km t 2 4 Fig Tectonic divisions of Siberian platform

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31 1 2012 3 GLOBAL GEOLOGY Vol. 31 No. 1 Mar. 2012 1004 5589 2012 01 0139 09 1 1 2 1 1 1 1. 130061 2. 130061 - P168. 130. 2 A doi 10. 3969 /j. issn. 1004-5589. 2012. 01. 017 Reserch on hydrocarbon accumulation condition and distributive regulation of Siberian platform Russia TAO Gao-qiang 1 DONG Qing-shui 1 2 NIE Hui 1 ZHANG Kai-wen 1 LOU Ren-xing 1 1. College of Earth Sciences Jilin University Changchun 130061 China 2. Oil-shale Laboratory Center Jilin University Changchun 130061 China Abstract Siberian platform of Russia has tremendous potential prediction in hydrocarbon but poor in exploration research. The platform is one of the important target areas of overseas hydrocarbon exploration and for the CNPC. On the basis of the types of tectonic units the comprehensive analysis results of hydrocarbon accumulation condition trap type and hydrocarbon distribution characteristics show that the key factors that controlling the hydrocarbon distribution of Siberian platform are tectonic action and the characteristics of strata and source rocks the model of hydrocarbon accumulation is characterized by being generated and reserved indigenously. Hydrocarbon reservoirs mainly distributed in uplifted areas of cratonic margin without shield and depressions of continental margin the former hydrocarbon enriched layer lay in Permian- Jurassic and the latter in Vendian-Cambrian. The main type of hydrocarbon reservoir is stratigraphical-structural composite. Key words Siberian platform hydrocarbon accumulation condition distribution rule accumulation model 0 78 ~ 120 E 55 ~ 80 N 2011-10-27 2012-02-13 GT-YQ-QQ-2008-2-07 1963-. E-mail dqs9518@ 163. com

140 31 6. 3 10 6 km 2 1 1. 1 1 1 19 20 1 20 20 30 2 50 60 t 2 4 Fig. 1 1 2 Tectonic divisions of Siberian platform

1 141 6 2 000 ~ 4 000 m 3 4 1 4 000 m - 6 500 m 5 1. 2 16 ~ 6. 5 a 6. 5 ~ 5. 7 a 6 7 6 000 ~ 8 000 m 7 8 9-3 7 600 m 10 000 ~ 14 000 m 7 000 m 2 1 400 m 50 m 2. 1 1 300 ~ 2 200 m 290 ~ 1 860 m 768 10 ~ 1 781 m 2. 1. 1 50 ~ 845 m 100 ~ 2 000 m 2 1 500 ~ 3 000 m 0. 5% ~ 3% Ro > 0. 85%

142 31-150 6 000 m ~ 2 000 m 0. 2% ~ 1% ~ 10% Ro > 0. 5% 1% Ro 0. 57% ~ 1. 18% 2% 0. 1% ~ 1% Ro 0. 1% ~ 1% Ro 0. 45% ~ 1. 15% 0. 76% ~ 1. 18% 195 ~ 330 m 0. 1% ~ 0. 5% Ro 0. 45% ~ 0. 85% Fig. 2 2 Distribution of hydrocarbon source rocks in Lifei System of Siberian platform 2. 1. 2 < 0. 2% Ro 0. 57% ~ 0. 76% - 2. 1. 3 125 ~ 750 m 0. 05% ~ 0. 5% Ro 0. 5% ~ 0. 86%

1 143 2. 2. 2 3 749 m 1% ~ 2% Ro 0. 54% ~ 0. 76% 930 m 0. 12% ~ 0. 6% 168 ~ 2 250 m 0. 5% ~ 1. 08% 370 ~ 1 397 m 0. 52% ~ 1. 07% 2% ~ 20% 1 ~ 100 10-3 μm 2 2. 2 5% ~ 20% 1 ~ 100 10-3 μm 2 2. 2. 1 2. 2. 3 - - 11. 2% ~ 5. 5% 25% < 100 10-3 μm 2 1. 5% ~ 18% 2% ~ 7% 10% ~ 12% 20% 20 ~ 30 10-3 μm 2-1 ~ 88 10-3 μm 2 15 ~ 20 m 2. 5% ~ 23. 6% 1 ~ 72. 4 10-3 μm 2 153 ~ 240 m 2. 7% ~ - 28. 2% 350 10-3 μm 2 6. 8% ~ 23. 9% 5. 5 ~ 15 2. 3 10-3 μm 2 6. 5% ~ 16% 63 2% ~ 15% 1 1 ~ 10 10-3 μm 2-52 1% ~ 15% 1 ~ 10 10-3 μm 2 17. 5% 11 3% ~ 14% - 22 ~ 56 m 2. 3% ~ 23. 7% 82. 5%

