Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas

doi:10.7623/syxb201504004

Acta Petrolei Sinica ›› 2015, Vol. 36 ›› Issue (4): 427-445.DOI: 10.7623/syxb201504004

• Petroleum Exploration • Previous Articles Next Articles

Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas

Li Jiao, He Dengfa, Mei Qinghua

Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism of the Ministry of Education, China University of Geosciences, Beijing 100083, China

Received:2014-09-10 Revised:2015-01-20 Online:2015-04-25 Published:2015-04-04

四川盆地及邻区奥陶纪构造-沉积环境与原型盆地演化

李皎, 何登发, 梅庆华

中国地质大学海相储层演化与油气富集机理教育部重点实验室北京 100083

通讯作者: 何登发,男,1967年12月生,1989年毕业于西北大学地质学系,1995年获北京石油勘探开发研究院博士学位,现为中国地质大学(北京)教授、博士生导师,主要从事含油气盆地构造分析研究。Email:hedengfa282@263.net
作者简介:李皎,女,1990年2月生,1990年获中国地质大学(北京)学士学位,现为中国地质大学(北京)硕士研究生,主要从事沉积盆地构造特征研究。Email:lijiao_cugb@qq.com
基金资助:
国家自然科学基金重点项目(No.40739906)和国家重大科技专项(2011ZX05008001)资助。

Abstract

Abstract:

The Ordovician strata are important marine carbonates in China. At present, a series of large oil and gas fields have been discovered in Tarim Basin and Ordos Basin, but no breakthrough has been achieved in the Ordovician strata of Sichuan Basin. The research and restoration of Ordovician tectonic-sedimentary environment provides a basis for studying the tectonic history of Sichuan Basin and adjacent areas and predict the favorable Ordovician reservoir facies belt. According to field outcrop, drilling, logging, seismic and geochemical data, as well as the surrounding tectonic environment, sedimentary facies and filling, paleo-geography, paleo-ecology and tectonic deformation, the tectonic-sedimentary environment of Sichuan Basin in different Ordovician periods was rebuilt by combining basin-filling evolution with the surrounding uplift and trough evolution. Meanwhile, the uplift property and prototype basin evolution were explored. Sichuan Basin and adjacent areas present the composite properties of intra-craton depression and craton-margin depression facies in Ordovician. The surrounding dynamic environment has evolved from tension to extrusion, mainly shown in two kinds of mechanism, i.e., basement subsidence and uplift. Basin surroundings are craton-margin depression basins, dominated by deep-water basin facies. The central part of study area is intra-craton depression basin, experiencing two large cycles of sea level eustasy. The sedimentary sequence is shown as the Early Ordovician rimmed platform→ the Middle Ordovician hybrid continental shelf-rimmed platform→ the Late Ordovician slope-deep water continental shelf facies sediments from bottom to top. The demise of the Middle Ordovician paleo-South China Sea basin and the intra-continent orogeny of South China Plate led to constant lifting and propagation of the central Sichuan uplift, central Guizhou uplift and other basin margin uplifts as well as the continuous rising of sea level. Till the sedimentary period of the Late Ordovician Wufeng Formation, the basement settled rapidly to form the deep-water continental-shelf sedimentary environment, indicating an abrupt change in basin properties and the termination of carbonate platform sedimentary history since Sinian.

Key words: tectonic-depositional environment, proto-type basin, Ordovician, evolution, Sichuan Basin

