康滇古陆西侧断裂及岩浆活动对油气保存条件的影响:以盐源盆地为例
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摘要
盐源盆地复杂的断裂体系及频繁的构造与岩浆活动对盆地内页岩气及常规油气保存的影响有待探讨.通过对断裂、岩浆活动与两套主要烃源岩生排烃史的匹配性分析,认为:(1)盐源盆地的边界断裂及其伴生的次级断裂在喜马拉雅期均有活动,且其活动作用主要是破坏早期的油气藏,并对油气的空间配置进行再次调整,对自生自储的原位页岩气保存主要起破坏作用;(2)盐源盆地内部北东向与北西向两组褶皱中仍然可能残留保存相对较完好的构造圈闭,并且可能富含气和轻质油;(3)盐源盆地及邻区所发育的海西期、印支期、燕山期及喜山期4期岩浆活动对盐源盆地中油气生成与运移的有利作用在于催熟烃源岩,加速其生油气,并提供潜在的运移通道;不利作用在于会破坏有利圈闭或先期油气藏,且烃源岩中的岩浆底辟会对自生自储的原位页岩气保存起破坏作用.
In order to understand the influences of the complex faults,frequent tectonics and magmatic activitieson on hydrocarbon preservation condition in the Yanyuan Basin,the relationship between faults,magmatism and the thermal history of two primary source rock are analyzed in the adjacent areas to the west of Kangdian ancient continent in this study. The results indicate that:( 1) the boundary faults and their associated secondary faults all have been active in the Himalayan period and their activities which mainly involves destroying the early oil and gas reservoirs and readjusting the spatial configuration of oil and gas,which mainly has been destructive in the self-generated in situ shale gas reservoirs.( 2) The north-east and north-west folds within Yanyuan Basin may still retain relatively well-preserved structural traps and may be rich in gas and light oil.( 3) In Yanyuan Basin and its adjacent areas,the Hercynian,Indosinian,Yanshanian and Himalayan magmatic activities have the following beneficial effects on hydrocarbon generation and migration: ripening source rocks,accelerating their hydrocarbon generation and providing potential migration channels; the negative effects include destroying the favorable traps or previous reservoirs,and destroying the self-generated and self-storage in situ shale gas by magmatic diapirism.
In order to understand the influences of the complex faults,frequent tectonics and magmatic activitieson on hydrocarbon preservation condition in the Yanyuan Basin,the relationship between faults,magmatism and the thermal history of two primary source rock are analyzed in the adjacent areas to the west of Kangdian ancient continent in this study. The results indicate that:( 1) the boundary faults and their associated secondary faults all have been active in the Himalayan period and their activities which mainly involves destroying the early oil and gas reservoirs and readjusting the spatial configuration of oil and gas,which mainly has been destructive in the self-generated in situ shale gas reservoirs.( 2) The north-east and north-west folds within Yanyuan Basin may still retain relatively well-preserved structural traps and may be rich in gas and light oil.( 3) In Yanyuan Basin and its adjacent areas,the Hercynian,Indosinian,Yanshanian and Himalayan magmatic activities have the following beneficial effects on hydrocarbon generation and migration: ripening source rocks,accelerating their hydrocarbon generation and providing potential migration channels; the negative effects include destroying the favorable traps or previous reservoirs,and destroying the self-generated and self-storage in situ shale gas by magmatic diapirism.
引文
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Xie,J.,2017.Rapid Shale Gas Development Accelerated by the Progress in Key Technologies:A Case Study of the Changning-Weiyuan National Shale Gas Demonstration Zone.Natural Gas Industry,37(12):1-10(in Chinese with English abstract).
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Feng,Q.,Tang,X.Y.,1997.Magma Activity's Influence on Conditions Forming Oil and Gas Pools.Geological Science&Technology Information,16(4):59-65(in Chinese with English abstract).
Guo,T.L.,2016.Discovery and Characteristics of the Fuling Shale Gas Field and Its Enlightenment and Thinking.Earth Science Frontiers,23(1):29-43(in Chinese with English abstract).
Guo,X.S.,Hu,D.F.,Wei,Z.H.,et al.,2016.Discovery and Exploration of Fuling Shale Gas Field.China Petroleum Exploration,21(3):24-37(in Chinese with English abstract).
