reserves, Bcfg
Prospect Name Mean P90 P50 P10
Fish 11508.6 28.6 2131.2 35491.8
Baleen 1452.0 17.2 472.2 4193.3
Shark 3510.9 44.1 752.2 10656.0
N Sei 435.3 8.5 162.3 1226.1
W Sei 192.9 3.7 71.9 543.4
E Sei 327.3 6.4 122.0 921.9
Trout 623.9 12.1 232.6 1757.3
Humpy 429.7 8.3 160.2 1210.4
Orca 810.7 15.7 302.3 2283.7
Octopus 471.4 9.2 175.7 1327.9
Squid 585.0 11.4 218.1 1647.7
Blue 799.0 15.5 297.9 2250.6
Blue Whale 3410.8 66.2 1271.6 9607.6
S Squid 777.2 66.2 289.7 2189.1
S Humpback 87.7 1.7 32.7 247.1

4

Introduction

Advent Energy has been granted an option to acquire up to an 85% interest in PEP 11, an oil and gas permit located in the offshore Sydney Basin, from Bounty Oil and Gas NL (Bounty).

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Fig. 1 Location of Block PEP 11 offshore Australia.

The block is a 200km long, 8,250km[2] permit area that covers most of the offshore extent of the Sydney Basin.

Petroleum system elements all seem to be present and active. There is gas production onshore and abundant gas seeps in both offshore and onshore parts of the basin. There is ready market and infrastructure for gas development. Three 2D seismic surveys (a total 2525 line miles), reprocessed in 2007 and in 2010, have been interpreted and mapped. A number of prospects have been defined from this database that are the subject of this study.

Mapped prospects and leads within the offshore Sydney Basin are generally located less than 50km from Australia’s largest energy market, the Sydney-Wollongong-Newcastle greater metropolitan area. This area has a population of approximately 5,000,000 people. Traditionally, all natural gas used in New South Wales has been piped in from South Australia and the Bass Strait. However, studies by the Australian Bureau of Agricultural and Resource Economics (ABARE) and the Australian Petroleum Production and Exploration Association (APPEA) state that those sources may not be able to meet the demand for gas in the medium to longer term. NSW government forecasts suggest an increased power requirement of 10,000 GWh by 2015.

5

Regional Geology

New South Wales / Offshore Sydney Basin

The Sydney Basin is a Late Paleozoic cratonic basin that was rifted first during Pangea breakup in Mid Jurassic, and during continued separation of the Lord Howe Rise.

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Figure 2. Major sedimentary basins of Australia

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Australian
PEP11
Plate
(approx)
Pacific Plate
Global Magnetic Field Data, Austral Region
Austral Region NOAA, NGDC, and CIRES
EMAG2- New Global mag coverage, compiled sat, ship, and air mag measurements, released Feb., 2009 (Maus et al, 2009)
Australian
Plate
Pacific Plate
Global Gravity Field Data, Austral Region
from GRACE- twin sats deployed in 2002, CSR, GFZ Potsdam, NASA, and DLR
Pacific-Antarctic Ridge
Pacific-Antarctic Ridge
New Caledonia
New Caledonia
New Hebrides
New Hebrides
Tasman Ridge
Tasman Ridge
Tonga-Kemadec Arc
Tonga-Kemadec Arc
Lord Howe Rise
Lord Howe Rise
V
V
V
V
V
V
V
V
V
V
V
V
V
V
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Figure 3. Global Magnetic and Gravity Field Data for SW Australian region showing major plate elements, ridges, trenches, and Plate transform margins.

7

This later rifting is a result of oceanic crust generation at the Tasman ridge south of the Sydney Basin. The Offshore extent of the basin is untested but prospective for gas (Blevin, 2001). The onshore extent of the basin produces some coal-associated gas, and has play elements that may be extended directly and by analogy into the offshore.

The Northwestward motion of oceanic crust and it’s subduction into the New Caledonian Trench, relative to the stable Australian Craton, places the Sydney Basin in left-lateral shear. Bends in a strikeslip system may be either restraing or releasing depending on the curve of the zone or faults. We hypothesise that a structural model of a restraining bend in a left-lateral system is valid for this area. We can match the highs and major faults with highs and faults predicted in such a model. Compare the Model (Fig. 4) with the mapped features (Fig. 5).

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Peel-
Manning
Thrust
Thrusting
develops in
confining
bend
Restraining Bend,
Sinistral (left- lateral)
Strike -Slip
deformation
V
V
Anticline
Anticline
V
V
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Fig. 4, Structural Model of the Sydney Basin

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Fig 5, Depth structure map. Note how the 2 main fault trends and locations of the 2 highs ( compare fig. 5 with fig. 4 above) correspond to the model predictions.

9

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Fig. 6, General Stratigraphy of the Sydney Basin (from Bradley, Graham)

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Although there have been over a thousand wells drilled in offshore Australia, no exploration drilling has ever taken place in the offshore Sydney Basin. The Fish and Baleen prospects will be the first primary structural targets drilled to test this basin.

Recent interrogation and reprocessing of seismic data has allowed for observation of Direct Hydrocarbon Indicators (DHI), including Amplitude Versus Offset (AVO) analysis, with positive results. Gas chimneys and hydrocarbon related diagenetic zones (HRDZ) have been identified, and flat spot events coincident with the Baleen prospect are being investigated.

