川东南地区中—下寒武统膏岩层系分布特征及其影响因素

朱彦先; 何生; 何治亮; 张殿伟; 张树林; 孙自明; 陶泽

doi:10.11781/sysydz202006910

川东南地区中—下寒武统膏岩层系分布特征及其影响因素

doi: 10.11781/sysydz202006910

1.
中国地质大学(武汉) 构造与油气资源教育部重点实验室, 武汉 430074
2.
中国石油化工股份有限公司, 北京 100728
3.
中国石化石油勘探开发研究院, 北京 100083

基金项目:

国家“十三五”科技重大专项子课题 2017ZX05005-001-008

中国石油化工股份有限公司科研项目 P19022-3

详细信息

作者简介:
朱彦先(1996—)，男，硕士研究生，从事油气成藏和构造解析研究。E-mail: 1201810213@cug.edu.cn

通讯作者:
何生(1956-), 男, 教授, 博士生导师, 从事油气地质及地球化学教学与研究。E-mail: shenghe@cug.edu.cn

中图分类号: TE121.3
计量
- 文章访问数: 847
- HTML全文浏览量: 240
- PDF下载量: 133
- 被引次数: 0
出版历程
- 收稿日期: 2020-05-29
- 修回日期: 2020-08-28
- 刊出日期: 2020-11-28

Distribution characteristics and influencing factors of Middle-Lower Cambrian gypsum in southeastern Sichuan Basin

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geoscience(Wuhan), Wuhan, Hubei 430074, China
2.
SINOPEC, Beijing 100728, China
3.
SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100083, China

摘要

摘要: 川东南地区中—下寒武统龙王庙组和高台组为膏岩层系，石膏岩广泛发育，被认为是该区震旦系至中—下寒武统储层的盖层。通过统计钻井和二维地震资料，结合前人相关成果，研究膏岩层系的岩性、纵向发育和平面分布特征，分析构造挤压作用对石膏岩流动加厚和平面分布特征的影响。川东南地区中—下寒武统膏岩层系中与膏盐和含膏有关的岩性主要为石膏岩、白云质石膏岩、膏质白云岩与含膏白云岩，纵向上膏岩层系岩性组合和单层厚度变化较大，平面上石膏岩分布广，但累计厚度变化较大；在构造挤压作用下，川东南低陡构造带中—下寒武统石膏岩类常向背斜核部流动，造成石膏岩在背斜轴部明显加厚，揉皱和底辟等伴生构造发育；由于石膏岩的流动性，相应的膏岩层系厚度平面变化与低陡构造带的构造变形部位有相关性，沿低陡构造带的走向膏岩层系厚度在背斜部位一般加厚，在向斜部位减薄较明显。
- 石膏岩 /
- 膏岩层系 /
- 高台组 /
- 龙王庙组 /
- 中—下寒武统 /
- 川东南地区
Abstract: The Middle-Lower Cambrian Longwangmiao Formation and Gaotai Formation in southeastern Sichuan Basin are gypsum rock layer systems, where gypsum rocks are widely developed and considered to be the Sinian to Middle-Lower Cambrian reservoir seals. Based on the drilling data and 2D seismic profile data, and combined with previous research results, this paper studies the lithologic features, vertical development and plane distribution characteristics of the gypsum rock layer system and analyzes the influence of tectonic compression on the flow deformation and plane distribution characteristics of gypsum rock. The gypsum salt and gypsum bearing lithologies in the Middle-Lower Cambrian gypsum rock layer system in the study area mainly include gypsum rock and dolomitic gypsum rock, as well as gypsiferous dolomite and dolomite with gypsum. The lithologic association and single layer thickness of the gypsum rock layer system vary greatly vertically. The gypsum rocks are widely distributed in the plane, but the accumulated thickness changes greatly. Under tectonic compression, the Middle-Lower Cambrian gypsum rocks in the low-steep folds in the southeastern Sichuan Basin usually flowed into the core of the anticline and obviously thickened. Crumpled, diapir and other associated structures developed. Due to the fluidity of gypsum rock, the plane variation of gypsum rock thickness is related to the structural deformation position of the low-folds, which is generally thickened in the anticline along the strike of the low-steep folds and obviously thinned in the syncline.
- gypsum rock /
- gypsum rock layer system /
- Gaotai Formation /
- Longwangmiao Formation /
- Middle-Lower Cambrian /
- southeastern Sichuan Basin

HTML全文

图 1 川东南地区构造纲要及井位、二维地震剖面位置

Figure 1. Structure outline map of southeastern Sichuan Basin and location of wells and seismic sections

