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河西走廊东部石炭系展布及找煤方向
引用本文:毛明陆,刘池洋.河西走廊东部石炭系展布及找煤方向[J].煤田地质与勘探,1994,22(6):1-4.
作者姓名:毛明陆  刘池洋
作者单位:西北大学含油气盆地研究所
摘    要:河西走廊东部石炭系发育、展布受晚古生代前陆盆地控制。虽然以武威为界的东、西两部存在一定差异,但均具有沉降中心和聚煤中心由南向北迁移,海浸方向由SW→SWW→NWW变化的特征。聚煤中心可能主要位于西部中央隆起南缘及东部靖远磁窑一带,北祁连逆冲推覆体下及山前可能也有较好的找煤前景。

关 键 词:含煤建造  煤田预测  河西走廊  找煤方向

THE DISTRIBUTION OF THE CARBONIFEROUS SYSTEM AND THE ORIENTATION FOR COAL EXPLORATION IN THE EASTERN PART OF THE HEXI CORRIDOR
Mao Minglu, Liu Chiyang, Zhao Zhongyuan.THE DISTRIBUTION OF THE CARBONIFEROUS SYSTEM AND THE ORIENTATION FOR COAL EXPLORATION IN THE EASTERN PART OF THE HEXI CORRIDOR[J].Coal Geology & Exploration,1994,22(6):1-4.
Authors:Mao Minglu  Liu Chiyang  Zhao Zhongyuan
Abstract:he development and distribution of the carboniferous system in the eastern part of the Hexi corridor were controlled by the foreland basin of the later Palaeozoic period. Although there are differences between regions which lie to the east and west of Wuwei county, both of the two regions have the same features of subsidence center and coal-forming center which migrated from south to north, and the change of orientation of transgression is SW-SWW-NWW. The coal-forming center is supposed to be situated at the southern edge of the western middle rising and nearby. Under the thrust faults and in front of the niorthern Qilian mountains there may be a better prospect for further exploration.
Keywords:coal-bearing formation  Carboniferous Period  ctructural controls  paleogeopraphic controls  orientation for coal explorition  Hexi corridor
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