The prospectivity of the northern sector has been further enhanced by the confirmation of the presence of ongoing hydrocarbon slicks. Originally detected on 1996 satellite imagery, a repeat analysis of 1998 and 2001 images again identified apparent slicks directly over the Baleen prospect. Inferred gas seepage along the PEP 11 / continental margin from Geoscience Australia’s 2006 continental slopes survey, and inshore observed hydrocarbon seepage has further evidenced the offshore Sydney Basin as an active hydrocarbon system. Independent study has found that 79% of wells drilled in positive geochemical anomalies resulted in commercial oil or gas discoveries.

Advent has secured a rig slot to drill PEP 11 in the 4[th] Quarter 2010.

Petroleum System Elements

The Sydney Basin has long been known as having resource potential and a having a working thermogenic gas-prone petroleum system. The first area assessment was done by Exon et al in 1991 (4.5 Mboe, or about 27 Bcfg) was and indicated a thermogenic source rock. Here are the details of the Petroleum System elements;

Summary

  • Source: Permian Coal Beds, Permian/Carboniferous marine shales

  • active seeps, Thermogenic Methane, gas production onshore

  • Reservoir: Triassic/Permian/Sands

  • Documented reservoirs Onshore

    • Porosity range 8 – 12 % (Triassic to 30%) Permeability. 1mD to 1 Darcy
  • Net Sand Thickness ~ 100ft

  • Seal: Triassic and Permian mudrocks

Source

“Although the high inertinite and vitrinite content of the coals indicate that they are primarily a potential source of gas, the Upper Permian coals of the Sydney Basin compare favourably as a potential source for both oil and gas with the Toolachee Formation, the main late Permian source in the Cooper Basin of southwest Queensland and South Australia. The Late Permian coal measures attain a thickness of about 1600m at the coast between Newcastle and Terrigal-1, and thicken and dip offshore.” (Alder, 1998).

It is expected, given the abundance of gas indications, that there is an active, coal source rock in the basin.

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It is worthwhile to note some of the abundant indications of migrated gas (Heggie, et al, 1997, Clennel et al, 2009, Kroh, 2009) ;

  • 1) Active seeps Chemotropic mounds

  • 2) Shallow BSR’s

  • 3) Amplitude anomalies

  • 4) Seismic evidence of seepage

If so, intervention would have positive environmental impacts besides being a significant energy resource.

Profile of proposed well Baleen # 1 [Seismic Line B4-19]

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Baleen #1
-200m
-1250m
-4000m
Cenozoic Layer S1
Top Tri-Permian
Top Dalwood Group ?
Basement?
Baleen #1
Oil/Gas
Pliocene + Q
Miocene
Middle Triassic
Early Triassic
Late Permian
Early Permian
Basement?
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Fig. 7, Seismic profile and interpretation showing proposed source generation and migration pathways and eventual leakage to surface. Compare suggested migration routes to fig.9 seep routes.

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Fig. 8, Line B19 Neural Network (Chimney Cube”) processing showing seep class in green. Demonstrates Nonfault seal trap type. Documents gas primary and secondary migration routes. These seeps can be seen to form seafloor mounds .

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Fig. 9, Details of seafloor mound on line 19 seep.

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Fig. 10, Isotopic analysis of samples from the area of Baleen mounds. Heavier hydrocarbons are to the right. There is an abundance of gas phase light compounds, and the range to heavier aromatics and aldehydes is indicating a mature petroleum source. Advent Energy report, “Gore” sampling, June 2010. Note the Gore technology does not sample methane.

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Reservoir

Direct evidence supporting the presence and quality of possible reservoir rock offshore is welldocumented. A summary of permeability and porosity measurements from numerous onshore wells is shown in Tables 3 and 4 below;

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Tables 2(left) and 3(right). Permeability and Porosity values by formation and age from Sydney Basin onshore wells. From Maung et al, 1997, modified by Sayers, 2004 .

This clearly demonstrates reservoir presence with porosity ranging up to 31% and permeability over 1 Darcy. Best reservoir development is from the Triassic Narrabeen Group.

Offshore an important datapoint is a dredge sample identified as Triassic sediments from offshore (Maung et al, 1997), proving the offshore extent of the proposed sedimentary basin. Another is the Munmorah well recently drilled on the west edge of the block from a surface location onshore correlates directly into the Fish prospect. Initial analysis of this well shows that it drilled a clastic sand-shale sequence with interbedded coals from surface to a total depth of 2227.42 meters.

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Fig. 11, Complete log suite from Munmorah. The section consists almost entirely of clastic rocks; 2 coaly sequences separated by a shaley interval. Resistivity in some sands is unusually high indicating possible gas saturation. There is a downward shift in Facies from coastal plain to offshore silts and shales at -1340, indicating a sequence boundary.

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Sequence Boundary
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Error! Objects cannot be created from editing field codes.

Fig. 12, Log analysis of select interval from -550m to -760 m depth, Munmorah. Gamma curve in green, SP in dark blue, Deep resistivity in Red, Sonic in light Blue, and bulk density in magenta. Gamma shading is yellow indicating possible reservoir SP is shaded in Blue above 320 mv. The few thin intrusives logged are characterized by very high SPs. Resistivity above 20 Ohmm is shaded red. When these high resistivities are found in reservoir indicated by gamma response, these may indicate possible gas-charged zones.

The sands here with distinct bases and fining-upward profiles may represent channel environments and good reservoir development.

Error! Objects cannot be created from editing field codes.