摘要：

奥陶系是中国重要的海相碳酸盐岩层系。目前,在塔里木、鄂尔多斯盆地奥陶系发现一系列大型油气田,但在四川盆地奥陶系至今仍未取得突破。研究和恢复奥陶纪的构造-沉积环境是研究四川盆地及邻区的构造历史和预测奥陶系有利储集相带的基础。根据野外露头、钻井、测井、地震和地球化学资料,从周缘大地构造背景、沉积相、沉积充填、古地理、古生态、构造变形出发,将盆地充填演化与周缘隆起、海盆演化相结合,重建了四川盆地奥陶纪不同时期的构造-沉积环境,并探讨了隆起性质和原型盆地演化。四川盆地及邻区在奥陶纪表现为克拉通内坳陷和克拉通边缘坳陷相复合的盆地性质,周缘动力学环境经历了拉张→挤压的演变,主要体现在基底沉降以及隆起/隆升两种机制上。盆地周缘为克拉通边缘坳陷盆地,主要为深水盆地相。研究区中部为克拉通内坳陷盆地,经历了两次大的海平面升降旋回,沉积序列由下向上表现为早奥陶世镶边台地→中奥陶世混积陆棚—镶边台地→晚奥陶世缓坡—深水陆棚相沉积。中奥陶世古华南海盆的消亡,华南板块陆内造山,导致川中隆起、黔中隆起等盆地边缘隆起不断隆升和扩展,海平面持续上升,至晚奥陶世五峰组沉积期,基底快速沉降,形成深水陆棚沉积环境,标志着盆地性质的急剧转变,结束了自震旦纪以来的碳酸盐台地沉积历史。

关键词: 构造-沉积环境, 原型盆地, 奥陶纪, 演化, 四川盆地

CLC Number:

P548

Li Jiao, He Dengfa, Mei Qinghua. Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas[J]. Acta Petrolei Sinica, 2015, 36(4): 427-445.

李皎, 何登发, 梅庆华. 四川盆地及邻区奥陶纪构造-沉积环境与原型盆地演化[J]. 石油学报, 2015, 36(4): 427-445.

