Assessment on distribution of the Cambrian evaporites affected by structural deformation in eastern Sichuan Basin
Liang Han1, Ma Bo1, Xiao Bo-Yi2, He Qing-Lin1
1 Exploration and Development Research Institute of Southwest Oil & Gas Field Company,PetroChina, Chengdu 610041,China; 2 Exploration Division of Southwest Oil & Gas Field Company, PetroChina, Chengdu 610041, China
Abstract The widely spread Cambrian Lagoon salt in eastern Sichuan Basin makes the tectonic belts of Lower Paleozoic-Sinian system become a great potential of oil and gas exploration. However, due to the complicated high-steep structural deformation and the limited drilling information, the characteristics of structural deformation is not clear, making it difficult to predict the distribution of structural trapping and favorable reservoirs. Based on the comprehensive analysis on seismogeology to obtain the seismic response characteristics of salt structures and evaporites, the structural deformation and distribution of Cambrian evaporites in eastern Sichuan Basin have been investigated in this paper. As the most essential detachment, the Cambrian salt layer caused the development of thin-layered structure in eastern Sichuan, can be regarded as the isolated fold. The isolated structural mode is positively correlated with the salt structural deformation of Cambrian salt layer, which is the dominated structural characteristics in this area, establishing the structural deformation mode of this area. Based on the rock mechanics of salt layer which is controlled by faults, together with the seismic reflection characteristics, the distribution of the Cambrian salt has been predicted, presenting that it is bounded by the Huayingshan belt to the west, and extends to the Daba Mountain Front along the Shuikouchang tectonic belt to the north, and extends to southwestern direction along the southern Sichuan low steep tectonic belt to the south. The Cambrian depositional center is located along the northeast to southwest direction of the Fangdou mountain.
Fund:Co-funded by National Science and Technology Major Project of China (No. 2016ZX05007-004) and Science and Technology Major Project of CNPC(No.2016E-0604)
About author: Liang Han,born in 1982,is a senior engineer. Now he is engaged in research of petroleum geology and structural geology. E-mail: lianghan01@petroChina.com.cn.
Cite this article:
Liang Han,Ma Bo,Xiao Bo-Yi et al. Assessment on distribution of the Cambrian evaporites affected by structural deformation in eastern Sichuan Basin[J]. JOPC, 2019, 21(5): 825-834.
Liang Han,Ma Bo,Xiao Bo-Yi et al. Assessment on distribution of the Cambrian evaporites affected by structural deformation in eastern Sichuan Basin[J]. JOPC, 2019, 21(5): 825-834.
[1] 冯伟明,谢渊,刘建清,林家善,陈果. 2016. 四川盆地东南缘清虚洞组层序-岩相古地理特征及其油气地质意义. 成都理工大学学报(自然科学版), 43(1): 35-43. [Feng W M,Xie Y,Liu J Q,Lin J S,Chen G.2016. Characteristics of sequence-based lithofacies and paleogeography of Qingxudong Formation on the southeast margin of Sichuan Basin,China. Journal of Chengdu University of Technology(Science & Technology Edition), 43(1): 35-43] [2] 谷志东,殷积峰,袁苗,薄冬梅,梁东星,张航,张黎. 2015. 四川盆地东部深层盐下震旦系—寒武系天然气成藏条件与勘探方向. 