Fig. 13, Log analysis of select interval from -1650m to -1870m depth, Munmorah. The shading and facies analysis is similar to figure 12 above. This deeper interval is for a coaly section and shows correlation of the logged samples with the logs. The interval shows a transition from coarsening-upward shoreface sands (exp., 1790-1800) upward into a coastal plane environments evidenced by the thin coals. These coarsening-upward shoreface environments are expected to be wide-spread and are excellent reservoir candidates. The coals show high resistivity, normal in coal, that may also indicate source potential.

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Error! Objects cannot be created from editing field codes. Fig. 14, Scaled correlation of Munmorah section with the Fish prospect location (projected) and line B4-29. Distance between Munmorah and South Fish II locations is 22 kms.

The correlation suggests that the section at the Fish prospect may be older than the rocks drilled at Munmorah. It is thought that the Munmorah section is similar of overall lithology to the deeper Fish prospect section. These correlations are somewhat speculative but it is a reasonable expectation that there will be sedimentary section drilled at the Fish prospect.

Seal

The Cainozoic section that overlies the Mesozoic unconformity is a system seal. This is evidenced by the proliferation of seeps around the subcrop of the exhumed unconformity, the collocated presence of shallow gas indications, and the seismic chimneys associated with this feature. The unconformity is a long-lived one- developing in the late Jurassic at the break-up of Pangea. It was essentially exposed from Mid-Jurassic to the Cainozoic. It is a major reflection in the seismic dataset and is easily mapped and identified. This amplitude is no doubt due to a velocity and density increase at the unconformity. It also marks the top of the Hydrocarbon system.

There are many interbedded seals in the section below the unconformity that would act as topseals for the prospects mapped. They may be exemplified by the shaley interval in the Munmorah well, and in fact thin shales like the shale that seals the sand at -1790 m, only a few meters thick, seems to be sufficient to seal that sand.

Error! Objects cannot be created from editing field codes.

Fig. 15, Log analysis of interval -1270m to -1490m, Munmorah well, shows possible trapped gas beneath prominent seal formed by a flooding surface/sequence boundary at -1353 m.

In regards to Petroleum Systems elements, this is all good evidence to suggest that there is a working hydrocarbon system in the PEP11 area.

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Prospect Summary

The structure map below is the basis for the assessed prospects. The actual correlation of this reflection with any known stratigraphic section is equivocal as discussed elsewhere, but it is a useful seismic marker and area-wide horizon.

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Prospects list, Mean Reserves
Fish 11.5 Tcfg
Baleen 1.5 Tcfg
Shark 3.5 Tcfg
North Sei 435 Bcfg
West Sei 193 Bcfg
East Sei 327 Bcfg
Trout 624 Bcfg
Humpy 430 Bcfg
Orca 811 Bcfg
Octopus 471 Bcfg
Squid 585 Bcfg
Blue 799 Bcfg
Blue Whale 3.4 Tcfg
S Squid 777 Bcfg
Fig. 16, Leads Map S Humpback 88 Bcfg
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Individual Prospect Reserves and Risks

All of the prospects evaluated here have been evaluated using SPE/AAPG guidelines and are considered Undiscovered Prospective Resources (SPE 2001, 2005, 2008). A probabilistic resource analysis is most applicable for projects such as evaluating the ‘potential’ resources of the subject area, where a great deal of uncertainty exists in the reservoir parameters.

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The uncertainty in the reservoir data is quantified by probability distributions, and an iterative approach yields an expected probability distribution for potential resources. This approach allows consideration of most likely resources for planning purposes, while gaining an understanding of what volumes of resources may have higher certainty, and what potential upside may be for the project. The analysis for this project was carried out considering uncertainty for all parameters in the volumetric equations. A good summary of the principles used in this analysis is summarized in Quirk and Rothrauff, 2008 and use principles and methodology developed and taught by Rose and Associates. All the estimates described herein represent the potential size of hydrocarbon deposits in the prospect areas if discovered to be present in economic quantity, in SPE terms, Undiscovered Prospective Resources. SPE allows use of either deterministic or probabilistic methodologies. While the SEC does not forbid probabilistic analyses, the disclosed quantities must be demonstrated to meet the defined deterministic criteria as they are here.

A Detailed Descriptions of Agencies’ Classifications/Definitions including summary and detailed (tables) comparison to SPE Reserves Definitions may be found in Etherington et al, 2005. Agencies included in the comparison are;

o US Security and Exchange Commission (SEC-1978)

o UK Statement of Recommended Practices (SORP-2001)

o Canadian Security Administrators (CSA -2002)

o Russian Ministry of Natural Resources (RF-2005)

o China Petroleum Reserves Office (PRO–2005)

o Norwegian Petroleum Directorate (NPD–2001)

o United States Geological Survey (USGS-1980)

o United Nations Framework Classification (UNFC-2004)

The output distributions were then used to characterize the Prospective Resources. Prospective resources are defined as “those quantities of oil and gas estimated on a given date to be potentially recoverable from undiscovered accumulations. They are technically viable and economic to recover.”

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Sydney Basin Offshore
Prospective Reserves, Tcfg
All Prospects
Tcfe
0.001 0.01 0.1 1 10 100
0
Fish
10 Baleen
Shark
20
N Sei
30 W Sei
E Sei
40
Trout
50 Humpy
Orca
60
Octopus
70 Squid
Blue
80
Blue Whale
90 S Squid
S Humpback
100
Probability
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Table 4 Prospective reserves distribution, this study, all prospects.