References

[1] 汪泽成,赵文智,张林,等.四川盆地构造层序与天然气勘探[M].北京:地质出版社,2002.
Wang Zecheng,Zhao Wenzhi,Zhang Lin,et al.Tectonic sequence and gas exploration in Sichuan Basin[M].Beijing:Geological Publishing House,2002.
[2] 何登发,李德生,张国伟,等.四川多旋回叠合盆地的形成与演化[J].地质科学,2011,46(3):589-606.
He Dengfa,Li Desheng,Zhang Guowei,et al.Formation and evolution of multi-cycle superposed Sichuan Basin,China[J].Chinese Journal of Geology,2011,46(3):589-606.
[3] 胡书毅,文玲,田海芹.扬子地区奥陶纪古地理与石油地质条件[J].中国海上油气:地质,2001,15(5):317-321.
Hu Shuyi,Wen Ling,Tian Haiqin.Ordovician palaeogeography and petroleum geology in Yangtze region[J].China Offshore Oil and Gas:Geology,2001,15(5):317-321.
[4] 陈宗清.论四川盆地奥陶系天然气勘探[J].天然气工业,2010,30(1):23-30.
Chen Zongqing.Discussion on the Ordovician gas exploration in Sichuan Basin[J].Natural Gas Industry,2010,30(1):23-30.
[5] 李英强,何登发,文竹.四川盆地及邻区晚震旦世古地理与构造-沉积环境演化[J].古地理学报,2013,15(2):231-246.
Li Yingqiang,He Dengfa,Wenzhu.Paleogeography and tectonic-depositional environment evolution of the late Sinian in Sichuan Basin and adjacent areas[J].Journal of Paleogeography,2013,15(2):231-246.
[6] 梅庆华,何登发,文竹,等.四川盆地乐山—龙女寺古隆起地质结构及构造演化[J].石油学报,2014,35(1):11-25.
Mei Qinghua,He Dengfa,Wen Zhu,et al.Geologic structure and tectonic evolution of Leshan-Longnvsi paleo-uplift in Sichuan Basin,China[J].Acta Petrolei Sinica,2014,35(1):11-25.
[7] 邹才能,杜金虎,徐春春,等.四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.
Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation,distribution,resource potential,prediction and discovery of Sinian-Cambrian giant gas field,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):278-293.
[8] 曹晓萌,于炳松,李心童,等.渝东南下寒武统页岩储层特征及测井评价——以渝科1井和酉科1井为例[J].石油学报,2014,35(2):233-244.
Cao Xiaomeng,Yu Bingsong,Li Xintong,et al.Reservoir characteristics and evaluation on logging of the Lower Cambrian gas shale in southeast Chongqing:a case study of Well Yuke 1 and Well Youke 1[J].Acta Petrolei Sinica,2014,35(2):233-244.
[9] 文玲,胡书毅,田海芹.扬子地区志留纪岩相古地理与石油地质条件研究[J].石油勘探与开发,2002,29(6):11-14.
Wen Ling,Hu Shuyi,Tian Haiqin.Lithofacis paleogeography and petroleum geology of the Silurian in Yangtze area[J].Petroleum Exploration and Development,2002,29(6):11-14.
[10] 张林,魏国齐,郭英海,等.四川盆地志留系层序地层及有利储集层分布[J].天然气工业,2005,25(5):6-8.
Zhang Lin,Wei Guoqi,Guo Yinghai,et al.Silurian sequence stratigraphy and favorable reservoir distribution in Sichuan Basin[J].Natural Gas Industry,2005,25(5):6-8.
[11] 王志峰,张元福,梁雪莉,等.四川盆地五峰组—龙马溪组不同水动力成因页岩岩相特征[J].石油学报,2014,35(4):623-632.
Wang Zhifeng,Zhang Yuanfu,Liang Xueli,et al.Characteristics of shale lithofacies formed under different hydrodynamic conditions in the Wufeng-Longmaxi Formation,Sichuan Basin[J].Acta Petrolei Sinica,2014,35(4):623-632.
[12] 冯增昭,彭勇民,金振奎,等.中国南方寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2001:57-200.
Feng Zengzhao,Peng Yongmin,Jin Zhenkui,et al.Paleogeography of the Cambrian and Ordorvician in South China[M].Beijing:Geological Publishing House,2001:57-200.
[13] 冯增昭,彭勇民,金振奎,等.中国南方中及晚奥陶世岩相古地理[J].古地理学报,2001,3(4):10-24.
Feng Zengzhao,Peng Yongmin,Jin Zhenkui,et al.Lithofacies paleogeography of the Middle and Late Ordorvician in South China[J].Journal of Paleogeography,2001,3(4):10-24.
