东胜煤田延安组岩相古地理
Paleogeographic of the Yan'an Formation in Dongsheng Coalfield
根据对东胜区西北方向在建色连煤矿1号井巷道揭露地层岩石特征及以往勘探阶段的大量钻孔资料的分析研究,作者对该区含煤地层侏罗系中下统延安组地层的岩石特征及其沉积环境演化予以分段论述。研究发现:延安组(J1-2y)为一套灰色、深灰色的砂岩、粉砂岩、砂质泥岩、泥岩及煤层的组合。其沉积环境演化从下至上是由河流沉积体系逐渐发展到湖湾或湖泊三角洲沉积体系,最后又转变成河流沉积体系。
Based on the analysis and study of the petrology features of the revealed stratum of No. 1 well tunnel in Selian coalmine which is under construction, northwest of Dongsheng area, and a large number of borehole datas in exploration stage, the auther has expounded the relationship between petrology features of coal bearing stratum and evolution of sedimentary environment in the Middle- Lower Jurassic Yan'an Formation. The results shows that the Yan'an Formation(J1-2y) is a set of dark gray sandstone, siltstone, silty mudstone, mudstone and coal. There are gradations from the fluvial sedimentary system to the lake delta sedimentary system from the base upwards in the Yan'an Formation , and finally into the fluvial sedimentary system.
刘小亮
地质学矿山地质、矿山测量矿山建设、矿山设计
延安组岩石特征沉积演化鄂尔多斯盆地东胜
Yan'an Formationpetrology featuresevolution of sedimentary environmentOrdos BasinDongsheng area
刘小亮.东胜煤田延安组岩相古地理[EB/OL].(2010-12-30)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201012-1313.点此复制
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