HYDROCARBON ACCUMULATION MODEL AND FUTURE EXPLORATION IN NORTHWEST SABAH BASIN
-
摘要: 以油气地质理论为指导, 在构造、沉积、石油地质特征分析基础上, 从典型油气藏解剖入手, 构建了西北沙巴盆地3种类型的油气成藏模式, 即岩性型、地层型和滚动背斜型油气成藏模式。盆地经历了裂谷期、挤压反转期和拗陷期3个演化阶段, 发育Stage Ⅰ、StageⅡ、StageⅢ、StageⅣ等4套新生代沉积地层。盆地以StageⅣ泥/页岩为主要烃源岩; 有利储集层为由StageⅣC、StageⅣD、StageⅣE砂岩构成的上砂岩单元、由StageⅣA砂岩构成的下砂岩单元及StageⅣC/ⅣD地层滑塌形成的深水浊积砂体; 空间配置方面, 烃源岩与储集体平面相接、空间叠置, 为油气运移成藏提供了有利条件。通过油气富集条件及分布规律的综合分析, 认为"内带"构造区的地层油气藏及"外带"构造区的岩性油气藏是盆地未来的油气勘探重点。Abstract: Guided by hydrocarbon geological theory, through typical reservoir dissecting, it identifies the features of Northwest Sabah Basin reservoir. The result shows that three different hydrocarbon accumulation patterns can be built based on the research for characteristic of structure, sedimentary formation and petroleum geology. They are lithologic, stratigraphic and rollover anticline type, respectively. The basin tectonic evolution involved rift, compression and inverse stage, depression stages and it developed four Cenozoic formations: Stage Ⅰ, StageⅡ, StageⅢ, StageⅣ. Mudstones and shales in the StageⅣ are the main source rocks. The pretty reservoir is provided by the Stage ⅠVA Lower Sandstone Unit, Stage ⅣC, ⅣD and ⅣE Upper Sandstone Unit and Stage ⅣC/ⅣD slump turbidite fan. Three reservoir-seal combinations, called lower, upper, deep-water turbidite fan combinations, are identified in basin. It builds three hydrocarbon accumulation models, named Updip sandstone pinchout, Unconformity and Rolling anticline type which distribute in different tectonic area in this basin. The fundamental conditions of hydrocarbon accumulation are analyzed. It shows that hydrocarbon source rocks and reservoir contacting each other in the plane and superimposing in the space provides favorable conditions for hydrocarbon migration and accumulation. Based on the above analysis, it suggests that stratigraphic reservoir in Inboard belt and lithologic reservoir in Outboard belt will be the future exploration targets for basin.
-
图 1 西北沙巴盆地构造要素[2]
Figure 1. Structural elements of the Northwest Sabah Basin
图 2 西北沙巴大陆边缘演化[3]
Figure 2. Schematic sections showing evolution of the northwestern Sabah continental margin
图 4 氢指数与岩石热裂解峰温(Tmax)交会图[4]
Figure 4. Hydrogen index VS pyrolysis Tmax cross-plots
图 6 岩性型油气成藏模式(据文献[7]修改)
Figure 6. Lithologic hydrocarbon accumulation pattern
图 7 地层型油气成藏模式(据文献[4]修改)
Figure 7. Stratigraphic hydrocarbon accumulation pattern
图 8 滚动背斜型油气成藏模式(据文献[6]修改)
Figure 8. Rollover anticline hydrocarbon accumulation pattern
-
[1] 张翀, 吴世敏, 丘学林.南海南部海区前陆盆地形成与演化[J].海洋地质与第四纪地质, 2007, 27(1):61~70. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200701012.htmZHANG Chong, WU Shi-min, QIU Xue-lin. Formation of foreland basin in the south of the South China Sea[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 61~70. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200701012.htm [2] Abbott W O, Alder K E, Boodoo W, et al. North Borneo regional study: Offshore Sabah[R]. Occidental Malaysia, Inc., 1990: 90~102. [3] Hazebroek H P, Tan D N K, Lamy J M. Tectonic evolution of the NW Sabah continental margin since the Late Eocene[J]. Bulletin of the Geological Society of Malaysia, 1990, 27: 241~260. http://www.gsm.org.my/products/702001-101074-PDF.pdf [4] Mazlan B H M, Leong K M, Azlina A. The petroleum geology and resources of Malaysia [M]. Kuala Lumpur: Petroliam Nasional Berhad, 1999: 499~542. [5] 张厚福, 方朝亮, 高先志, 等.石油地质学[M].北京:石油工业出版社, 1999:228~271.ZHANG Hou-fu, FANG Chao-liang, GAO Xian-zhi. Petroleum Geology[M]. Beijing: Petroleum Industry Press, 1999, 228~271. [6] 徐思煌, 郑丹, 朱光辉, 等.