144 31 Table 1 1 Trap types of founded oil and gas fields in Siberian platform - - - - - 3 0 0 0 0 0 3 0 0 0 0 0 0 0 0 0 0 0 0 0 19 2 0 1 0 0 30 3 0 0 0 2 3 0 2 1 0 0 0 6 3 0 0 0 0 0 12 0 0 0 0 0 24 2 0 0 0 0 0 10 0 0 0 0 0 52 4 1 1 2 3 63 30 21 47. 6% - 24 38% - - 3 2. 4 3 1 000 ~ 2 000 m 3 3. 1 1 63 30 24

1 145 1-2 14 km 13 3. 2 12 1 63 52-4 3 - - 2-3. 3-1 91% 15 1 16 4-14 2 63 1 93% - 3

146 31 Fig. 3 3 East-west regional geological cross-section of Siberian platform Fig. 4 4 Hydrocarbon reservoir formation model of Siberian platform 4 1 2 3

1 147 9 711-720. 9 Ulmishek F. Petroleum geology and resources of the Baykit High Province East Siberia Russia R. U S Department of the Interior. U S Geological Survey 2001. 10. 3 M. 1999 1-137. XIAO De-ming WANG Rong-hua CAI Tian-cheng et al. Oil and gas basins of Russia's East Siberia and the Far East M. Beijing Petroleum Industry Press 1999 1-137. 1 Khudoley A K Rainbird R H Stern R A et al. Sedimentary evolution of the Riphean-Vendian basin of southeastern Siberia J. Precambrian Research 2001 111 1 /4 129-163. Health Publishing House 1991 248-271. 2. M. 12. 2000 17-25. J. 2007 2 LI Guo-yu. Atlas of global fields M. Beijing Petroleum Industry 33-38. Press 2000 17-25. 3. M. 2004 138-163. TONG Xiao-guang XU Shu-bao. Atlas of the global oil exploration and development M. Beijing Petroleum Industry Press 2004 138-163. 4. M. 1992 1-11. GAN Ke-wen. An explication for the sedimentary basin and petroleum distribution map of the world M. Beijing Petroleum Industry Press 1992 1-11. 5. J. 1993 18 6 699-814. LIU He-fu. The geodynamic classification of the sedimentary basins and analysis of structural styles J. Earth Science 1993 18 6 699-814. rocks and the oil-source correlation in Bayanhushu sag of 6 А D. M. Hailaer Basin J. Global Geology 2011 30 2. 1959 110-129. 231-237. Archangel Chomsky А D. The geological structure and history of Soviet Union M. ZHOU Yu-fan translated. Beijing Geological Publishing House 1959 110-129. 1996 1 1 18-24. HE Deng-fa. The oil and gas geological theory and prac- 7. tice of cratonic basins J. Explorationists 1996 1 M. 2007 56-84. WANG Zhi-xin JIN Zhi-jun. The oil and gas geologic feature of Siberian platform and the depression of its edge M. Beijing Chinese Petrochemical Publishing House 2007 56-84. 8 Khomentovsky V V. The Upper Riphean of the Yenisei range J. Russian Geology and Geophysics 2007 48 11 S P. M.. 1991 248-271. Maksimov S P. The manual of oil and gas field Soviet Union M. MAO Yi-kang YANG Wei-dong translated. Urumqi Xinjiang Science and Technology and XU Shu-bao WANG Su-hua. Petroleum geologic features and resource potential of East Siberian oil and gas basins J. Petroleum Technology Forum 2007 2 33-38. 13. J. 2010 29 2 271-276. CUI Xue-hui LIU Zhong-bao YANG Sheng-bin. Application of Cambrian -Ordovician carbonate sequence stratigraphyon petroleum exploration in Tarim Basin J. Global Geology 2010 29 2 271-276. 14. J. 2011 30 2 231-237. BAI Xue-feng ZHANG Hai-qiao. Evaluation on source 15. J. 1 18-24. 16. J. 2003 18 4 561-568. XIE Fang-ke CAI Zhong-xian. Analysises of basal structural features and differences in accumulation of oil and gas of cratonic basins J. The development of Earth Sciences 2003 18 4 561-568.