NORTH SUMATRA MERGUI BASIN CROSS BORDER CASE STUDY EPPM-CCOP PROGRESS REVIEW INDONESIAN TEAM STUDY
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1 NORTH SUMATRA MERGUI BASIN CROSS BORDER CASE STUDY EPPM-CCOP PROGRESS REVIEW INDONESIAN TEAM STUDY P1W3 2-5 AUGUST LANGKAWI, MALAYSIA
2 PROGRESS REVIEW GRAVITY MAP OF NORTH SUMATRA BASIN INDONESIAN SEISMIC INTERPRETATION INDONESIAN WELLS DATA ANALYSIS SEISMIC & MAP INTEGRATION PRELIMINARY BASIN MODELING SOME IDEA FOR THE NEXT
3 GENERAL BASIN OUTLINE & PHYSIOGRAPHY
4 GRAVITY MAP OF NORTH SUMATRA BASIN
5 Basin Dimension : 3 Main Depocenter (Graben/Sub Graben) Width : Km Length : Km Several faults are a sub basin boundary Within the main basin
6 INDONESIAN SEISMIC INTERPRETATION
7 SEISMIC LINES & WELLS LOCATION MAP 12 Seismic Lines 2 Wells
8 SEISMIC LINES SUMMARIES NO. LINE SP INTERVAL (m) SP POSITION RANGE Total SP LENGTH (m) 1 123A B /EXT C A NSO NSO (-11) NSO NSO TOTAL 1,156,307.8
9 Line NSO & Well NSB C-1 NSB C-1 CMP CMP Shot Shot 0 0 Julu Rayeu Top Seurula Top Keutapang Top Baong Top
10 Line & Well GPM-1
11 INDONESIAN WELLS DATA ANALYSIS
12 Wells : 1.Gleumpang Minyeuk-1 2.NSB-C1 WELL SUMMARY
13 Gleumpang Minyeuk-1 NSB-C1
14 Gleumpang Minyeuk-1 BIOSTRATIGRAPHIC ANALYSIS Sequence Boundary Candidate : 1. Top Basement 2. Upper Middle Miocene 3. Mid Upper Pliocene 4. Plio-Pleistocene 5. Mid Lower Pleistocene Top Upper Miocene Horizon Miocene Unconformity Horizon Top Syn Rift Horizon Basement Horizon
15 Gleumpang Minyeuk-1 Quick Look on Wireline Log Top Upper Miocene Horizon Miocene Unconformity Horizon Top Syn Rift Horizon Basement Horizon
16 Gleumpang Minyeuk-1 VITRINITE REFLECTANCE RESULTS Range : 0.21 % % Sea Bottom Temperature : 50 F (10 C) at 456 SS BHT : 138 F (58.9 C) at 1436 m ( m) Avg Geothermal gradient : 2.76 F/100ft or C/100 m
17 Gleumpang Minyeuk-1 VITRINITE REFLECTANCE PROFILE SEQUENCE BOUNDARY? SEQUENCE BOUNDARY?
18 SEISMIC SECTIONS & MAP INTEGRATION
19 SEISMIC LINES BASE MAP DATUM : WGS 1984
20 AGREEMENTS a. Sea bed blue b. Top Upper Miocene Green c. Miocene Unconformity Yellow d. Top Syn rift Orange e. Basement red/purple a. Maps 1: 500,000 b. Seismic sect ions 5cm/sec, vertical up to 6 sec.