The distribution represents a distribution of possible outcomes given the input distributions of individual prospect parameters. Points may be used to represent individual outcomes, such as the pink

19

square representing the prospect Baleen on the chart above. This point, located at a probability of 10% and 4 Tcf, that is, 90% of the outcomes for this prospect will have reserves less than 4Tcf.

It should be noted that difference between the P90 and P10 cases represents a broad range in possible value between the minimum and maximum expected resources. This is reflective of the high degree of uncertainty associated with any evaluation such as this one prior to actual field discovery, development, and production. These numbers represent percentile in a population, inverse of probability. These populations are produced by Monte Carlo simulation of 500 cases or more, and the sorted by rank from highest reserve outcome ( 99 Percentile) to lowest (1 Percentile). A 10% probability would be equivalent to a 90 Percentile of the population meaning that 90% of the cases have those reserves or less, ie., a high case. Also note that, in general, the high probability resource estimates at the left side of these distributions represents downside risk, while the low probability estimates on the right side of the distributions represent upside potential.

Principle Risks are Seal and Reservoir. There is generally a low Source Risk due to numerous and different observances of hydrocarbons. Risk for each individual prospect is estimated using a 4-element risk matrix; Trap, Seal, Reservoir, and Source and Migration. The prospect risk varies by prospect, and ranges from the least-risky (Fish, 21% COS) to the most risky (Blue Whale, 7.5% COS). Individual Average Prospect COS is 16.6%.

Because of the abundant evidence of a charged gas system there is thought to be a low risk of migration and charge in general, although this varies by fetch area (Blue and Whale) and distance from suspect kitchen (Orca, SEI’s).

Some of the more shallow prospects may have more seal risk, certainly there is much evidence of leakage where the Mesozoic unconformity is breached to the seafloor, both mounds and seismic chimneys. Some of the less well documented or subtle closures have higher trap risk (Blue Whale, Squid).

Key Parameters

For Fish, Baleen, and Shark maps were derived for each of 3 possible cases representing P10, P50, and P90 percentiles. It is important to note that a success at Fish of the P10 area includes the Baleen and Shark prospects. Other prospect areas are map-based for the P50 area andP10 and P90 areas are estimated using a lognormal distribution.

Net intervals that were used for all prospects are 30 ft for P90, 100 ft. for P50 and 200 ft. for P10. These are based on values used in a previous evaluation by Santos and are consistant with field and reported values. Porosity was likewise varied from 10% to 15% to 20% for P90, P50, and P10 cases respectively. Hydrocarbon saturations varied from 60% to 72% to 85% based on analogy with similar clastic reservoirs. Temperatures, pressures and Gas expansion were calculated using a ‘normal’ pressure gradient of .433 psi/ft, temperature gradient of 1.5 degrees F/100 ft. and Boyles Law. Geometric correction factors were estimated from mapped shapes. Recovery is varied from .5 to .75 to .8 for P50 and 200 ft. for P10 cases respectively representing a gas, pressure-depletion production mechanism. References for equations, fluid and gas properties, and other miscellanea can be found at the Texas A&M website at: http://www.pe.tamu.edu/virtuallab/OilFVbelowBP.aspx A complete glossary of terminology is at; http://www.glossary.oilfield.slb.com .

Mean values were calculated from the resulting distributions. The mean is a statistical representation of the average expected successful outcome of a well drilled at the prospect.

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Table 5 - Individual prospect assessment and risking details

Input Values in Red P1 4.23144355 Sum of Means Sum of Means 235.7840106 Bcfg
in-
place
p10 694.5662909 75.55390045
P2 21.19086091 Sum of Means 25.42230446 Tcfg Recoverable P50 65.62631674 6.692563404 25.42230446
P3 206.1302626 Sum, risked means 4.23144355 Tcfg Recoverable p90 3.878655581 0.263696534
Name Case area Net
Interval
Porosity Shc geom
correction
ft2/ac In-place gas
expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
Sydney
Basin
Offshore
acres ft
%
%
Bcfg
Tcfg bblo/Mcfg Mbo
Fish Prospect 10 244780 200 20.0% 85.0% 0.9 43560 326.2760741 135.9731631 0.8 35.49183187 50 1.774591594
50 55528 100 15.0% 72.0% 0.8 43560 20.89842924 135.9731631 0.75 2.131219146 50 0.106560957
90 7162 30 10.0% 60.0% 0.75 43560 0.421168572 135.9731631 0.5 0.028633811 50 0.001431691
Reservoir (Depth, ft): 4395.2 m: 1340
Deg/100 ft: 1.5 psi/ft 0.43300
res temp: 125.928 res
pressure:
1917.2216 Swanson's
Mean:
106.3685445 Gas, Bcfg in-place
surf temp 60 deg F 11.50862736 Gas,
Tcf
recoverable
Mbo
recov
Swanson's
Mean=
0.575431368
surf pressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% Source
Migration
100.0% Total Risk 21.00%
Mounds and BSR indicate charge,
mounds
http://www.pe.tamu.edu/virtuallab/OilFVbelowBP.aspx
Risked
Expected
Outcome:
2.41681175 Tcf risked recoverable http://www.glossary.oilfield.slb.com

