天然气地球化学

川东南地区震旦系――志留系下组合有效烃源岩综合研究

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  • [1]成都理工大学油气藏地质及开发工程国家重点实验室,四川成都610059 [2]中国石化南方分公司勘探开发科学研究院,云南昆明650200 [3]四川石油管理局,四川成都610051 [4]西南石油大学油气藏地质及开发工程国家重点实验室,四川成都610500
刘若冰(1973-),男,河南邓州人,工程师,在读博士,从事油气田勘探开发研究工作.

收稿日期: 2006-06-19

  修回日期: 2006-08-08

  网络出版日期: 2006-12-10

基金资助

国家自然科学基金项目(编号:90210022);四川省青年学科带头人培养基金项目联合资助.

COMPREHENSIVE RESEARCH OF EFFECTIVE HYDROCARBON SOURCEROCK OF LOWER STRATA FROM SINIAN TO SILURIAN SYSTEM INSOUTHEAST AREA OF SICHUAN PROVINCE

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  • 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology,Chengdu 610059, China;2.Southern Exploration and Development Company, SINOPEC, Kunming 650200, China;3.CNPC Sichuan Petroleum, Chengdu 610051, China; 4.State Key Laboratory of Oil and Gas ReservoirGeology and Exploitation, Southwest Petroleum University, Chengdu 610050, China

Received date: 2006-06-19

  Revised date: 2006-08-08

  Online published: 2006-12-10

摘要

震旦系志留系是川东南地区油气勘探的新层系、新领域,具有较好的勘探前景,但勘探程度极低。以地表露头、钻井岩芯样品为基础,通过地球化学特征、气源和沥青源对比分析,明确了下寒武统牛蹄塘组、下奥陶统五峰组下志留统龙马溪组灰黑色泥岩、页岩为区内震旦系一志留系主要烃源岩,其中下志留统龙马溪组烃源岩最为发育,且其发育时期与大地构造格局或沉积盆地性质发生重大变革的转换时期相吻合,还明确了主要烃源岩横向展布特征及其构造沉积主控因素。

本文引用格式

刘若冰;田景春;魏志宏;张明文;钟水清;张光华;王碧; . 川东南地区震旦系――志留系下组合有效烃源岩综合研究[J]. 天然气地球科学, 2006 , 17(6) : 824 -828 . DOI: 10.11764/j.issn.1672-1926.2006.06.824

Abstract

The strata from Sinian to Silurian system are new formations and fields with better exploration potential in southeast area in Sichuan province, but the degree of prospecting is quite low. Based on the ground outcrops and drilling core samples, contrasted and analysed the organic geochemical characteristic, gas source and asphalt source, it clarifies that the grey-black mudstone and shale are main hydrocarbon source rocks, included Niu-Ti-Tang formation of lower Cambrian system, Wu-feng formation of lower Ordovieian system and Long-ma-xi formation of lower Silurian system, whose developing periods consist with the converting periods of earth tectonic framework or the important transformation of sedimentary basin character. The hydrocarbon source rock of Long-ma-xi formation of lower Silurian system is most developing among them. At the same time, it also clarifies the lateral continuity and the main controlling factor of the structure and deposition of the chief hydrocarbon source rock.

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