21 COMPOSITE LINE INDONESIA THAILAND A A A A
22 B COMPOSITE LINE THAILAND MALAYSIA IND B B B
23 W9-C-1 BASEMENT SIKAO-1 SINGA BESAR-1 LANGGUN TIMUR-1 GPM-1 NSB C km BASEMENT, Time Structure Map (ms) CCOP MERGUI BASIN EPPM P1W3: Basin Analysis (cross border CS) Indonesia Malaysia Thailand
24 W9-C-1 TOP SYN RIFT SIKAO-1 SINGA BESAR-1 LANGGUN TIMUR-1 GPM-1 NSB C km Top Synrift, Time Structure Map (ms) CCOP MERGUI BASIN EPPM P1W3: Basin Analysis (cross border CS) Indonesia Malaysia Thailand
25 W9-C-1 MIOCENE UNCONFORMITY SIKAO-1 SINGA BESAR-1 LANGGUN TIMUR-1 GPM-1 NSB C km Miocene Unconformity, Time Structure Map (ms) CCOP MERGUI BASIN EPPM P1W3: Basin Analysis (cross border CS) Indonesia Malaysia Thailand
26 W9-C-1 TOP UPPER MIOCENE SIKAO-1 SINGA BESAR-1 LANGGUN TIMUR-1 GPM-1 NSB C km Top Upper Miocene,Time Structure Map (ms) CCOP MERGUI BASIN EPPM P1W3: Basin Analysis (cross border CS) Indonesia Malaysia Thailand
27 W9-C-1 SEA BED SIKAO-1 SINGA BESAR-1 LANGGUN TIMUR-1 GPM-1 NSB C km SEABED, Time Structure Map (ms) CCOP MERGUI BASIN EPPM P1W3: Basin Analysis (cross border CS) Indonesia Malaysia Thailand
28 PRELIMINARY BASIN MODELING USING TEMIS 2D
29 MODELING PARAMETER (Derived from GM-1 Well) STRATIGRAPHIC FRAMEWORK HORIZON AGE Average TEMPERATURE GRADIENT Sea Bottom TEMPERATURE HISTORY (MYA) ( C /m) ( C ) Sea bottom Top Upper Miocene 5.3 Top Miocene Unconformity Top Syn Rift 20.4 Top Basement 65
30 ROCKS PROPERTIES FOR MODELING INPUT
31 TYPYCAL SOURCE ROCK FOR MODELING INPUT Shales & mudstones of Bampo & Peutu Formation were dominantly tipe III kerogen with TOC range from 0.5 % to 3 %. Buck & Mc. Culloh (1994)
32 2D PRELIMINARY BASIN MODELING FROM COMPOSITE LINE INDONESIA & THAILAND A INDONESIA THAILAND A Projected Well GPM-1 (280 ft) A A
33 SW Projected Gleumpang Minyeuk-1 Sea level E Sea Bottom Top Upper Miocene Top Upper Miocene Layer Top Miocene Unconformity Top Upper Miocene Layer Top Syn Rift Top Syn Rift - Top Basement Present day (0 Ma)
34 A B SW GM-1 Sea level E SIMPLIFIED BURIAL HISTORY MODEL Present day (0 Ma) 5.3 Ma Ma A 13.8 Ma B Sea Bottom Top Upper Miocene Top Upper Miocene Layer Top Miocene Unconformity Top Upper Miocene Layer Top Syn Rift Top Syn Rift - Top Basement 20.4 Ma
35 Modeling Verification Ro measurement Not fit yet Calculated Ro
36 MATURATION MODEL SW Projected Gleumpang Minyeuk-1 Sea level E Possible HC Migration Present day (0 Ma)
37 RECOMMENDATION FOR THE NEXT MODELING Need more data/info to complete - Need more Facies/lithology distribution/interpretation along seismic section - Need more layer/horizon to define - Need Well data/information from another country (VR, TOC, HI, BHT, TG, HF)
38 SOME IDEA FOR THE NEXT
39 EXAMPLE FROM SIMEULUE WHY WE NEED GRAVITY MODEL/MAP TO DELINIATE BASIN BOUNDARY & KITCHEN AREA (Sediment Thickness) COMBINE WITH BASIN MODELING ROUGHLY ESTIMATED HYDROCARBON GENERATED FROM KITCHEN AREA
40 SIMEULUE AREA MAP
41 SEISMIC LINE USED FOR BASIN MODELING
42 Speculative Modeling Line BGR06_139 Vitrinite Reflectance (Ro) Model Ro = 0.6 Ro = 0.6 (at depth ~ 5000 m) Ro = 0.6 (at depth ~ 5000 m), top of EF_1 Sediment (24 Ma/ Late Oligocene)
43 Sediment Thickness Map derived from Gravity Model Sedime ent thickness Simeulue basin Boundary
44 A B D C E Sedime ent thickness F Simeulue basin Boundary
45 SPECULATIVE AMOUNT OF HYDROCARBON GENERATED Ro = 0.6 A B D C E Ro = 0.6 (at depth ~ 5000 m) Ro : 0.6 F Scenario 1
46 THANK YOU
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