天然气地球科学 ›› 2010, Vol. 21 ›› Issue (1): 5461.doi: 10.11764/j.issn.1672-1926.2010.01.54
曾萍
ZENG Ping
摘要:
下扬子区是南方海相具有油气勘探远景的地区之一。应用新增的勘探资料,采用新的技术方法,结合野外、室内综合研究,分析烃源岩构造—热演化。研究结果表明,晚印支—早燕山期,下扬子区的构造运动以逆冲推覆为主,大部分地区遭到抬升剥蚀,部分地区下古生界烃源岩抬升后晚期没有再度深埋,保留了印支期的热演化状况,因此下古生界高成熟腐泥型烃源岩现今仍具有一定的生烃潜力。在演化程度普遍较高的下扬子区下古生界,找到局部热演化程度相对较低,具有油气勘探前景的地区和层位是可能的。
中图分类号:
[1]Dai Jinxing, Qin Shengfei, Tao Shizhen,et al.Developing trends of natural gas industry and the significant progress on natural gas geological theories in China[J].Natural Gas Geoscience, 2005,16(2):127-142.[戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重要进展[J].天然气地球科学,2005,16(2):127-142.]
[2]Zhang Shuichang,Liang Digang,Zhu Guangyou,et al.Fundamental geological elements for the occurrence of Chinese marine oil and gas accumulations[J].Chinese Science Bulletin,2007,2007,52(Supplement I):19-31.[张水昌,梁狄刚,朱光有,等.中国海相油气形成的地质基础[J].科学通报,2007,52(增I):19-31.]
[3]Zhu Guangyou,Zhao Wenzhi,Liang Yingbo,et al.Discussion of gas enrichment mechanism and natural gas origin in marine sedimentary basin,China[J].Chinese Science Bulletin,2007,52(Supplement I):46-57.[朱光有,赵文智,梁英波,等.中国海相沉积盆地富气机理与天然气的成因探讨[J].科学通报,2007,52(增I):46-57.]
[4]Zhang Shuichang,Liang Digang,Zhang Dajiang.Evaluation criteria for Paleozoic effective hydrocarbon source rocks[J].Petroleum Exploration and Development, 2002,29(2):8-12.[张水昌,梁狄刚,张大江.关于古生界烃源岩有机质丰度评价标准[J].石油勘探与开发,2002,29(2):8-12.]
[5]Li Jinchao,Ma Yongsheng,Zhang Dajiang,et al.Problems of exploration of marine oil and gas in China[J].Petroleum Exploration and Development, 1998,25(5):1-2.[李晋超,马永生,张大江,等.中国海相油气勘探若干重大科学问题[J].石油勘探与开发,1998,25(5):1-2.]
[6]Zhang Shuichang,Zhu Guangyou.Gas accumulation characteristics and exploration potential of marine sediments in Sichuan basin[J].Acta Petrolei Sinica,2006,27(5):1-8.[张水昌,朱光有.四川盆地海相天然气富集成藏特征与勘探潜力[J].石油学报, 2006,27(5):1-8.]
[7]Ma Yongsheng,Guo Tonglou,Zhu Guangyou,et al.Simulated experiment evidences of the corrosion and reform actions of H2S to carbonate reservoirs:An example of Feixianguan formation,east Sichuan[J].Chinese Science Bulletin,2007,52(Supplement I):136-141.[马永生,郭彤楼,朱光有,等. 硫化氢对碳酸盐储层溶蚀改造作用的模拟实验证据——以川东飞仙关组为例[J].科学通报, 2007, 52(增I):136-141.]
[8]Jin Zhijun.Particularity of petroleum exploration on marine carbonate strata in China sedimentary basins[J].Earth Science Frontiers,2005,12(3):15-22 .[金之钧.中国海相碳酸盐岩层系油气勘探特殊性问题[J].地学前缘,2005,12(3):15-22.]
[9]Luo Ping,Qiu Yinan,Jia Ailin,et al.The present challenges of Chinese petroleum reservoir geology and research direction[J].Acta Sedimentologica Sinica, 2003,21(1):142-147.[ 罗平,裘怿楠,贾爱林, 等.中国油气储层地质研究面临的挑战和发展方向[J].沉积学报,2003,21(1):142-147.]