He,D.F.,Ma,Y.S.,Yang,M.H.,2004.Concept and Appraisal Principles of Hydrocarbon Preservation Unit.Oil&Gas Geology,25(1):1-8(in Chinese with English abstract).
He,W.H.,Tang,T.T.,Yue,M.L.,et al.,2014.Sedimentary and Tectonic Evolution of Nanhuan-Permian in South China.Earth Science,39(8):929-953.https://doi.org/10.3799/dqkx.2014.087
He,Y.X.,Qian,Y.Z.,2000.The Silurian Devonian Boundary in Baizitian,Yanbian,Sichuan and Its Geological Implications.Sedimentary Geology and Tethyan Geology,20(1):98-112(in Chinese with English abstract).
He,Z.L.,Hu,Z.Q.,Nie,H.K.,et al.,2017a.Characterization of Shale Gas Enrichment in the Wufeng-Longmaxi Formation in the Sichuan Basin and Its Evaluation of Geological Construction-Transformation Evolution Sequence.Natural Gas Geoscience,28(5):724-733(in Chinese with English abstract).
He,Z.L.,Li,S.J.,Wo,Y.J.,et al.,2017b.Major Factors Controlling Hydrocarbon Preservation Condition in the Marine Basins of China and Its Evaluation Ideas.Acta Petrologica Sinica,33(4):1221-1232(in Chinese with English abstract).
Hu,D.F.,Zhang,H.R.,Ni,K.,et al.,2014.Main Controlling Factors for Gas Preservation Conditions of Marine Shales in Southeastern Margins of the Sichuan Basin.Natural Gas Industry,34(6):17-23(in Chinese with English abstract).
Hu,S.Q.,Guo,W.P.,1995.Rhombohedral Structure Framework and Its Junction Structure Style in Ninglang Area of Yunnan.Journal of Mineralogy&Petrology,15(4):93-99(in Chinese with English abstract).
Jin,C.T.,1982.Summary of Strata in Southwest China.Department of Geology and Mineral Resources Chengdu Institute of Geology and Mineral Resources,Chengdu(in Chinese).
Jin,Z.J.,Cai,X.Y.,Liu,J.L.,et al.,2018.The Recent Exploration Progress and Resource Development Strategy of China Petroleum and Chemical Corporation.China Petroleum Exploration,23(1):14-25(in Chinese with English abstract).
Li,M.C.,Li,W.,Cai,F.,et al.,1997.Integrative Study of Preservation Conditions of Oil and Gas Pools.Acta Petrolei Sinica,18(2):41-48(in Chinese with English abstract).
Li,Y.,Hou,Z.J.,Si,G.Y.,et al.,2001.Sedimentary Characteristics and Tectonic Controls in Neogene Yanyuan Tectonic Escape Basin in Southeastern Qinghai-Tibet Plateau.Journal of Mineralogy&Petrology,21(3):34-43(in Chinese with English abstract).
Liang,X.,Wang,G.C.,Zhang,J.H.,et al.,2017.High-Efficiency Integrated Shale Gas Development Model of Zhaotong National Demonstration Zone and Its Practical Enlightenment.China Petroleum Exploration,22(1):29-37(in Chinese with English abstract).
Lou,Z.H.,Shang,C.J.,Yao,G.S.,et.al.,2011.Hydrocarbon Preservation Conditions in Marine Strata of the Guizhong Depression and Its Margin.Acta Petrolei Sinica,32(3):432-441(in Chinese with English abstract).
Luo,Q.,Sun,H.Z.,2000,Relationship between Faulting and the Preservation of Oil and Gas Accumulation.Experimental Petroleum Geology,22(3):225-231(in Chinese with English abstract).
Nie,H.K.,Bao,S.J.,Gao,B.,et al.,2012.A Study of Shale Gas Preservation Conditions for the Lower Paleozoic in Sichuan Basin and Its Periphery.Earth Science Frontiers,19(3):280-294(in Chinese with English abstract).
Pan,R.F.,Tang,X.L.,Meng,J.H.,et al.,2014,Shale Gas Preservation Conditions for the Upper Paleozoic in Guizhong Depression.Oil&Gas Geology,35(4):534-541(in Chinese with English abstract).
