四川盆地三叠纪蒸发岩盆地形成环境及白云岩储层

陈莉琼; 沈昭国; 侯方浩; 方少仙

doi:10.11781/sysydz201004334

四川盆地三叠纪蒸发岩盆地形成环境及白云岩储层

doi: 10.11781/sysydz201004334

1.
中国石油化工股份有限公司江苏油田分公司地质研究院, 江苏扬州 225009
2. 西南石油大学成都 610500
3. 中国石油天然气股份有限公司杭州石油地质研究院, 杭州 310023

基金项目: 四川省重点学科建设项目(SZD0414)资助

详细信息

作者简介:
陈莉琼(1962- ),女,高级工程师,主要从事石油勘探综合研究.E-mail:chenliq@joeco.com.cn.

中图分类号: TE121.1
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出版历程
- 收稿日期: 2010-02-09
- 修回日期: 2010-06-08
- 刊出日期: 2010-08-28

FORMATION ENVIRONMENT OF TRIASSIC EVAPORATE ROCK BASIN AND DOLOSTONE RESERVOIRS IN THE SICHUAN BASIN

1.
Institute of Petroleum Geology, Jiangsu Oil field, SINOPEC, Yangzhou, Jiangsu 225009, China
2. Southwest Petroleum University, Chengdu, Sichuan 610500, China
3. Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou, Zhejiang 310023, China

摘要

摘要: 四川盆地中、下三叠统嘉陵江组二段—中三叠统雷口坡组厚达1 500 m以上,主要为白云岩、硬石膏岩和石盐岩,夹少量石灰岩地层组合,其中白云岩是盆地内天然气主产层之一。嘉陵江初期,四川盆地周边山系不断隆升,基底下陷东倾,周期性干热气候促使盆地由开放陆棚向局限盆地转变。嘉陵江早中期,干热气候使盆内海水浓缩,在建南及万县等地形较低处沉积白云岩—硬石膏岩地层。嘉陵江中期—雷口坡期,江南古陆急剧隆升、向西北挤压,七矅山、泸州—开江水下隆起相继形成,迫使盆地不断向西迁移,形成深坳陷高含盐盆地,并与外海隔绝,广泛沉积以白云岩—硬石膏岩—石盐岩为主的地层组合,局部见钙芒硝岩和杂卤石岩。白云岩储层除发育晶间孔外,亦有溶蚀孔隙,其上覆膏盐层是良好的区域盖层。
- 储层 /
- 白云岩 /
- 嘉陵江组 /
- 雷口坡组 /
- 三叠系 /
- 蒸发岩盆地 /
- 四川盆地
Abstract: The strata thickness from Second Member of Jialingjiang Formation to Leikoupo Formation in the Sichuan Basin is over 1 500 m.It is composed of dolostone,anhydrite,halilith and interbedded limestone,among which the dolostone is one of the main gas reservoirs in the basin.In the early Jialingjiang stage,the mountain system around the Sichuan Basin keeps uplifting,and the base depresses and dips eastwards.Periodically dry and hot weather makes the basin turn from open shelf to constrained basin.In the early-middle Jialingjiang stage,dry and hot weather makes sea water within the basin concentrate.A set of dolostone and anhydrite formation deposits at the lower land of Jiannan and Wanxian.From the late Jialingjiang stage to the Leikoupo stage,the Jiangnan old land uplifts rapidly and compresses northwestward.The underwater uplifts in Qiyaoshan and Luzhou-Kaijiang are formed,which drive the basin to migrate westwards.The basin with deep depression and high salinity is formed and isolated from open sea.A formation association dominated by dolostone,anhydrite and halilith is massively deposited.Locally,there exists glauberite and polyhalite.The dolostone reservoirs develop dissolved pores in addition to inter-crystal pores,and the over-lying anhydrite and salt rocks are good regional cover rocks.
- reservoir /
- dolostone Jialingjiang Formation /
- Leikoupo Formation /
- Triassic /
- evaporate rock basin /
- Sichuan Basin /

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参考文献(11)

[1]	张继铭,黄鉴平.四川盆地碳酸盐岩油气田[J].天然气勘探与开发,1984,(4):1-94.
[2]	四川油气区石油地质志编写组.中国石油地质志(卷10)四川油气区[M].北京:石油工业出版社,1989:5-8.
[3]	崔德树,魏凌琛.早、中三叠世四川盆地古地理概况及与油气关系探讨[G]/岩相古地理文集编辑部.岩相古地理文集(2).北京:地质出版社,1986:53-64.
[4]	朱洪发,刘翠章,林傅律.四川盆地中下三叠统成盐古地理景观、成盐机理及钾盐预测[G]/岩相古地理文集编辑部.岩相古地理文集(4).北京:地质出版社,1988:117-128.
[5]	郭正吾,邓康龄,韩永辉,等.四川盆地形成与演化[M].北京:地质出版社,1996:67-75.
[6]	冯增昭.沉积岩石学(下册)[M].2版.北京:石油工业出版社,1993:1-8.
[7]	中国地质科学院地质研究所,武汉地质研究院.中国古地理图集[M].北京:地质出版社,1985:53-56.
[8]	侯方浩,方少仙,赵敬松,等.鄂尔多斯盆地奥陶系碳酸盐岩储层图册[M].成都:四川人民出版社,2002:1-2,8-10.
[9]	侯方浩,方少仙,董兆雄,等.鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征[J].沉积学报,2003,21(1):106-112.
[10]	吴应林,袁敬阆.上扬子地区三叠纪蒸发岩的成因和相模式[M].北京:地质出版社,1985:132-152.
[11]	READING H G.沉积环境和相[M].周明鉴,译.北京:科学出版社,1985.