石油勘探与开发, 42(2): 137-149. [Gu Z D,Yin J F,Yuan M,Bo D M,Liang D X,Zhang H,Zhang L.2015. Accumulation conditions and exploration directions of natural gas in deep subsalt Sinian-Cambrian System in the eastern Sichuan Basin,SW China. Petroleum Exploration & Development, 42(2): 137-149] [3] 郭彤楼. 2011. 元坝深层礁滩气田基本特征与成藏主控因素. 天然气工业, 31(10): 12-16. [Guo T L.2011. Basic characteristics of deep reef-bank reservoirs and major controlling factors of gas pools in the Yuanba Gas Field. Natural Gas Industry, 31(10): 12-16] [4] 黄士鹏,廖凤蓉,吴小奇,陶小晚. 2010. 四川盆地含硫化氢气藏分布特征及硫化氢成因探讨. 天然气地球科学, 21(5): 705-714. [Huang S P,Liao F R,Wu X Q,Tao X W.2010. Distribution characteristics of hydrogen sulphide-bearing gas pools and the genesis of hydrogen sulphide in Sichuan Basin. Natural Gas Geoscience, 21(5): 705-714] [5] 金之钧,龙胜祥,周雁,沃玉进,肖开华,杨志强,殷进垠. 2006. 中国南方膏盐层分布特征. 石油与天然气地质, 27(5): 571-583. [Jin Z J,Long S X,Zhou Y,Wo Y J,Xiao K H,Yang Z Q,Yin J Y.2006. A study on the distribution of saline-deposit in southern China. Oil & Gas Geology, 27(5): 571-583] [6] 李双建,孙冬胜,郑孟林,孟宪武. 2014. 四川盆地寒武系盐相关构造及其控油气作用. 石油与天然气地质, 35(5): 622-631,638. [Li S J,Sun D S,Zheng M L,Meng X W.2014. Salt-related structure and its control on hydrocarbon of the Cambrian in Sichuan Basin. Oil & Gas Geology, 35(5): 622-631,638] [7] 李辛子,刘彬,武晓玲,刘国萍,冯琼,付孝悦. 2013. 通南巴地区膏盐层分布及其流变学特征. 石油与天然气地质, 34(4): 533-539. [Li X Z,Liu B,Wu X L,Liu G P,Feng Q,Fu X Y.2013. Distribution and rheological characteristics of evaporates in Tongnanba area. Oil & Gas Geology, 34(4): 533-539] [8] 林良彪,郝强,余瑜,彭勇民. 2014. 四川盆地下寒武统膏盐层发育特征与封盖有效性分析. 岩石学报, 30(3): 718-726. [Lin L B,Hao Q,Yu Y,Peng Y M.2014. Development characteristics and sealing effectiveness of Lower Cambrian gypsum rock in Sichuan Basin. Acta Petrologica Sinica, 30(3): 718-726] [9] 吕修祥,金之钧,周新源,皮学军. 2000. 塔里木盆地库车坳陷与膏盐岩相关的油气聚集. 石油勘探与开发, 27(4): 20-21. [Lü X X,Jin Z J,Zhou X Y,Pi X J.2000. Oil and gas accumulation related to salt in Kuqa Depression. Petroleum Exploration and Development, 27(4): 20-21] [10] 马新华,华爱刚,李景明,姚建军. 2000. 含盐油气盆地. 北京: 石油工业出版社: 1-2. [Ma X H,Hua A G,Li J M,Yao J J.2000. Petroliferous Saltbearing Basin. Beijing: Petroleum Industry Press, 1-2] [11] 马永生. 2007. 四川盆地普光超大型气田的形成机制. 石油学报, 28(2): 9-21. [Ma Y S.2007. Generation mechanism of Puguang Gas Field in Sichuan Basin. Acta Petrolei Sinica, 28(2): 9-21] [12] 马永生,蔡勋育,赵培荣,罗毅,张学丰. 2010. 四川盆地大中型天然气田分布特征与勘探方向. 石油学报, 31(3): 347-354. [Ma Y S,Cai X Y,Zhao P R,Luo Y,Zhang X F.2010. Distribution and further exploration of the large-medium sized gas fields in Sichuan Basin. Acta Petrolei Sinica, 31(3): 347-354] [13] 门玉澎,许效松,牟传龙,余谦,闫剑飞,刘伟. 2010. 中上扬子寒武系蒸发岩岩相古地理. 沉积与特提斯地质, 30(3): 58-64. [Men Y P,Xu X S,Mou C L,Yu Q,Yan J F,Liu W.2010. Sedimentary facies and palaeogeography of the evaporates in the middle-upper Yangtze area. Sedimentary Geology and Tethyan Geology, 30(3): 58-64] [14] 唐鹏程. 2011. 南天山库车坳陷西段新生代盐构造: 构造分析和物理模拟. 浙江大学博士论文: 18. [Tang P C.2011. Cenozoic salt structures in the western Kuqa depression,Southern Tianshan: Structural analysis and physical modeling. Docteral Dissertation of Zhejiang University: 18] [15] 王淑丽,郑绵平,焦建. 2012. 上扬子区寒武系蒸发岩沉积相及成钾潜力分析. 地质与勘探, 48(5): 947-958. [Wang S L,Zheng M P,Jiao J.2012. Sedimentary facies of the Cambrian evaporites in the upper Yangtze region and their potash-forming potential. Geology and Exploration, 48(5): 947-958] [16] 汪新,唐鹏程,谢会文,雷刚林,黄少英. 2009. 