层序地层与同位素地球化学响应特征及礁滩发育模式——以川东城口—鄂西海槽边缘带长兴组为例

董庆民; 胡忠贵; 蔡家兰; 李世临; 苏楠; 左洺滔; 秦鹏

doi:10.11781/sysydz201902243

层序地层与同位素地球化学响应特征及礁滩发育模式——以川东城口—鄂西海槽边缘带长兴组为例

doi: 10.11781/sysydz201902243

1. 长江大学沉积盆地研究中心, 武汉 430100;
2. 中国石油西南油气田公司重庆气矿, 重庆 400021;
3. 中国石油勘探开发研究院, 北京 100083

基金项目:

十三五国家科技重大专项"重点海相层系构造-沉积响应与有利储层分布预测"（2016ZX05007002）和长江青年人才基金项目（2015cqr09）资助。

详细信息

作者简介:
董庆民(1993-),男,硕士研究生,从事沉积学方面的研究。E-mail:416648529@qq.com。

通讯作者:
胡忠贵(1979-),男,博士,副教授,从事储层沉积学方面的研究。E-mail:hzg1978@yangtzeu.edu.cn。

中图分类号: TE121.34
计量
- 文章访问数: 954
- HTML全文浏览量: 85
- PDF下载量: 145
- 被引次数: 0
出版历程
- 收稿日期: 2018-10-11
- 修回日期: 2019-02-11
- 刊出日期: 2019-03-28

Sequence stratigraphy and isotope geochemical response and development pattern of reef and shoal: a case study of Changxing Formation in the marginal zone of Eastern Sichuan Chengkou-Western Hubei Oceanic Trough

1. Sedimentary Basin Research Center, Yangtze University, Wuhan, Hubei 430100, China;
2. Chongqing Gas District, Southwest Oil and Gas Field Co., Ltd., PetroChina, Chongqing 400021, China;
3. Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China

摘要

摘要: 川东地区上二叠统长兴组生物礁滩相带具有巨大的油气勘探潜力，分析层序地层与同位素组成的响应特征及礁滩发育模式，可为该区礁滩勘探提供可靠的地质依据。通过对城口-鄂西海槽边缘带典型露头剖面观察及层序地层分析，结合长兴组碳同位素组成特征，对长兴组层序地层与同位素地球化学响应特征及同一区域内礁滩发育模式进行了研究，将长兴组划分为2个三级层序，5个四级层序，层序格架内碳同位素与海平面升降变化具有良好响应关系。不同沉积相带其礁滩发育模式具有明显差异，迎风一侧的盘龙洞剖面处于最高能台缘相带，礁滩最为发育，云化作用明显，储层发育；背风一侧、同属于台缘带的羊鼓洞剖面，礁滩发育次之，云化作用较弱；而处于开阔台地的渡口剖面，只发育台内颗粒滩沉积，储层不发育。
- 礁滩 /
- 层序地层 /
- 同位素地球化学 /
- 长兴组 /
- 上二叠统 /
- 城口—鄂西海槽 /
- 川东地区
Abstract: The Upper Permian Changxing Formation reef and shoal in the eastern Sichuan Basin has great potential for oil and gas exploration. The analysis of sequence stratigraphic and isotopic composition response as well as reef and shoal development patterns can provide a reliable geologic basis for reef and shoal exploration in this area. Observation of the typical outcrop section and the sequence stratigraphic analysis of the margin of the Chengkou-Western Hubei Oceanic Trough, combined with the carbon isotope composition of the Changxing Formation, show the sequence stratigraphic and geochemical response characteristics of the Changxing Formation and the reef and shoal development patterns. The Changxing Formation was divided into two third-order sequences and five fourth-order sequences. The carbon isotope distributions in the sequence framework have a good relationship with sea level fluctuation. There are obvious differences in the development patterns of reef and shoal in different sedimentary facies belts. The Panlongdong section on the windward side is in the highest energy platform margin belt, where reef and shoal are the most developed, the dolomitization of reef and shoal is obvious, and the reservoir is developed. In the Yanggudong section, which is on the leeward side of the platform margin, the development of reef and shoal takes the second place, and the dolomitization is weak. However, only the intra-platform grain shoal is developed in the Dukou section in the open platform, and reservoir is not developed.
- reef and shoal /
- sequence stratigraphy /
- isotope geochemistry /
- Changxing Formation /
- Upper Permian /
- Chengkou-Western Hubei Oceanic Trough /
- eastern Sichuan region

HTML全文

参考文献(23)