下载: 全尺寸图片幻灯片

图 2 川东南地区下组合地层柱状图

Figure 2. Stratigraphic column of lower assemblage in southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

图 3 川东南地区及邻区典型井位龙王庙组—高台组石膏岩类和膏质及含膏岩类累计厚度占地层厚度的百分比

Figure 3. Percentage histogram of accumulated thickness of gypsum rocks, gypsiferous and gypsum-bearing rocks in Longwangmiao-Gaotai formations in typical wells in southeastern Sichuan Basin and its periphery

下载: 全尺寸图片幻灯片

图 4 川东南地区典型钻井龙王庙组—高台组地层及膏岩层纵向分布特征

Figure 4. Vertical distribution of Longwangmiao-Gaotai formations and gypsum rock layers in typical wells in southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

图 5 川东南地区阳1井中寒武统高台组膏岩层系中石膏岩层和膏质白云岩层测井响应特征

Figure 5. Logging response characteristics of gypsum rock layers and gypsiferous dolomite layers in Middle Cambrian Gaotai Formation in well Yang 1, southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

图 6 川东南地区林1井中—下寒武统膏岩层系地震响应特征剖面位置见图 1A—A’。

Figure 6. Seismic response of Middle-Lower Cambrian gypsum rock layer system in well Lin 1, southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

图 7 川东南地区中—下寒武统膏岩层系厚度分布

Figure 7. Thickness of Middle-Lower Cambrian gypsum rock layer system in southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

图 8 川东南中—下寒武统膏岩层系厚度与低陡构造带分布关系

Figure 8. 3D configuration between thickness of Middle-Lower Cambrian gypsum rock layer system and low-steep folds the southeastern Sichuan Basin

下载: 全尺寸图片幻灯片

表 1 川东南及邻区中—下寒武统石膏岩类和膏质及含膏岩类岩性统计

Table 1. Lithologies of Middle-Lower Cambrian gypsum rocks, gypsiferous and gypsum-bearing rocks in southeastern Sichuan Basin and its periphery

井位	石膏岩类		膏质及含膏岩类
井位	石膏岩	白云质石膏岩	膏质白云岩	含膏白云岩	含膏石盐岩	膏质砂(泥)岩
阳深2井	0	0	129.5/26/1/32	2/2/1/1	0	2/2/1/1
阳1井	35/12/0.5/9	17/4/2/7	65.5/12/1/19	15/3/3.5/6	0	0
丁山1井	31.1/7/2/9.5	0	30.3/11/0.8/7	13.8/5/2/5.8	0	0
林1井	13/1/13/13	0	58/5/6/22	0	0	0
座3井	71/3/12/44	0	4/2/2/2	0	0	0
太和1井	97/10/2/28	8/2/4/4	113/12/3/32	5/1/5/5	0	1/1/1/1
合探1井	35/2/16/19	0	0	0	0	0
合12井	0	0	1/1/1/1	0	0	0
荷深1井	7/2/3/4	4/2/2/2	0	0	0	0
自深1井	0	0	17/2/？/？	0	0	0
塔探1井	20/7/1/8	4/2/2/2	28/8/2/7	0	11/1/11/11	0
注：表中数据含义为：累计厚度(m)/层数/单层最小厚度(m)/单层最大厚度(m)。

下载: 导出CSV

参考文献(26)