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Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Condratio Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
**Baleen ** 10 28920 200 20.0% 85.0% 0.9 43560 38.54850912 135.9731631 0.8 4.193250175 50 0.20966251
50 12302 100 15.0% 72.0% 0.8 43560 4.629961037 135.9731631 0.8 0.472162835 50 0.02360814
90 4299 30 10.0% 60.0% 0.75 43560 0.252806994 135.9731631 0.5 0.017187483 50 0.00085937
Reservoir Depth,ft: 5195.5 m: 1584
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 137.9328 res
pressure:
2263.7602 Swanson's
Mean:
13.4923792 Gas,Bcfgin-place
surftemp 60 degF 1.45199643 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.07259982
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% SourceMigration 90.0% Total Risk 18.90%
better seal preservation at
DHI(mound)
Baleen. Good
Risked
Expected
Outcome:
0.27442733 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Shark 10 73492 200 20.0% 85.0% 0.9 43560 97.96013251 135.9731631 0.8 10.65595926 50 0.53279796
50 36746 100 8.0% 72.0% 0.8 43560 7.375821742 135.9731631 0.8 0.75218536 50 0.03760927
90 18373 30 6.0% 60.0% 0.75 43560 0.648265583 135.9731631 0.5 0.044073361 50 0.00220367
Reservoir Depth,ft: 5149.6 m: 1570
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 137.244 res
pressure:
2243.8768 Swanson's
Mean:
32.5328481 Gas,Bcfgin-place
surftemp 60 degF 3.51088393 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.1755442
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% SourceMigration 80.0% Total Risk 16.80%
Risked
Expected
Outcome:
0.58982850 Tcf riskedrecoverable

22

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
**NSei ** 10 8456 200 20.0% 85.0% 0.9 43560 11.27130682 135.9731631 0.8 1.226076192 50 0.06130381
50 4228 100 15.0% 72.0% 0.8 43560 1.591243315 135.9731631 0.8 0.16227479 50 0.00811374
90 2114 30 10.0% 60.0% 0.75 43560 0.124315884 135.9731631 0.5 0.008451812 50 0.00042259
Reservoir Depth,ft: 5726.9 m: 1746
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 145.9032 res
pressure:
2493.839 Swanson's
Mean:
4.05518414 Gas,Bcfgin-place
surftemp 60 degF 0.43526832 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.02176342
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% SourceMigration 80.0% Total Risk 16.80%
Risked
Expected
Outcome:
0.07312508 Tcf
risked
recoverable
Name Case area Net
Interval
Porosity Shc geom
correction
ft2/ac In-place gas
expansion
factor
Rf Recoverable
Reserves
Condratio Cond
Sydney
Basin
Offshore
acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
**WSei ** 10 3748 200 20.0% 85.0% 0.9 43560 4.995844128 135.9731631 0.8 0.543440583 50 0.02717203
50 1874 100 15.0% 72.0% 0.8 43560 0.705295642 135.9731631 0.8 0.071925959 50 0.0035963
90 937 30 10.0% 60.0% 0.75 43560 0.055101222 135.9731631 0.5 0.003746144 50 0.00018731
Reservoir Depth,ft: 6054.9 m: 1846
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 150.8232 res
pressure:
2635.863 Swanson's
Mean:
1.79740186 Gas,Bcfgin-place
surftemp 60 degF 0.1929264 Gas,
Tcf
recoverable
Mbo recov Swanson's
Mean =
0.00964632
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% Source
Migration
100.0% Total Risk 21.00%
Risked
Expected
Outcome:
0.0405145 Tcf riskedrecoverable http://www.pe.tamu.edu/virtuallab/OilFVbelowBP.aspx
http://www.glossary.oilfield.slb.com

23

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
**ESei ** 10 6358 200 20.0% 85.0% 0.9 43560 8.474807088 135.9731631 0.8 0.921877061 50 0.04609385
50 3179 100 15.0% 72.0% 0.8 43560 1.196443354 135.9731631 0.8 0.12201314 50 0.00610066
90 1589.5 30 10.0% 60.0% 0.75 43560 0.093472137 135.9731631 0.5 0.006354851 50 0.00031774
Reservoir Depth,ft: 6396 m: 1950
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 155.94 res
pressure:
2783.568 Swanson's
Mean:
3.04906111 Gas,Bcfgin-place
surftemp 60 degF 0.32727483 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.01636374
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% SourceMigration 80.0% Total Risk 16.80%
Risked
Expected
Outcome:
0.05498217 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Trout 10 12120 200 20.0% 85.0% 0.9 43560 16.15518432 135.9731631 0.8 1.75733721 50 0.08786686
50 6060 100 15.0% 72.0% 0.8 43560 2.280731904 135.9731631 0.8 0.232588748 50 0.01162944
90 3030 30 10.0% 60.0% 0.75 43560 0.17818218 135.9731631 0.5 0.012113997 50 0.0006057
Reservoir Depth,ft: 6560 m: 2000
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 158.4 res
pressure:
2854.58 Swanson's
Mean:
5.81230271 Gas,Bcfgin-place
surftemp 60 degF 0.62387086 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.03119354
surfpressure 14.1 psi
Risk: Trap 70% Seal 50% Reservoir 60.0% SourceMigration 85.0% Total Risk 17.85%
Risked
Expected
Outcome:
0.11136095 Tcf riskedrecoverable

