川东北地区长兴组-飞仙关组碳酸盐岩台地层序充填结构及成藏效应

陈洪德; 钟怡江; 侯明才; 林良彪; 董桂玉; 刘家洪

doi:10.11743/ogg20090503

四川盆地及邻区油气地质 | 浏览量 : 0 下载量: 562 CSCD: 0

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川东北地区长兴组-飞仙关组碳酸盐岩台地层序充填结构及成藏效应
Sequence styles and hydrocarbon accumulation effects of carbonate rock platform in the Changxing-Feixianguan formations in the northeastern Sichuan Basin
2009年30卷第5期页码：539-547
网络首发：2009-10-25，

纸质出版：2009
DOI： 10.11743/ogg20090503
稿件说明：

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陈洪德, 钟怡江, 侯明才, 等. 川东北地区长兴组-飞仙关组碳酸盐岩台地层序充填结构及成藏效应[J]. 石油与天然气地质, 2009,30(5):539-547. DOI： 10.11743/ogg20090503.

Chen Hongde, Zhong Yijiang, Hou Mingcai, et al. Sequence styles and hydrocarbon accumulation effects of carbonate rock platform in the Changxing-Feixianguan formations in the northeastern Sichuan Basin[J]. 2009, 30(5): 539-547. DOI： 10.11743/ogg20090503.

摘要

川东北地区长兴组和飞仙关组可分别划分为两个Ⅱ型层序:PSQ1

PSQ2

TSQ1和TSQ2。除TSQ2由TST

EHST和LHST组成以外

其他层序均由TST和HST组成。在古断裂的控制下

长兴期至飞仙关期川东北碳酸盐岩台地呈现出独特的台-盆相间以及台地内的滩-洼相间沉积格局。古断裂和相对海平面变化分别通过控制沉积格局和沉积环境的水体能量变化而制约碳酸盐生产率和产出类型

从而影响碳酸盐岩层序充填结构特征。层序充填结构中发育的各成藏要素构成了川东北礁、滩气藏完整的生储盖组合。

Abstract

The Changxing and Feixianguan formations in northeastern Sichuan Basin can both be divided into two type-Ⅱ sequences:PSQ1

PSQ2

TSQ1 and TSQ2.The TSQ2 sequence can be subdivided into TST

EHST and LHST

and the rest can be divided into TST and HST.Controlled by fossil fractures

during Changxing-Feixianguan period

unique sedimentary pattern of platform alternating with basin and shoal alternating with topographic low occurred in the carbonate rock platform in northeastern Sichuan Basin.The fossil fractures and relative sea-level changes influenced the productivity and type of carbonate by controlling sedimentary pattern and water energy change

and further influenced the sequence structures of carbonate rocks.Hydrocarbon pooling elements developed in the sequence structure constitute the integrated source-reservoir-caprock assemblages of reef and shoal gas reservoirs in northeastern Sichuan Basin.