[1]	林良彪, 陈洪德, 淡永, 等. 四川盆地中寒武统膏盐岩特征与成因分析[J]. 吉林大学学报(地球科学版), 2012, 42(S2): 95-103. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S2012.htm LIN Liangbiao, CHEN Hongde, DAN Yong, et al. Characteristics and genesis of Middle Cambrian gypsum rock in Sichuan Basin[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(S2): 95-103. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S2012.htm
[2]	余一欣, 周心怀, 彭文绪, 等. 盐构造研究进展述评[J]. 大地构造与成矿学, 2011, 35(2): 169-182. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201102001.htm YU Yixin, ZHOU Xinhuai, PENG Wenxu, et al. An overview on salt structures[J]. Geotectonica et Metallogenia, 2011, 35(2): 169-182. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201102001.htm
[3]	ADAM J, GE Zhiyuan, SANCHEZ M. Salt-structural styles and kinematic evolution of the Jequitinhonha deepwater fold belt, central Brazil passive margin[J]. Marine and Petroleum Geo-logy, 2012, 37(1): 101-120. doi: 10.1016/j.marpetgeo.2012.04.010
[4]	王彦青, 陈迎宾, 胡烨, 等. 蒸发环境烃源岩生烃能力探讨: 以川西坳陷雷口坡组为例[J]. 断块油气田, 2018, 25(4): 426-430. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201804004.htm WANG Yanqing, CHEN Yingbin, HU Ye, et al. Discussion on hydrocarbon generation ability of evaporation environment: a case study of Leikoupo Formation in West Sichuan Depression[J]. Fault-Block Oil and Gas Field, 2018, 25(4): 426-430. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201804004.htm
[5]	金之钧, 龙胜祥, 周雁, 等. 中国南方膏盐岩分布特征[J]. 石油与天然气地质, 2006, 27(5): 571-583. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200605003.htm JIN Zhijun, LONG Shengxiang, ZHOU Yan, et al. A study on the distribution of saline-deposit in southern China[J]. Oil & Gas Geology, 2006, 27(5): 571-583. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200605003.htm
[6]	林良彪, 郝强, 余瑜, 等. 四川盆地下寒武统膏盐岩发育特征与封盖有效性分析[J]. 岩石学报, 2014, 30(3): 718-726. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201403011.htm LIN Liangbiao, HAO Qiang, YU Yu, et al. Development characteristics and sealing effectiveness of Lower Cambrian gypsum rock in Sichuan Basin[J]. Acta Petrologica Sinica, 2014, 30(3): 718-726. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201403011.htm
[7]	顾志翔, 何幼斌, 彭勇民, 等. 四川盆地下寒武统膏盐岩"多潟湖"沉积模式[J]. 沉积学报, 2019, 37(4): 834-846. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201904015.htm GU Zhixiang, HE Youbin, PENG Yongmin, et al. "Multiple-lagoon" sedimentary model of the Lower Cambrian gypsum-salt rocks in the Sichuan Basin[J]. Acta Sedimentologica Sinica, 2019, 37(4): 834-846. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201904015.htm
[8]	张玺华, 罗文军, 文龙, 等. 四川盆地寒武纪龙王庙组沉积相演化及石油地质意义[J]. 断块油气田, 2018, 25(4): 419-425. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201804003.htm ZHANG Xihua, LUO Wenjun, WEN Long, et al. Sedimentary facies evolution characteristics and petroleum geological significance of Cambrian Group in Sichuan Basin[J]. Fault-Block Oil and Gas Field, 2018, 25(4): 419-425. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201804003.htm
[9]	徐美娥, 张荣强, 彭勇民, 等. 四川盆地东南部中、下寒武统膏岩盖层分布特征及封盖有效性[J]. 石油与天然气地质, 2013, 34(3): 301-306. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201303007.htm XU Meie, ZHANG Rongqiang, PENG Yongmin, et al. Distribution and sealing effectiveness of Middle-Lower Cambrian evaporite cap rocks in the southeastern Sichuan Basin[J]. Oil & Gas Geology, 2013, 34(3): 301-306. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201303007.htm
[10]	徐安娜, 胡素云, 汪泽成, 等. 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[J]. 天然气工业, 2016, 36(6): 11-20. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201606004.htm XU Anna, HU Suyun, WANG Zecheng, et al. Sedimentary mode and reservoir distribution of the Cambrian carbonate & evaporite paragenesis system in the Sichuan Basin[J]. Natural Gas Industry, 2016, 36(6): 11-20. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201606004.htm
[11]	李双建, 孙冬胜, 郑孟林, 等. 四川盆地寒武系盐相关构造及其控油气作用[J]. 石油与天然气地质, 2014, 35(5): 622-631. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201405007.htm LI Shuangjian, SUN Dongsheng, ZHENG Menglin, et al. Salt-related structure and its control on hydrocarbon of the Cambrian in Sichuan Basin[J]. Oil & Gas Geology, 2014, 35(5): 622-631. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201405007.htm
[12]	彭勇民, 张荣强, 陈霞, 等. 四川盆地南部中下寒武统石膏岩的发现与油气勘探[J]. 成都理工大学学报(自然科学版), 2012, 39(1): 63-69. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201201010.htm PENG Yongmin, ZHANG Rongqiang, CHEN Xia, et al. Discovery and significance of the Middle-Lower Cambrian gypsolith in the south of Sichuan Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2012, 39(1): 63-69. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201201010.htm
