地质通报2013，Vol.32Issue(8)：1253-1259,7.
内蒙古突泉盆地双低阻层的发现及其地质意义
The discovery of two conductive layers in Tuquan basin, Inner Mongolia, and its geological significance
摘要
Abstract
MT and AMT profiling was conducted in Mangniuhai sag area of Tuquan basin so as to evaluate the potential of oil and gas resources associated with the late Paleozoic and Mesozoic strata.The results of MT and AMT profile survey shows that there are two thick and transverse continuous distribution conductive layers under the volcanic layer at the depth of 800～2000m and 2000～8000m,respectively.By combining drilling material and regional geological material,the authors consider that the first conductive layer represents the coal strata of early Jurassic,and the second conductive layer represents the mudstone layer of upper Paleozoic.Based on the results of ground hydrocarbon source rocks survey,it can be predicted that both the conductive layers could contain excellent hydrocarbon source rocks,which means that there exists great potential for detecting the upper Paleozoic and the early Mesozoic hydrocarbon resources in Tuquan basin.关键词
内蒙古突泉盆地/大地电磁测深/低阻层/有利烃源岩Key words
Tuquan basin/ magnetotelluric survey/ conductive layers/ favorable hydrocarbon source rocks分类
天文与地球科学引用本文复制引用
方慧,钟清,陈树旺..内蒙古突泉盆地双低阻层的发现及其地质意义[J].地质通报,2013,32(8):1253-1259,7.基金项目
中国地质调查局项目(编号:1212011120971)和国土资源部公益性行业科研专项项目(编号:SinoProbe-01-04) （编号:1212011120971）