库车坳陷西段新生代盐构造特征及演化. 大地构造与成矿学, 33(1): 57-65. [Wang X,Tang P C,Xie H W,Lei G L,Huang S Y.2009. Cenozoic salt structures and evolution in the western Kuqa depression,Tarim basin,China. Geotectonica et Metallogenia, 33(1): 57-65] [17] 王宗秀,张进,关会梅,汤良杰,肖伟峰,鄢犀利. 2012. 雪峰山西侧地区构造形变与油气圈闭. 地质通报, 31(11): 1812-1825. [Wang Z X,Zhang J,Guan H M,Tang L J,Xiao W F,Yan X L.2012. A discussion on the structural deformation and oil/gas traps on the western side of the Xuefeng Mountain. Geological Bulletin of China, 31(11): 1812-1825] [18] 徐安娜,胡素云,汪泽成,薄冬梅,李梅,鲁卫华,翟秀芬. 2016. 四川盆地寒武系碳酸盐岩—膏盐岩共生体系沉积模式及储层分布. 天然气工业, 36(6): 11-20. [Xu A N,Hu S Y,Wang Z C,Bo D M,Li M,Lu W H,Zhai X F.2016. Sedimentary mode and reservoir distribution of the Cambrian carbonate & evaporite paragenesis system in the Sichuan Basin. Natural Gas Industry, 36(6): 11-20] [19] 徐美娥,张荣强,彭勇民,陈霞,冯菊芳. 2013. 四川盆地东南部中、下寒武统膏盐盖层分布特征及封盖有效性. 石油与天然气地质, 34(3): 301-306. [Xu M E,Zhang R Q,Peng Y M,Chen X,Feng J F.2013. Distribution and sealing effectiveness of Middle-Lower Cambrian evaporite cap rocks in the southeastern Sichuan Basin. Oil & Gas Geology, 34(3): 301-306] [20] Bahroudi A,Koyi H A,Talbot C J.2003. Modelling the effect of ductile and frictional décollements on structural style of extension. Journal of Structural Geology, 160(5): 719-733. [21] Cotton J T,Koyi H A.2000. Modeling of thrust fronts above ductile and frictional detachments: Application to structures in the Salt Range and Potwar Plateau,Pakistan. Geological Society of America Bulletin, 112(3): 351-363. [22] Davis D M,Engelder T.1985. The role of salt in fold-and-thrust belts. Tectonophysics, 119: 67-88. [23] Epard J L,Groshong Jr R H.1995. Kinematic model of detachment folding including limb rotation,fixed hinges and layer-parallel strain. Tectonophysics, 247(1-4): 85-103. [24] Liu H,Tan X C,Yonghao L,Jian C,Bin L.2018. Occurrence and conceptual sedimentary model of Cambrian gypsum-bearing evaporites in the Sichuan Basin,SW China. Geoscience Frontiers, 9(4): 1179-1191. [25] Jackson M P A,Talbot C J.1991. A glossary of salt tectonics: The University of Texas at Austin. Bureau of Economic Geology. Geological Circular, 91(4): 1-42. [26] Jackson M P A,Vendeville B C.1994. Regional extension as a geologic trigger for diapirism. Geological Society of America Bulletin, 106(1): 57-73. [27] Letouzey J, Colletta B,Vially R,Chermette J C.1995. Evolution of salt-related structures in compressional settings. In: Jackson M P A, Roberts D G,and Snelson S(eds). Salt Tectonics: A Global Perspective. AAPG Memoir, 65: 41-60. [28] Marshak S,Wilkerson M S.2004. Fold-Thrust Belts·Earth Structure(2nd). In: van der Pluijm B A, Marshak S(eds). Fold-Thrust Belts. Publisher: W. W. Norton & Company,Inc.: 466. [29] Mitra S.2002. Fold-accommodation faults.AAPG Bulletin, 86(4): 671-693. [30] Weijermars R,Jaekson M P A,Vendeville B C.1993. Rheologieal and tectonic modelling of salt Provinces.Tectonophysics, 217: 143-174. [31] Yan D P,Zhou M F,Song H L,Wang X W,Malpas J.2003. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block(South China). Tectonophysics, 23: 239-254. [32] Zulauf J,Zulauf G.2004. Rheology of Plasticine used as rock analogue: The impact of temperature,composition and strain. Journal of Structural Geology, 26: 725-737.