缅甸安达曼海弧后坳陷天然气成藏要素及成藏模式[J].地球科学与环境学报, 2012, 34(1):29~34. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201201006.htmXU Si-huang, ZHENG Dan, ZHU Guang-hui, et al. Main controlling factors and models of gas accumulation in back-arc depression of Andaman Sea, Burma[J]. Journal of Earth Sciences and Environment, 2012, 34 (1): 29~34. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201201006.htm [7] Johnson H D, Chapman J W, Ranggon J. Structural and stratigraphic configuration of the Late Miocene Stage C reservoirs in the St. Joseph Field, offshore Sabah, NW Borneo[J]. Bulletin of the Geological Society of Malaysia, 1989, 25: 79~118. [8] Brcce L, Awang K. Slumping at the Late Miocene shelf-edge offshore West Sabah: A view of a Turbidite Basin margin[J]. Bulletin of the Geological Society of Malaysia, 1985, 18(12): 1~29. http://gsm.org.my/products/702001-101146-pdf.pdf [9] 王先德, 王友启, 刘书权, 等.二连盆地白音查干凹陷油气成藏模式及勘探方向研究[J].石油实验地质, 2012, 34(3):291~295. doi: 10.11781/sysydz201203291WANG Xian-de, WANG You-qi, LIU Shu-quan, et al. Hydrocarbon accumulation pattern and exploration direction in Baiyinchagan sag of Erlian Basin[J]. Petroleum Geology & Experiment, 2012, 34(3): 291~295. doi: 10.11781/sysydz201203291 [10] 易士威, 王元杰, 钱铮.二连盆地乌里雅斯太凹陷油气成藏模式及分布特征[J].石油学报, 2006, 27(3):28~31. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200603005.htmYI Shiwei, WANG Yuan-jie, QIAN Zheng. Forming pattern and distribution features of hydrocarbon reservoir in Wuliyasitai sag of Erlian Basin[J]. Acta Petrolei Sinica, 2006, 27(3): 28~31. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200603005.htm [11] 何登发.不整合面的结构与油气聚集[J].石油勘探与开发, 2007, 34(2):142~149. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200702002.htmHE Deng-fa. Structure of unconformity and its control on hydrocarbon accumulation[J]. Petroleum Exploration and Development, 2007, 34(2): 142~149. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200702002.htm [12] 宋国奇, 卓勤功, 孙莉.济阳坳陷第三系不整合油气藏运聚成藏模式[J].石油与天然气地质, 2008, 29(6):716~720. doi: 10.11743/ogg20080602SONG Guo-qi, ZHUO Qin-gong, SUN Li. Hydrocarbon migration and accumulation patterns in the Tertiary unconformity reservoirs of the Jiyang depression[J]. Oil & Gas Geology, 2008, 29(6): 716~720. doi: 10.11743/ogg20080602 [13] 吴孔友, 查明, 肖敦清, 等.黄骅坳陷埕北断坡不整合特征与油气成藏[J].古地理学报, 2008, 10(5):545~554. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200805018.htmWU Kong-you, ZHA Ming, Xiao Dun-qing, et al. Characteristics of unconformity and hydrocarbon accumulation in Chengbei fault slope of Huanghua depression[J]. Journal of Palaeogeography, 2008, 10(5): 545~554. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200805018.htm [14] 张以明, 王余泉, 刘井旺, 等.冀中坳陷复杂断块油藏成藏模式研究[J].中国石油勘探, 2006, 11(2):15~18. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY200602002.htmZHANG Yi-ming, WANG Yu-quan, LIU Jing-wang, et al. Complicated fault-block reservoir accumulation model research of Gizhong depression [J]. China Petroleum Exploration, 2006, 11(2): 15~18. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY200602002.htm [15] 付广, 付晓飞.断裂输导系统及其组合对油气成藏的控制作用[J].世界地质, 2001, 20(4):344~349. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ200104005.htmFU Guang, FU Xiao-fei. Controlling of fault transport system and its combination to the formation and distribution of oil or gas reservoirs[J]. Word Geology, 2001, 20(4): 344~349. http://www.cnki.com.cn/Article/CJFDTOTAL-SJDZ200104005.htm