[10]Zhu Guangyou, Zhang Shuichang, Liang Yingbo. Formation mechanism and distribution prediction of high-quality marine reservoir in deeper Sichuan basin[J]. Petroleum Exploration and Development, 2006, 33(2):161-166[朱光有,张水昌,梁英波.四川盆地深部海相优质储集层的形成机理及其分布预测[J].石油勘探与开发,2006,33(2):161-166.]
[11]Ma Yongsheng, Guo Xusheng,Guo Tonglou,et al.Discovery of the large-scale Puguang gas field in the Sichuan basin and its enlightenment for hydrocarbon prospecting[J]. Geological Review,2005, 51(4):477-480.[马永生,郭旭升,郭彤楼,等.四川盆地普光大型气田的发现与勘探启示[J].地质论评, 2005, 51(4):477-480.]
[12]Zhou Xinyuan,Wang Zhaoming,Yang Haijun,et al.Cases of discovery and exploration of marine fields in China(Part 5):Tazhong Ordovician condensate field in Tarim basin[J]. Marine Origin Petroleum Geology,2006, 11(1):45-51.[周新源,王招明,杨海军,等. 中国海相油气田勘探实例之五——塔中奥陶系大型凝析气田的勘探和发现[J].海相油气地质,2006, 11(1):45-51.]
[13]Kang Yuzhu. Palaeokarst of Cambro-Ordovician and oil-gas distribution in Tarim basin[J].Xinjiang Petroleum Geology,2005,26(5):472-480.[康玉柱.塔里木盆地寒武—奥陶系古岩溶特征与油气分布[J].新疆石油地质,2005,26(5):472-480.]
[14]Ma Yongsheng.Generation mechanism of Puguang gas field in Sichuan basin[J].Acta Petrolei Sinica,2007,28(2):9-14,21.[马永生.四川盆地普光超大型气田的形成机制[J].石油学报,2007,28(2):9-14,21.]
[15]Zhao Xuefeng,Zhu Guangyou,Liu Qinfu,et al.Main control factors of pore development in deep marine carbonate reservoirs[J].Natural Gas Geoscience, 2007,18(4):514-521.[赵雪凤,朱光有,刘钦甫,等. 深部海相碳酸盐岩储层孔隙发育主控因素研究[J].天然气地球科学,2007,8(4):514-521.]
[16]Chen Anding,Liu Dongying,Liu Ziman. Demonstration and quantification analysis of late hydrocarbon generation of Mesozoic-Paleozoic marine source rocks in the lower Yangzi sedimentary region[J]. Marine Origin Petroleum Geology ,2001,6(4):27-33.[陈安定,刘东鹰,刘子满.江苏下扬子区中、古生界烃源岩晚期生烃的论证与定量研究[J].海相油气地质,2001,6(4):27-33.]
[17]Qin Jianzhong, Li Zhiming, Liu Baoquan,et al.The potential of generating heavy oil and solid bitumen of exceuent marine source rocks[J]. Petroleum Geology & Experiment, 2007,29(3):280-285,291.[ 秦建中,李志明,刘宝泉,等.海相优质烃源岩形成重质油与固体沥青潜力分析[J].石油实验地质,2007,(2) 9: 280-285,291. ]
[18]Liao Yongsheng.Some issues about evaluation on high-over matured gas source rocks[J]. Petroleum Exploration and Development, 2005,32( 4):147-152.[廖永胜.高—过成熟气源岩评价的若干问题[J].石油勘探与开发,2005,32( 4):147-152.][JP]
[19]Guo Tonglou,Tian Haiqin.Several geology issues about Mesozoic-Palaeozoic oil and gas exploration in southern China and the way of how to deal with[J].Oil & Gas Geology,2002,23(3):244-247.[郭彤楼,田海芹.南方中—古生界油气勘探的若干地质问题及对策[J].石油与天然气地质,2002,23(3):244-247.]
[20]Zhao Wenzhi, Wang Zhaoyun,Zhang Shuichang,et al.Successive generation of natural gas from organic materials and its significance in future exploration[J].Petroleum Exploration and Development,2005,32(2):1-7.[赵文智,王兆云,张水昌,等.有机质“接力成气”模式的提出及其在勘探中的意义[J].石油勘探与开发,2005,32(2):1-7.]
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