[13]	LIU Hong, TAN Xiucheng, LI Yonghao, et al. Occurrence and conceptual sedimentary model of Cambrian gypsum-bearing evaporites in the Sichuan Basin, SW China[J]. Geoscience Frontiers, 2018, 9(4): 1179-1191.
[14]	胡素云, 石书缘, 王铜山, 等. 膏盐环境对碳酸盐岩层系成烃、成储和成藏的影响[J]. 中国石油勘探, 2016, 21(2): 20-27. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201602003.htm HU Suyun, SHI Shuyuan, WANG Tongshan, et al. Effect of gypsum-salt environment on hydrocarbon generation, reservoir-forming and hydrocarbon accumulation in carbonate strata[J]. China Petroleum Exploration, 2016, 21(2): 20-27. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201602003.htm
[15]	唐永, 周立夫, 陈孔全, 等. 川东南构造应力场地质分析及构造变形成因机制讨论[J]. 地质论评, 2018, 64(1): 15-28. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201801004.htm TANG Yong, ZHOU Lifu, CHEN Kongquan, et al. Analysis of tectonic stress field of southeastern Sichuan and formation mechanism of tectonic deformation[J]. Geological Review, 2018, 64(1): 15-28. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201801004.htm
[16]	李英康, 高建伟, 韩健, 等. 扬子块体两侧造山带地壳推覆的地球物理证据及其地质意义[J]. 中国科学(地球科学), 2019, 49(4): 687-705. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201904005.htm LI Yingkang, GAO Jianwei, HAN Jian, et al. Geophysical evidence for thrusting of crustal materials from orogenic belts over both sides of the Yangtze Block and its geological significance[J]. Science China Earth Sciences, 2019, 62(5): 812-831. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201904005.htm
[17]	LIU Shugen, DENG Bin, LI Zhiwu, et al. Architecture of basin-mountain systems and their influences on gas distribution: a case study from the Sichuan Basin, South China[J]. Journal of Asian Earth Sciences, 2012, 47: 204-215.
[18]	CLARK M K, SCHOENBOHM L M, ROYDEN L H, et al. Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patterns[J]. Tectonics, 2004, 23(1): TC1006.
[19]	RICHARDSON N J, DENSMORE A L, SEWARD D, et al. Extraordinary denudation in the Sichuan Basin: insights from low-temperature thermochronology adjacent to the eastern margin of the Tibetan Plateau[J]. Journal of Geophysical Research: Solid Earth, 2008, 113(B4): B04409.
[20]	YAN Danping, ZHOU Meifu, SONG Honglin, et al. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)[J]. Tectonophysics, 2003, 361(3/4): 239-254.
[21]	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(S2): 21-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB2012S2002.htm YANG Wei, XIE Wuren, WEI Guoqi, et al. Sequence lithofacies paleogeography, favorable reservoir distribution and exploration zones of the Cambrian and Ordovician in Sichuan Basin, China[J]. Acta Petrolei Sinica, 2012, 33(S2): 21-34. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB2012S2002.htm
[22]	王淑丽, 郑绵平, 焦建. 上扬子区寒武系蒸发岩沉积相及成钾潜力分析[J]. 地质与勘探, 2012, 48(5): 947-958. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201205012.htm WANG Shuli, ZHENG Mianping, JIAO Jian. Sedimentary facies of the Cambrian evaporites in the Upper Yangtze region and their potash-forming potential[J]. Geology and Prospecting, 2012, 48(5): 947-958. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201205012.htm
[23]	门玉澎, 许效松, 牟传龙, 等. 中上扬子寒武系蒸发岩岩相古地理[J]. 沉积与特提斯地质, 2010, 30(3): 58-64. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201003009.htm MENG Yupeng, XU Xiaosong, MOU Chuanlong, et al. Sedimentary facies and palaeogeography of the evaporates in the Middle Upper Yangtze area[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(3): 58-64. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201003009.htm
[24]	邹灏. 四川盆地寒武系膏盐岩特征研究[D]. 成都: 成都理工大学, 2011. ZOU Hao. Characteristics of the Cambrian gypsum-salt rocks in Sichuan Basin[D]. Chengdu: Chengdu University of Technology, 2011.
[25]	JACKSON M P A, TALBOT C J. External shapes, strain rates, and dynamics of salt structures[J]. GSA Bulletin, 1986, 97(3): 305-323.
[26]	刘树根, 马永生, 蔡勋养, 等. 四川盆地震旦系-下古生界天然气成藏过程和特征[J]. 成都理工大学学报(自然科学版), 2009, 33(4): 345-354. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200904000.htm LIU Shugen, MA Yongsheng, CAI Xunyang, et al. Characteristic and accumulation process of the natural gas from Sinian to Lower Paleozoic in Sichuan Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2009, 33(4): 345-354. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200904000.htm