[1]	胡忠贵,黎荣,胡明毅,等.川东华蓥山地区长兴组台内礁滩内部结构及发育模式[J].岩性油气藏,2015,27(5):67-73. HU Zhonggui,LI Rong,HU Mingyi,et al.Internal structure and development model of intra-platform reef and shoal of Chang-xing Formation in Huayingshan area,eastern Sichuan[J].Litho-logic Reservoirs,2015,27(5):67-73.
[2]	马永生,蔡勋育,赵培荣,等.元坝气田长兴组-飞仙关组礁滩相储层特征和形成机理[J].石油学报,2014,35(6):1001-1011. MA Yongsheng,CAI Xunyu,ZHAO Peirong,et al.Characteristics and formation mechanisms of reef-shoal carbonate reservoirs of Changxing-Feixianguan formations,Yuanba Gas Field[J].Acta Petrolei Sinica,2014,35(6):1001-1011.
[3]	马永生,蔡勋育,李国雄.四川盆地普光大型气藏基本特征及成藏富集规律[J].地质学报,2005,79(6):858-865. MA Yongsheng,CAI Xunyu,LI Guoxiong.Basic characteristics and concentration of the Puguang Gas Field in the Sichuan Basin[J].Acta Geologica Sinica,2005,79(6):858-865.
[4]	郭彤楼.川东北地区台地边缘礁、滩气藏沉积与储层特征[J].地学前缘,2011,18(4):201-211. GUO Tonglou.The characteristics of sedimentation and reservoirs of reef-beach gas fields in carbonate platform margins,northeastern Sichuan Basin[J].Earth Science Frontiers,2011,18(4):201-211.
[5]	刘宏,谭秀成,周彦,等.川东北黄龙场气田飞仙关组台缘滩型碳酸盐岩储层预测[J].石油学报,2009,30(2):219-224. LIU Hong,TAN Xiucheng,ZHOU Yan,et al.Prediction of platform-edge bank carbonate reservoir in Feixianguan Formation of Huanglongchang Gas Field in the northeastern Sichuan Basin[J].Acta Petrolei Sinica,2009,30(2):219-224.
[6]	赵文光,郭彤楼,蔡忠贤,等.川东北地区二叠系长兴组生物礁类型及控制因素[J].现代地质,2010,24(5):951-956. ZHAO Wenguang,GUO Tonglou,CAI Zhongxian,et al.The controlling factors and types of Permian Changxing Formation in northeast of Sichuan Basin[J].Geoscience,2009,30(2):219-224.
[7]	周刚,郑荣才,罗韧,等.环开江-梁平海槽长兴组生物礁类型及储层特征[J].岩性油气藏,2013,25(1):81-87. ZHOU Gang,ZHENG Rongcai,LUO Ren,et al.Types and characteristics of reefs of Permian Changxing Formation around Kaijiang-Liangping Trough,eastern Sichuan Basin[J].Lithologic Reservoirs,2013,25(1):81-87.
[8]	胡明毅,钱勇,胡忠贵,等. 塔里木柯坪地区奥陶系层序地层与同位素地球化学响应特征[J].岩石矿物学杂志,2010,29(2):199-205. HU Mingyi,QIAN Yong,HU Zhonggui,et al.Carbon isotopic and element geochemical responses of carbonate rocks and Ordovician sequence stratigraphy in Keping area,Tarim Basin[J].Acta Petrologica et Mineralogica,2010,29(2):199-205.
[9]	贾承造,刘德来,赵文智,等.层序地层学研究新进展[J].石油勘探与开发,2002,29(5):1-4. JIA Chengzao,LIU Delai,ZHAO Wenzhi,et al.Some new achievements in sequence stratigraphy research[J].Petroleum Exploration and Development,2002,29(5):1-4.
[10]	李小燕,王琪,韩元红,等.川东北地区长兴组-飞仙关组礁滩相沉积体系优质储层形成过程及储集空间演化主控因素分析[J].天然气地球科学,2014,25(10):1594-1602. LI Xiaoyan,WANG Qi,HAN Yuanhong,et al.Main controlling factors on reservoir space evolution and high quality reservoir forming process of reef-beach facies in Changxing-Feixianguan formation of northeastern Sichuan area[J].Natural Gas Geoscience,2014,25(10):1594-1602.
[11]	杨雨,文应初.川东北开江-梁平海槽发育对T₁f鲕粒的预测[J].天然气工业,2002,22(增刊):30-32. YANG Yu,WEN Yingchu.Northeastern Sichuan Kaijiang-Liangping Trough development of oolitic forecast[J].The Natural Gas Industry,2002,22(Supp.):30-32.
[12]	杨雨,王一刚,文应初,等.川东飞仙关组沉积相与鲕滩气藏的分布[J].天然气勘探与开发,2001,24(3):18-21. YANG Yu,WANG Yigang,WEN Yingchu,et al.Eastern Sichuan Basin Feixianguan ooltic sedimentary facies and the distribution of gas reservoir[J].Natural Gas Exploration and Development,2001,24(3):18-21.
