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作 者:李斌 葛栋锋 宋子辉 Li Bin;Ge Dongfeng;Song Zihui(Urumqi Geological Brigade of Xinjiang Uyghur Autonomous Region Geological Bureau,Urumqi,Xinjiang,830000,China;School of Mining Engineering and Geology Xinjiang Institute of Engineering,Urumqi,Xinjiang,830023,China;College of Earth Sciences and Engineering,Shandong University of Science and Technology,Qingdao,Shandong,266400,China)
机构地区:[1]新疆维吾尔自治区地质局乌鲁木齐地质大队,新疆乌鲁木齐830000 [2]新疆工程学院矿业工程与地质学院,新疆乌鲁木齐830023 [3]山东科技大学地球科学与工程学院,山东青岛266400
出 处:《新疆地质》2024年第4期587-592,共6页Xinjiang Geology
摘 要:通过对准东煤田五彩湾矿区下侏罗统八道湾组开展沉积学、层序地层学研究,分析在层序地层格架下可采煤层的分布特征和煤层聚集的主要控制因素,总结聚煤规律。八道湾组煤层主要发育于两期湖扩体系域沉积期的滨浅湖相区域,区内湖扩体系域滨浅湖相向区外西、南、东侧仍有较大的展布区域,具进一步找煤潜力。Sedimentology and sequence stratigraphy of badaowan Formation in Wucaiwan mining area of Zhundong coalfield,are analyzed by using the methods of coal geology and sequence stratigraphy,and the distribution characteristics of coalbed under the sequence stratigraphy framework are discussed,the main controlling factors of coalbed accumulation are analyzed,and the law of coalbed accumulation is preliminarily summarized.The results show that the coal seams of badaowan Formation are mainly developed in the coastal and shallow lake area during the sedimentary period of the two-stage lake expansion system tract,and the coastal and shallow lake in the inner lake expansion system tract still spread to the west,south and east of the area.Therefore,there is a potential for further coal exploration in the west,south and east of the area.
分 类 号:P539.2[天文地球—古生物学与地层学] P612[天文地球—地质学]
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