成岩伊利石K—Ar年龄分析及其意义

成岩伊利石K—Ar年龄分析及其意义

吴劲薇1，陈小明2，杨忠芳2 3

1. 南京大学学报编辑部，江苏南京 210093; 2. 南京大学成矿机制研究国家重点实验室，江苏南京 210093; 3. 中国地质大学，北京 100083

收稿日期:2001-12-20 修回日期:2001-12-20 出版日期:2001-12-20 发布日期:2001-12-20

Diagenetic Illite K-Ar Age Analysis and Its Significance

WU Jing-wei1, CHEN Xiao-ming2, YANG Zhong-fang3;2

1. Editorial Board, Journal of Nanjing University, Nanjing 210093; 2. State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093; 3. China University of Geosciences, Beijing 10083

Received:2001-12-20 Revised:2001-12-20 Online:2001-12-20 Published:2001-12-20

摘要/Abstract

摘要： 烃源岩何时达到最高温度以及其经历加热时与成油构造的时间关系，一直是油气勘探研究中的关系问题。成岩作利石的K－Ar年龄可以用来确定碳氢化合物的形成时间，但由于无法将成岩伊利石从沉积岩中单独分离出来，因工源岩达到最高温度的时间一直不能确定，伊利石K－Ar年龄分析（IAA）方法的建立，使成岩伊利石年龄的获得成为可能。利用该方法对塔里木盆地某地区2772m处的奥陶系烃源层达到最高温度的时代进行了分析，结果表明，该地层是在上志留纪（408Ma)达到最高温度的。

Abstract: The timing of hydrocarbon generation is of particular concern in resource exploration. When were the solid organic matters heated to form oil and gas? Because illite forms in rocks in response to heating in the same temperature range as oi1 formation, its K-Ar age is all important parameter. Illite in reservoir sedimentary rocks is a mixture of detrital and diagenetic components. Defining reliable diagenetic ages of illitization in sedimentary rocks still remains a formidable challenge because separation of the diagenetic component is impossible, even if it is carried out down to the grain size as small as

吴劲薇，陈小明，杨忠芳. 成岩伊利石K—Ar年龄分析及其意义[J]. J4.

WU Jing-wei1, CHEN Xiao-ming2, YANG Zhong-fang3;2. Diagenetic Illite K-Ar Age Analysis and Its Significance[J]. J4.