[14] 马永生,陈洪德,王国力,等.中国南方层序地层与古地理[M].北京:科学出版社,2009:1-591.
Ma Yongsheng,Chen Hongde,Wang Guoli,et al.Sequence stratigraphy and paleography in South China[M].Beijing:Science Press,2009:1-591.
[15] 郑和荣,胡宗全.中国前中生代构造-岩相古地理图集[M].北京:地质出版社,2010:1-194.
Zheng Herong,Hu Zongquan.Atlas of tectonic-lithofacies paleography of Pre-Mesozoic in South China[M].Beijing:Geological Publishing House,2010:1-194.
[16] 梅冥相,曾羽.贵州及邻区奥陶纪红花园期岩相古地理特征[J].岩相古地理,1989 (5):15-25..
Mei Mingxiang,Zeng Yu.Ordovician Honghuayuan sedimentary facies and paleogeography in Guizhou and its adjacent area[J].Lithofacies and Paleogeography,1989 (5):15-25.
[17] 梅冥相,曾羽.贵州及邻区奥陶纪湄潭晚期岩相古地理研究[J].贵州工学院学报,1990,19(1):59-67.
Mei Mingxiang,Zeng Yu.Study of lithofacies and paleogeography of late Meitanian age of Ordovician in Guizhou and its adjacent areas[J].Journal of Guizhou Institute of Technology,1990,19(1):59-67.
[18] 梅冥相.贵州及邻区奥陶纪桐梓期岩相古地理特征[J].贵州地质,1989,16(3):217-225.
Mei Mingxiang.The features of lithofacies paleogeography of Tongzi age in Guizhou province and its adjacent areas[J].Geology of Guizhou,1990,16(1):217-225.
[19] 谢尚克,汪正江,王剑.黔东北地区晚奥陶世岩相古地理[J].古地理学报,2011,13(5):539-549.
Xie Shangke,Wang Zhengjiang,Wang Jian.Lithofacies paleogeography of the Late Ordovician in northeastern Guizhou province[J].Journal of Paleogeography,2011,13(5):539-549.
[20] 崔金栋.黔中隆起及周缘构造演化的沉积响应[D].长沙:中南大学,2013:18-133.
Cui Jindong.Sedimentary response to tectonic evolution of the central Guizhou uplift and its adjacent areas[D].Changsha:Central South University,2013:18-133.
[21] 刘宝珺,许效松.中国南方岩相古地理图集:震旦纪—三叠纪[M].北京:科学出版社,1994:61-73.
Liu Baojun,Xu Xiaosong.Paleogeographic atlas of Sinian Triassic in South China[M].Beijing:Science Press,1994:61-73.
[22] 杨威,谢武仁,魏国齐,等.四川盆地寒武纪—奥陶纪层序岩相古地理、有利储层展布与勘探区带[J].石油学报,2012,33(增刊2):21-34.
Yang Wei,Xie Wuren,Wei Guoqi,et al.Sequence lithofacies paleogeography,favorable reservoir distribution and exploration zones of the Cambrian-Ordorvician in Sichuan Basin,China[J].Acta Petrolei Sinica,2012,33(Supplement 2):21-34.
[23] 高长林,秦德余,吉让寿,等.东秦岭俯冲消减古洋壳的地球化学鉴定[J].石油实验地质,1990,12(2):135-146.
Gao Changlin,Qin Deyu,Ji Rangshou,et al.A geochemical determination of the subduction ocean crust in east Qinling mountains[J].Experimental Petroleum Geology,1990,12(2):135-146.
[24] 吉让寿,秦德余,高长林.古东秦岭洋关闭和华北与扬子两地块拼合[J].石油实验地质,1990,12(4):353-365.
Ji Rangshou,Qin Deyu,Gao Changlin.Closing of eastern Qinling palaeoocean and collaging between the North China and Yangtze blocks[J].Experimental Petroleum Geology,1990,12(4):353-365.
[25] 杨森楠.秦岭古生代陆间裂谷系的演化[J].地球科学:武汉地质学院学报,1985,10(4):53-62.
Yang Sennan.The evolution of Qinling intercontinental rift system in Paleozoic[J].Earth Science:Journal of Wuhan College of Geology,1985,10(4):53-62.
[26] 杨巍然.东秦岭"开""合"史[J].地球科学:武汉地质学院学报,1987,12(5):487-493.
Yang Weiran."Openning" and "closing" history in east Qinling area[J].Earth Science:Journal of Wuhan College of Geology,1987,12(5):487-493.
[27] 李佐臣,裴先治,刘战庆,等.扬子地块西北缘后龙门山南华纪—早古生代沉积地层特征及其形成环境[J].地球科学与环境学报,2011,33(2):117-124.
Li Zuochen,Pei Xianzhi,Liu Zhanqing,et al.Characteristics of sedimentary strata and their forming environments of Nanhuan period-early Paleozoic of back-Longmenshan in the Northwest margin of the Yangtze block[J].Journal of Earth Sciences and Environment,2011,33(2):117-124.