Sichuan Earthquake Administration,1986.Study on Seismic Hazards in Panxi Area.Sichuan Science and Technology Press,Chengdu(in Chinese).
Sichuan Provincial Institute of Geology and Mineral Resources,1987.The Triassic Strata and Sedimentary Facies in Yanyuan-Lijiang District.Geological Publishing House,Beijing(in Chinese).
Tang,R.L.,1987.The Relationship between the Tectonic Characteristics of the Muli-Yanyuan Nappe and the Metallogenic Relationship between Gold and Copper,Lead and Zinc.Acta of Sichuan Geology,7(2):5-11(in Chinese with English abstract).
Wang,C.Y.,Wang,P.,Yang,G.H.,et al.,2009.Restudy on the Silurian Conodont Biostratigraphy of the Baizitian Section in Yanbian County,Sichuan.Journal of Stratigraphy,33(3):302-317(in Chinese with English abstract).
Wang,F.Y.,Duan,Y.H.,Yang,Z.X.,et al.,2008.Velocity Structure and Active Fault of Yanyuan-Mabian Seismic Zone:The Result of High-Resolution Seismic Refraction Experiment.Science in China(Series D),38(5):611-621(in Chinese).
Wang,Z.H.,2000.An Analysis of Oil-Gas Exploration Perspective of Ninglang Basin.Yunnan Geology,19(4):443-448(in Chinese with English abstract).
Wu,M.Q.,2017.Tectonic Deformation and Evolution of Xiaojinhe Fault of Muli Area(Dissertation).Chengdu University of Technology,Chengdu(in Chinese with English abstract).
Xie,J.,2017.Rapid Shale Gas Development Accelerated by the Progress in Key Technologies:A Case Study of the Changning-Weiyuan National Shale Gas Demonstration Zone.Natural Gas Industry,37(12):1-10(in Chinese with English abstract).
Yue,P.S.,Shi,Q.,Yue,L.Q.,et al.,2017.The Latest Progress of Shale Gas Exploration and Development in China.Natural Gas Exploration and Development,40(3):38-44(in Chinese with English abstract).
Zhong,K.H.,Liu,Z.C.,Shi,Y.,et al.,2004.Yanyuan-Lijiang Tectonic Zone:A Cenozoic Intracontinental Orogenic Belt.Acta Geologica Sinica,78(1):36-43(in Chinese with English abstract).
Zhu,M.,Chen,H.L.,Zhou,J.,et al.,2016.Provenance of Early Triassic in Yanyuan Basin,Upper Yangtze and Its Implication for the Tectonic Evolution.Earth Science,41(8):1309-1321(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.106
房建军,2004.楚雄盆地构造变动与后期改造综合研究(硕士学位论文).西安:西北大学.
冯乔,汤锡元,1997.岩浆活动对油气藏形成条件的影响.地质科技情报,16(4):59-65.
郭彤楼,2016.涪陵页岩气田发现的启示与思考.地学前缘,23(1):29-43.
郭旭升,胡东风,魏志红,等,2016.涪陵页岩气田的发现与勘探认识.中国石油勘探,21(3):24-37.
何登发,马永生,杨明虎,2004.油气保存单元的概念与评价原理.石油与天然气地质,25(1):1-8.
何卫红,唐婷婷,乐明亮,等,2014.华南南华纪-二叠纪沉积大地构造演化.地球科学,39(8):929-953.https://doi.org/10.3799/dqkx.2014.087
何原相,钱咏臻,2000.四川盐边稗子田志留系与泥盆系的界线划分及地质意义.沉积与特提斯地质,20(1):98-112.
何治亮,胡宗全,聂海宽,等,2017a.四川盆地五峰组-龙马溪组页岩气富集特征与“建造-改造”评价思路.天然气地球科学,28(5):724-733.
何治亮,李双建,沃玉进,等,2017b.中国海相盆地油气保存条件主控因素与评价思路.岩石学报,33(4):1221-1232.
胡东风,张汉荣,倪楷,等,2014.四川盆地东南缘海相页岩气保存条件及其主控因素.天然气工业,34(6):17-23.
胡受权,郭文平,1995.云南宁蒗地区菱形构造格局及其联合构造型式.矿物岩石,15(4):93-99.
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