24

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Humpy 10 8348 200 20.0% 85.0% 0.9 43560 11.12734973 135.9731631 0.8 1.210416752 50 0.06052084
50 4174 100 15.0% 72.0% 0.8 43560 1.570919962 135.9731631 0.8 0.160202217 50 0.00801011
90 2087 30 10.0% 60.0% 0.75 43560 0.122728122 135.9731631 0.5 0.008343865 50 0.00041719
Reservoir Depth,ft: 7652.2 m: 2333
2333
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 174.7836 res
pressure:
3327.5199 Swanson's
Mean:
4.00339134 Gas,Bcfgin-place
surftemp 60 degF 0.42970907 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.02148545
surfpressure 14.1 psi
Risk: Trap 70% Seal 55% Reservoir 60.0% SourceMigration 80.0% Total Risk 18.48%
Risked
Expected
Outcome:
0.07941024 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Orca 10 15750 200 20.0% 85.0% 0.9 43560 20.993742 135.9731631 0.8 2.283668404 50 0.11418342
50 7875 100 15.0% 72.0% 0.8 43560 2.9638224 135.9731631 0.8 0.30225023 50 0.01511251
90 3937.5 30 10.0% 60.0% 0.75 43560 0.231548625 135.9731631 0.5 0.015742199 50 0.00078711
Reservoir Depth,ft: 7242.2 m: 2208
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 168.6336 res
pressure:
3149.9899 Swanson's
Mean:
7.55311615 Gas,Bcfgin-place
surftemp 60 degF 0.81072327 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.04053616
surfpressure 14.1 psi
Risk: Trap 70% Seal 60% Reservoir 60.0% SourceMigration 80.0% Total Risk 20.16%
Risked
Expected
Outcome:
0.16344181 Bcf riskedrecoverable

25

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Octopus 10 9158 200 20.0% 85.0% 0.9 43560 12.20702789 135.9731631 0.8 1.327862555 50 0.06639313
50 4579 100 15.0% 72.0% 0.8 43560 1.723345114 135.9731631 0.8 0.175746515 50 0.00878733
90 2289.5 30 10.0% 60.0% 0.75 43560 0.134636337 135.9731631 0.5 0.009153464 50 0.00045767
Reservoir Depth,ft: 6645.3 m: 2026
2026
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 159.6792 res
pressure:
2891.5062 Swanson's
Mean:
4.39183731 Gas,Bcfgin-place
surftemp 60 degF 0.47140341 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.02357017
surfpressure 14.1 psi
Risk: Trap 60% Seal 55% Reservoir 60.0% SourceMigration 85.0% Total Risk 16.83%
Risked
Expected
Outcome:
0.07933719 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Condratio Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Squid 10 11364 200 20.0% 85.0% 0.9 43560 15.1474847 135.9731631 0.8 1.647721127 50 0.08238606
50 5682 100 15.0% 72.0% 0.8 43560 2.138468429 135.9731631 0.8 0.218080737 50 0.01090404
90 2841 30 10.0% 60.0% 0.75 43560 0.167067846 135.9731631 0.5 0.011358372 50 0.00056792
Reservoir Depth,ft: 5923.7 m: 1806
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 148.8552 res
pressure:
2579.0534 Swanson's
Mean:
5.44975314 Gas,Bcfgin-place
surftemp 60 degF 0.58495614 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.02924781
surfpressure 14.1 psi
Risk: Trap 55% Seal 55% Reservoir 60.0% SourceMigration 75.0% Total Risk 13.61%
Risked
Expected
Outcome:
0.07962716 Tcf riskedrecoverable

26

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
Blue 10 15522 200 20.0% 85.0% 0.9 43560 20.68983259 135.9731631 0.8 2.250609586 50 0.11253048
50 7761 100 15.0% 72.0% 0.8 43560 2.920917542 135.9731631 0.8 0.297874798 50 0.01489374
90 3880.5 30 10.0% 60.0% 0.75 43560 0.228196683 135.9731631 0.5 0.015514312 50 0.00077572
Reservoir Depth,ft: 9075.8 m: 2767
2767
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 196.1364 res
pressure:
3943.9041 Swanson's
Mean:
7.4437758 Gas,Bcfgin-place
surftemp 60 degF 0.79898709 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.03994935
surfpressure 14.1 psi
Risk: Trap 50% Seal 50% Reservoir 60.0% SourceMigration 50.0% Total Risk 7.50%
Risked
Expected
Outcome:
0.05992403 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
BlueWhale 10 66262 200 20.0% 85.0% 0.9 43560 88.32300523 135.9731631 0.8 9.607646718 50 0.48038234
50 33131 100 15.0% 72.0% 0.8 43560 12.46913015 135.9731631 0.8 1.271600301 50 0.06358002
90 16565.5 30 10.0% 60.0% 0.75 43560 0.974150793 135.9731631 0.5 0.066229182 50 0.00331146
Reservoir Depth,ft: 3804.8 m: 1160
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 117.072 res
pressure:
1661.5784 Swanson's
Mean:
31.7767989 Gas,Bcfgin-place
surftemp 60 degF 3.41080289 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.17054014
surfpressure 14.1 psi
Risk: Trap 50% Seal 50% Reservoir 60.0% SourceMigration 50.0% Total Risk 7.50%
Risked
Expected
Outcome:
0.25581022 Tcf riskedrecoverable