[13]	刘治成,张廷山,党录瑞,等.川东北地区长兴组生物礁成礁类型及分布[J].中国地质,2011,38(5):1298-1311. LIU Zhicheng,ZHANG Tingshan,DANG Lurui,et al.Reef-forming types and distribution of organic reefs in Changxing Formation of northeastern Sichuan area[J].Geology in China,2011,38(5):1298-1311.
[14]	邹才能,徐春春,汪泽成,等.四川盆地台缘带礁滩大气区地质特征与形成条件[J].石油勘探与开发,2011,38(6):641-651. ZOU Caineng,XU Chunchun,WANG Zengtao,et al.Geological characteristics and forming conditions of the large platform margin reef-shoal gas province in the Sichuan Basin[J].Petroleum Exploration and Development,2011,38(6):641-651.
[15]	腾飞,胡忠贵,刘忠保,等.川东奉节及周缘地区下三叠统飞仙关组沉积特征及相带演化[J].石油天然气学报,2016,38(4):23-31. TENG Fei,HU Zhonggui,LIU Zhongbao,et al.The sedimentary characteristics and facies evolution of the Lower Triassic Feixianguan Formation in Fengjie and its peripheral areas in the east Sichuan region[J].Journal of Oil and Gas Technology,2016,38(4):23-31.
[16]	王必金,胡明毅.建南地区上二叠统长兴组层序地层特征研究[J].石油天然气学报,2013,35(10):14-19. WANG Bijin,HU Mingyi.The sequence stratigraphic characteris-tics of Upper Permian Changxing Formation in Jiannan area[J].Journal of Oil and Gas Technology,2013,35(10):14-19.
[17]	胡明毅,胡忠贵,魏国齐,等.四川盆地茅口组层序岩相古地理特征及储集层预测[J].石油勘探与开发,2012,39(1):45-55. HU Mingyi,HU Zhonggui,WEI Guoqi,et al.Sequence lithofacies paleogeography and reservoir prediction of the Maokou Formation in Sichuan Basin[J].Petroleum Exploration and Deve-lopment,2012,39(1):45-55.
[18]	张建勇,周进高,郝毅,等.四川盆地环开江-梁平海槽长兴组-飞仙关组沉积模式[J].海相油气地质,2011,16(3):45-54. ZHANG Jianyong,ZHOU Jingao,HAO Yi,et al.A sedimentary model of Changxing and Feixianguan reservoirs around Kaijiang-Liangping Trough in Sichuan Basin[J].Marine Origin Petroleum Geology,2011,16(3):45-54.
[19]	符颖,韩林.淹没不整合层序:一种特殊的加深淹没[J].海相油气地质,2007,12(3):15-20. FU Ying,HANLin.Drowned unconformity sequence:a special type of deepened submerge sequence interface[J].Marine Origin Petroleum Geology,2007,12(3):15-20.
[20]	朱金富,于炳松,黄文辉,等.塔里木盆地塔中地区晚寒武世-奥陶世碳酸盐岩碳、氧同位素特征[J].大庆石油地质与开发,2008,27(1):40-42. ZHU Jinfu,YU Bingsong,HUANG Wenhui,et al.Carbon and oxygen isotope features of Late Cambrian-Ordovician in central Tarim Basin[J].Petroleum Geology & Oilfield Development in Daqing,2008,27(1):40-42.
[21]	彭苏萍,何宏,邵龙义,等.塔里木盆地寒武-奥陶系碳酸盐岩碳同位素组成特征[J].中国矿业大学学报,2002,31(4):353-358. PENG Suping,HE Hong,SHAO Longyi,et al.Carbon isotopic compositions of the Cambrian-Ordovician carbonates in Tarim Basin[J].Journal of China University of Mining & Technology,2002,31(4):353-358.
[22]	肖娇静,王龙樟,陈梅,等.四川盆地早三叠世多尺度海平面变化旋回及对储层发育的影响[J].石油实验地质,2017,39(5):618-624. XIAO Jiaojing,WANG Longzhang,CHEN Mei,et al.Multiple scale fluctuations of the Early Triassic sea level and its influence on reservoirs in the Sichuan Basin[J].Petroleum Geology & Experiment,2017,39(5):618-624.
[23]	黄可可,黄思静,胡作维,等.四川盆地宣汉渡口和重庆北碚下三叠统海相碳酸盐岩的碳同位素组成与演化[J].古地理学报,2016,18(1):101-114. HUANG Sijing,HUANG Sijing,HU Zuowei,et al.Carbon isotopic composition and evolution of Early Triassic marine carbo-nate from Dukou of Xuanhan and Beibei of Chongqing,Sichuan Basin,China[J].Journal of Palaeogeography,2016,18(1):101-114.