首页|碳酸盐岩致密气成藏地质条件分析——以四川盆地大安区块茅一段为例

碳酸盐岩致密气成藏地质条件分析——以四川盆地大安区块茅一段为例

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四川盆地大安区块大安2、大安1、大坝1井相继在茅一段石灰岩中获得天然气发现,由于勘探程度低,对天然气成藏地质条件认识不清.文中以该区茅一段为例,综合野外地质调查、单井分析,以及有机碳分析、薄片鉴定、X射线衍射、场发射扫描电镜等测试成果,开展烃源岩岩性、地球化学特征、储层沉积相、矿物组分、微观孔隙特征及含气系统研究,分析致密气成藏地质条件,建立成藏模式.研究结果表明:茅一段眼球、眼皮灰岩沉积受控于中缓坡沉积环境,构成了 自生自储的物质基础;眼皮灰岩是一套有效烃源岩,提供充足的烃源供给;眼球、眼皮灰岩为低孔低渗致密储层,互层状叠置,纳米孔、微米孔发育,微裂缝贯通穿插,有利于大面积成藏;成藏模式为致密气源储一体、源内聚集、就近吸附,天然气动态生成,动态聚集,不易逸散;该区在燕山中晚期成藏,喜马拉雅期保存,中缓坡的眼皮灰岩带具有高脆性、中高TOC、中含气性特点,是致密气有利勘探方向.
Analysis on geological conditions of tight gas accumulation in carbonate rock:a case study of Mao 1 Member in Da'an block,Sichuan Basin
Natural gas has been discovered successively in the limestone of Mao 1 Member in Da'an block of Sichuan Basin,including Well Da'an 2,Well Da'an 1,and Well Daba 1.However,geological conditions of natural gas accumulation are unclear because of the low degree of exploration.Taking Mao 1 Member in Da'an block as an example,combining field geological survey,single well analysis,organic carbon analysis,thin section identification,X-ray diffraction,field emission scanning electron microscopy and other test results,the source rock lithology,geochemistry charateristics,reservoir sedimentary facies,mineral component,micro pore characteristics and gas bearing system analysis are studied,geological conditons of tight gas accumulation of Mao 1 Member in Da'an block are analyzed,and the reservoir forming model is established.The results indicate that the Mao 1 Member eyeball and eyelid limestone deposits are controlled by the middle gentle slope sendimentary environment,which forms the material basis for self-generation and self-accumulation.Eyelid limestone is a set of effective source rock,which ensures sufficient supply of hydrocarbon source.The eyeball and eyelid limestone are tight reservoirs with low porosity,low permeability,displaying interlayered stacking.Nano and micro pores are developed in the reservoir with interconnected micro cracks,which are conducive to large-scale reservoir formation The reservoir forming model is tight gas source-reservoir integration,in-source accumulation,and nearby adsorption.Natural gas is dynamically generated and gathered,which is not easy to escape.The area was formed in the Middle and Late Yanshan period and preserved during the Himalayan period.The eyelid limestone of the middle gentle slope facices has characteristics of high brittleness,medium high TOC and medium gas content,making it a favorable direction for tight gas exploration.

tight gascarbonate rockaccumulationMao 1 MemberDa'an blockSichuan Basin

栗维民、马立桥、何方雨、王鹏万、计玉冰、徐云俊、徐政语、曹全斌、贾丹

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中国石油浙江油田分公司,浙江杭州 310023

中国石油杭州地质研究院,浙江杭州 310023

中国石油天然气集团有限公司碳酸盐岩储集层重点实验室,浙江杭州 310023

致密气 碳酸盐岩 成藏 茅一段 大安区块 四川盆地

中国石油油气和新能源分公司项目中国石油浙江油田分公司项目

2022KT01042022-N/G-72546

2024

断块油气田
中原石油勘探局

断块油气田

CSTPCD北大核心
影响因子:1.493
ISSN:1005-8907
年,卷(期):2024.31(2)
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