镜质组反射率测试及其所反映的构造应力场

蒋建平,高广运,康继武.镜质组反射率测试及其所反映的构造应力场.地球物理学报,2007,50(1):138～145

Jiang J P ,G ao G Y,K ang J W.T ests on vitrinite reflectance of coal and analysis of tectonic stress field.Chinese J .G eophys .(in Chinese ),2007,50(1):138～145

镜质组反射率测试及其所反映的构造应力场

蒋建平1

,高广运2

,康继武

3

1上海海事大学交通运输学院,上海　2001352同济大学地下建筑与工程系,上海　2000923河南理工大学资源与环境工程系,焦作　454000

摘　要　为了利用煤镜质组反射率推断豫北构造应力场,基于构造应力是造成镜质组反射率各向异性(VRA )的主要控制因素,对在豫北焦作、安阳、鹤壁三个矿区井下取的定向煤样品进行了室内显微镜下反射率测试,对测试数据按有关公式进行计算后就得出了由最大反射率值、中间反射率值、最小反射率值为轴组成的镜质组反射率椭球体(VRI ).结果表明,研究区煤样显示二轴晶正光性,它们经过了强烈的构造变形,研究区煤样镜质组反射率各向异;由镜质组反射率椭球体(VRI )得出的豫北构造应力场与钻探、节理统计、河南省区域构造应力场分析等方法得出的应力场基本上是吻合的,但也有一定的区别,主要体现在应力场到安阳、鹤壁矿区后发生了向左的偏转.总之,利用煤镜质组反射率各向异性推断构造应力场的方法是可行的、是有效的.关键词　镜质组反射率,构造应力场,煤,豫北文章编号　0001-5733(2007)01-0138-08

中图分类号　P313

收稿日期　2005-11-01,2006-10-29收修定稿

基金项目　上海市交通运输规划与管理重点学科建设项目和上海市教委科研项目(05FZ 03)资助.

作者简介　蒋建平,男,1966年生,2002年6月于南京大学获博士学位,2004年5月于同济大学博士后出站.现在上海海事大学任教,主要从事

岩土工程、港航工程和工程地质方面的教学和研究工作.E 2mail :jjpwx @1631com

T ests on vitrinite reflectance of coal and analysis of tectonic stress field

J IANGJian 2Ping 1,G AO G uang 2Y un 2,K ANGJi 2Wu 3

1College o f Tra ffic Transportation ,Shanghai Maritime Univer sity ,Shanghai 200135,China 2Department o f G eotechnical Engineering ,Tongji Univer sity ,Shanghai 200092,China

3College o f Resource and Environment Engineering ,H enan Univer sity o f Science and Technology ,Jiao zuo 454000,China

Abstract In order to deduce the tectonic stress field in North Henan by coal vitrinite reflectance ,based on the principle that the tectonic stress is the main controlling factor of the vitrinite reflectance anis otropy (VRA ),we have performed tests of coal vitrinite reflectance under microscope for directional coal specimen collected from Jiaozuo ,Anyang ,Hebi mining field in Henan province ,and gained vitrinite reflectance ellips oids (VRI )made up of reflectance maximum ,reflectance middle value and reflectance minimum through s ome calculation to testing data.The results show that coal specimen in studied area indicate indicatrix of optical biaxial crystal ,which su ffered from intense tectonic deformation and the vitrinite reflectance anis otropy (VRA )is induced by tectonic stress.The tectonic stress field of North Henan obtained from vitrinite reflectance ellips oids (VRI )is accordant basically with the tectonic stress field acquired from other methods ,such as drilling ,joint statistics and Henan province territorial tectonic stress field analysis ,but there is small difference that the tectonic stress field has left deflexion in Anyang and Hebi.In short ,the method deducing tectonic stress field by vitrinite reflectance anis otropy (VRA )is feasible and effective.

K eyw ords Vitrinite reflectance ,T ectonic stress field ,C oal ,North Henan

第50卷第1期2007年1月

地　球　物　理　学　报

CHI NESE JOURNA L OF GE OPHY SICS

V ol.50,N o.1

Jan.,2007