[28] 陈旭,张元动,樊隽轩,等.广西运动的进程:来自生物相和岩相带的证据[J].中国科学:地球科学,2012,42(11):1617-1626.
Chen Xu,Zhang Yuandong,Fan Junxuan,et al.Onset of the Kwangsian Orogeny as evidenced by biofacies and lithofacies [J].Science China:Earth Sciences,2012,55(10):1592-1600.
[29] 舒良树.华南构造演化的基本特征[J].地质通报,2012,31(7):1035-1053.
Shu Liangshu.An analysis of principal features of tectonic evolution in South China block[J].Geological Bulletin of China,2012,31(7):1035-1053.
[30] 戎嘉余,詹仁斌,许红根,等.华夏古陆于奥陶—志留纪之交的扩展证据和机制探索[J].中国科学:地球科学,2010,40(1):1-17.
Rong Jiayu,Zhan Renbin,Xu Honggen,et al.Expansion of the Cathaysian Oldland through the Ordovician-Silurian transition:emerging evidence and possible dynamics[J].Science China:Earth Sciences,2010,53(1):1-17.
[31] 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题[J].中国科学:地球科学,2013,43(10):1553-1582.
Zhang Guowei,Guo Anlin,Wang Yuejun,et al.Tectonics of South China continent and its implications[J].Science China:Earth Sciences,2013,56(11):1804-1828.
[32] 陆克政,朱筱敏,漆家福.含油气盆地分析[M].东营:石油大学出版社,2003:285-318.
Lu Kezheng,Zhu Xiaomin,Qi Jiafu.Basin analysis[M].Dongying:China University of Petroleum Press,2003:285-318.
[33] 杜旭东,朱建伟.沉降曲线原理及应用[J]. 世界地质,1994,13(3):104-113.
Du Xudong,Zhu Jianwei.Principles and applications of subdiction curves[J].World Geology,1994,13(3):104-113.
[34] Wenzel B,Joachimmski M M.Carbon and oxygen isotope composition of Silurian branchiopodas (Gotland/Sweden):paleoceanographic implications[J].Paleogeography,Paleoclimatology,Paleoecology,1996,122(3/4):143-166.
[35] Jenkyns H C,Cale A S,Corfield R M.Carbon-and oxygen-isotope stratigraphy of the English Chalk and Italy Scaglia and its paleoclimatic significance[J].Geological Magazine,1994,131(1):1-34.
[36] Munnecke A,Zhang Y D,Liu X,et al.Stable carbon isotope stratigraphy in the Ordovician of South China[J].Paleogeography,Paleoclimatology,Paleoecology,2007,307(1/4):17-43.
[37] 许效松,万方,尹福光,等.奥陶系宝塔组灰岩的环境相、生态相与成岩相[J].矿物岩石,2001,21(3):64-68.
Xu Xiaosong,Wan Fang,Yin Fuguang,et al.Environmental facies,ecological facies and diagenetic facies of Baota Formation,of Late Ordovina[J].Journal of Mineralogy and Petrology,2001,21(3):64-68.
[38] 戎嘉余.中国的赫南特贝动物群(Hirnantia fauna)并论奥陶系与志留系的分界[J].地层学杂志,1979,3(1):1-28.
Rong Jiayu.The Hirnantia fauna in China and a discussion on the boundaries of the Ordovician and Silurian[J].Acta Stratigraphica Sinica,1979,3(1):1-28.
[39] 张岳桥,施炜,李建华,等.大巴山前陆弧形构造带形成机理分析[J].地质学报,2010,84(9):1300-1315.
Zhang Yueqiao,Shi Wei,Li Jianhua,et al.Formation mechanism of the Dabashan foreland arc-shaped structural belt[J].Acta Geologica Sinica,2010,84(9):1300-1315.
[40] 周小军,李三忠,王岳军,等.雪峰山西侧梵净山—桑植地区构造变形特征[J].地球科学—中国地质大学学报,2011,36(6):985-992.
Zhou Xiaojun,Li Sanzhong,Wang Yuejun,et al.Tectonic features of the Fanjing mount and Sangzhi area on the west of Xuefeng Uplift[J].Earth Science:Journal of China University of Geosciences,2011,36(6):985-992.

Tectonic-depositional environment and proto-type basins evolution of the Ordovician in Sichuan Basin and adjacent areas

四川盆地及邻区奥陶纪构造-沉积环境与原型盆地演化

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