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盆地构造演化沉积环境及非煤能源矿产评述
Comments on structural evolution,depositional environment and minerals of non-coal energy
【摘要】 阜新盆地是中生代陆相断陷型盆地,由太古界、中元古界组成盆地基底,其上接受了晚中生代地层沉积,包括沙海组、阜新组两套含煤岩系。盆地的沉积充填组合反映了盆地构造演化的阶段性,而同沉积构造的演化又控制了沉积环境。通过研究盆地构造演化及沉积特征,论述了煤层气、砂体气、石油、地热等相关非煤矿产能源的形成条件及开发远景,并提出进一步勘探开发的建议。
【Abstract】 Fuxin basin is a continental graben basin of the Mesozoic.Based on the strata of the Archean and the mid-Proterozoic it was filled with two coal-bearing series of rocks during the late Mesozoic,named Shahai Group and Fuxin Group.Its depositional combination is a reflction of successive structural evolution of the basin,and the evolution of synsedimentary structures controls depositional environment of the basin.The paper discusses original conditions related to minerals of non-coal energy resources and development perspective of them,such as coalbed methane,gas in sandstone.petroleum and geothermal energy,etc.some suggestions are given for futher exploration and development of the minerals in the basin.
【Key words】 structure evolution; deposit environment; coal seam gas; sand-body gas; petroleum; terrestrial heat;
- 【文献出处】 辽宁工程技术大学学报 ,Journal of Liaoning Technical University , 编辑部邮箱 ,2003年05期
- 【分类号】P512.2
- 【被引频次】9
- 【下载频次】144