27

Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
S Squid 10 15098 200 20.0% 85.0% 0.9 43560 20.12466773 135.9731631 0.8 2.189131782 50 0.10945659
50 7549 100 15.0% 72.0% 0.8 43560 2.841129562 135.9731631 0.8 0.28973803 50 0.0144869
90 3774.5 30 10.0% 60.0% 0.75 43560 0.221963247 135.9731631 0.5 0.015090522 50 0.00075453
Reservoir Depth,ft: 8541.1 m: 2604
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 188.1168 res
pressure:
3712.405 Swanson's
Mean:
7.24044112 Gas,Bcfgin-place
surftemp 60 degF 0.7771619 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.0388581
surfpressure 14.1 psi Risk
Risk: Trap 60% Seal 50% Reservoir 60.0% SourceMigration 75.0% Total Risk 13.50%
Risked
Expected
Outcome:
0.10491686 Tcf riskedrecoverable
Name Case area NetInterval Porosity Shc geomcorrection ft2/ac In-place gas expansion
Factor
Rf Recoverable
Reserves
Cond
ratio
Cond
SydneyBasinOffshore acres ft % % Bcfg Tcfg bblo/Mcfg Mbo
SHumpback 10 1704 200 20.0% 85.0% 0.9 43560 2.271322944 135.9731631 0.8 0.247071172 50 0.01235356
50 852 100 15.0% 72.0% 0.8 43560 0.320657357 135.9731631 0.8 0.032700596 50 0.00163503
90 426 30 10.0% 60.0% 0.75 43560 0.025051356 135.9731631 0.5 0.001703156 50 8.5158E-05
Reservoir Depth,ft: 8692 m: 2650
Deg/100ft: 1.5 psi/ft 0.43300
res temp: 190.38 res
pressure:
3777.736 Swanson's
Mean:
0.81717523 Gas,Bcfgin-place
surftemp 60 degF 0.08771254 Gas,Tcf recoverable Mbo
recov
Swanson's Mean
=
0.00438563
surfpressure 14.1 psi Risk
Risk: Trap 60% Seal 60% Reservoir 60.0% SourceMigration 60.0% Total Risk 12.96%
Risked
Expected
Outcome:
0.01136754 Tcf riskedrecoverable

28

Portfolio Aggregation

SPE recommends that probabilistic aggregation be confined to the field, property or project level. For the purpose of evaluating the combined potential of all prospects in PEP11 it may be useful to aggregate them statistically. Given the effect of the central limit theorem, the arithmetic summation of field Proved volumes in a large portfolio of properties would typically be much less than the P90 of the probabilistic aggregation of the distributions associated with these same properties. This same ‘portfolio effect’ will cause the arithmetic sum of P10 volumes to be much greater than the P10 of the probabilistic aggregate. (The actual variance is a function of the dependencies defined in the probabilistic aggregation model; the mean of the aggregate is not impacted by dependency variations.). The aggregate sum of the P10 and P90 are summed and re-projected to P2 and P98 respectively, and a P50 representing the summed aggregate is taken from this plot;

==> picture [478 x 395] intentionally omitted <==

----- Start of picture text -----

Sydney Basin Offshore
Probabilistic Reserves Assessment
Portfolio Aggregation
Tcfe
0.1 1 10 100 1000
0
x
10
20
30
40
All Prospects, Reserves Sum, Tcfg
50
Aggregate Portfolio
60
70 Aggregate
P50, 4.2 Tcfg
80
90
x
100
Table 6, Portfolio Aggregation.
Sums aggregated
Tcfg Tcfg
98 P98 0.263697
90 P90sum 2 0.263697 0.41
50 P50 5.05 4.25
10 P10 sum 75.5539 47
2 P2 75.5539
mean 24.76528 15.923
Probability
----- End of picture text -----

Table 6, Portfolio Aggregation.

Table 7, Table of Aggregate Portfolio values.

The Mean of the Portfolio Aggregate in this study is 15.9 Tcfg (Table 7). These are “Undiscovered Prospective Reserves” as defined by the SEC and SPE 2005. The problem is that it is impossible to represent a range of values by a single number, especially a distribution that is skewed or dominated by a few large successful outcomes.

29

If there was a discovery, the equivalent classification in terms of a 3P assessment would be: (Low) P1= 410 Bcfg, P2= 4.25 Tcfg, (Best) and P3 (High)= 47 Tcfg, the equivalencies are allowed and defined specifically by the SPE (Etherington, 2005), these are also by those same definitions and guidelines considered “Undiscovered Prospective Reserves”.

Conclusions

“Entirely covered by the PEP 11 permit (200km long, 8,250km[2] ) the offshore Sydney Basin is a significant exploration area with large scale structuring and potentially multi-Tcf gas and condensatecharged Triassic and Permian reservoirs.

The permit has well defined gas prospects and evidence of the potential for oil. PEP 11 contains all the elements for success needed in world class sized structures. Advent Energy Ltd, through wholly owned subsidiary Asset Energy Pty Ltd, is exercising its exclusive option to increase its interest from 25% to 85% in this highly prospective basin.

A rig contract has been finalised for drilling in Q4 2010.

Approximately A$1 million of sub-bottom profiles and swath data collected by the Federal Government in 2006 has been acquired, and reviews have been extremely positive leading to a reassessment of the petroleum prospectivity of the offshore Sydney Basin. Evidence for active gas seepage has been detected along the PEP 11/continental margin, LandSat analysis has revealed streaming slicks clustered over the Baleen prospect, and inshore thermogenic hydrocarbon seepage has been observed and analysed – the offshore Sydney Basin is now considered an active thermogenic hydrocarbon system.

