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随南地区武当岩群地层层序
引用本文:李雄伟,汪国虎.随南地区武当岩群地层层序[J].资源环境与工程,2000,14(1):3-11,19.
作者姓名:李雄伟  汪国虎
作者单位:湖北省区域地质矿产调查所
摘    要:在安居镇、随州市、均川幅一比五万区调成果的基础上,通过广泛综合对比分析,认为随南地区武当岩群(原随县群)实为“大套有序,局部无序”之构造(岩石)地层单位,由下至上可划分为三个岩石组:一岩石组(变沉积岩岩组)、二岩组(变火山岩岩组)、三岩组(变沉积火山岩岩组)、并对建立三岩组正式组级构造(岩石)地层单位名称进行了讨论。

关 键 词:随南地区  武当岩群  地层层序  地质特征  前震旦纪

STRATIGRAPHIC SEQUENCE OF WUDANG ROCK GROUP IN SOUTHERN SUIZHOU,HUBEI
Li Xiongwei,Wang Guohu.STRATIGRAPHIC SEQUENCE OF WUDANG ROCK GROUP IN SOUTHERN SUIZHOU,HUBEI[J].Resources Environment & Engineering,2000,14(1):3-11,19.
Authors:Li Xiongwei  Wang Guohu
Affiliation:Hubei Survey of Regional Geology and Mineral Resources
Abstract:According to the 1:50000 geological mapping data of Anjuzhen Sheet,Suizhoushi Sheet and Junchuan Sheet, this paper proposed that Wudang Rock Group (original Suixian Group) can be regarded as a overall ordered but local disordered"tectono(rock)-stratigraphic unit which can be divided into three rock formations from top to bottom as following:First rock formation( metasedimentary rock formation) , Second rock formation(metavolcanic rock formation) and Third rock formation( metasedimental-volcanic rock formation) whose formal names are discussed as well.
Keywords:Southern Suizhou  Wudang Rock Group  stratigraphic  sequence  stratigraphic unit  
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