The exploration programme, if successful, could meet Sydney’s gas consumption needs for the next decade; Permit resource estimates also allow for LNG project consideration. If available estimates were to be realised, PEP 11 would be on a par with some of the giant gas reserves in Australia such as those on the North West Shelf. The potential reward from a successful drilling programme makes this a very attractive and exceptional exploration opportunity in an inimitable geographical location.”

The Block is prospective for gas and if successful, could have giant (> 3 Tcfg field size is a possibility) gas potential. Gas production would displace other market sources and supply GTL facilities.

Our conclusion of block potential is based on the aggregate sum of the Prospective Reserves. The Mean of the Portfolio Aggregate is 15.9 Tcfg recoverable. These are “Undiscovered Prospective Reserves” as defined by the SEC and SPE 2005. The equivalent classification in terms of a 3P assessment would be: (Low) P1= 410 Bcfg, P2= 4.25 Tcfg, (Best) and P3 (High)= 47 Tcfg, the equivalencies are allowed and defined specifically by the SPE (Etherington, 2005), these are also by those same definitions and guidelines considered “Undiscovered Prospective Reserves” and assume successful outcomes.

30

Digital Appendix

Excel File “SydneyBasinPEP11block assessmentFinal” Word File “PEP11 Prospectivity Report2010” http://www.spe.org/industry/reserves/mapping.php www.tbberge.com

Bibliography

Alder, J.D., S. Hawley, T. Maung, J. Scott, R.D. Shaw, A. Sinelnikov, and G. Kouzmina, 1998, “Prospectivity of the Offshore Sydney Basin: A New Perspective”, in AAPEA Journal, pp 68 – 92.

Blevin, J., 2001, “Hydrocarbon Prospectivity of Australia’s Remote Frontier Areas in Offshore East and South-East Australia- Examples from the Basins of Lord Howe Rise”, PESA Eastern Australian Basins Symposium, Melborne, Vic., Nov. 2001. Abstract, p 25-35.

Bradley, Graham, 1992, “Evolution and Hydrocarbon Prospectivity of the Offshore Sydney Basin – NSW/P10” report by Bradley Oilsearch.

Clennell, B., Talukder, A., Dariush, N., Rajput, S., and Pevzner, R., 2009, “Advent Energy Seabed Studies Interim Report”, CISRO study, TOPAS data, April, 2009, Part 1, 11 p.

Etherington, John, Pollen Torbjorn, and Luca Zuccolo, 2005, “Comparison of Selected Reserves and Resource Classifications and Associated Definitions” “Mapping” Subcommittee Final Report- December 2005. Sandwell, D.T., and W.H.F. Smith, “Global marine gravity from retracked Geosat and ERS-1 altimetry; Ridge Segmentation versus spreading rate, J. Geophysical Res., 114, BO1411, doi: 10. 1029/2008JB006008.2009

Exon, N.F., Dickens, G.R., Auzende, J-M, Lafoy, Y., Symonds, P.A., and Van de Beuque, S., 1998, “Gas Hydrates and free gas on the Lord Howe Rise, Tasman Sea”, in PESA Journal, no. 26, pp 148 -156.

Gore “Report on sea floor sampling” unpub June 2010

Heggie, D.T., Fredericks, D.J., Bickford, G.P. and Bishop, J.H., 1997, “Light Hydrocarbons and the Deepwater Ocean Outfalls Offshore Sydney, Rig Seismic Survey112” AGSO Record, 120 p.

Kroh, Fred, 2008, “Geophysical Evidence for Gas in the Offshore Sydney Basin” unpub. Manuscript, 20 p.

Sayers, J., A. Kernich and T. Dance, 2004, “Geosequestration investigations- offshore New South Wales, Australia” PESA Eastern Australasian Basins Symposium II, Adelaide, 19-22 Sept., 2004, p. 389- 401.

Maung, T, Alder, D., Shaw, R. and Hawley, S., 1997, “Offshore Sydney Basin” Canberra, Bureau of Resource Sciences, Petroleum Prospectivity Bulletin 1997/1.

O’Brien, G.W., Lawrence, G.M., Williams, A.K., Glenn, K., Barrett, A.G., Lech, M., Edwards, D.S., Cowley, R., Boreham, C.J., and Summons, R.E., 2004, “Yampi Shelf, Browse Basin, North-West Shelf, Australia: a test-bed for constraining hydrocarbon migration and seepage rates using combinations of 2D and 3D seismic data and multiple, independent remote sensing technologies” in Marine and Petroleum Geology, vol 22, (2005) , pub. Elsevier Ltd., pp 517-549.

Quirk, David G., and Richard G. Ruthrauff, 2008, “Toward consistency in petroleum exploration: A systematic way of constraining uncertainty in prospect volumetrics”, in AAPG bull v. 92, NO. 10 (October 2008), pp. 1263-1291.

31

CONSENT LETTER

Pangean Resources LLC hereby consents to the use of all or any part of this Resource Evaluation Report, for the Advent Energy Ltd. Block PEP11 offshore Australia as of 15 November 2010, In any document filed with any Securities Commission by Advent.

This document is fully compliant with SEC, SPE, and AAPG reserves estimation guidelines and Industry Best Practices.

==> picture [257 x 194] intentionally omitted <==

Company name: Pangean Resources LLC Company address: 2036 Ogden St. Denver, CO 80205

Company phone no.; 303-894-8811 Company EIN: 26-2760041 Authorizing Official: Timothy Berge Title: President

==> picture [136 x 127] intentionally omitted <==

32