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大东沟砂砾岩地质特征
引用本文:刘培喜. 大东沟砂砾岩地质特征[J]. 吉林地质, 1997, 16(4): 42-48
作者姓名:刘培喜
作者单位:地矿部吉林地勘局第六地质调查所
摘    要:汪清县东北部红光,六道崴子一带,北东向晚三叠世火山断陷盆地西侧,出露一套变砂砾岩地层,本文重点论述了该地层的分布特征、层序特征、岩石特征、岩相古地理特征和地层对比及时代确定。

关 键 词:砂砾岩 变质岩 晚二叠世 地质特征

THE GEOLOGICAL FEATURES OF THE DADONGGOU SAND CONGLOMERATE
Liu Peixi. THE GEOLOGICAL FEATURES OF THE DADONGGOU SAND CONGLOMERATE[J]. Jilin Geology, 1997, 16(4): 42-48
Authors:Liu Peixi
Abstract:In the Hongguang and Liudaowaizi areas,northeastern Wangqing County,the western part of the late Triassic EN trending volcanic fault basin,a series of meta-sandstone and conglomerate with metapelite are outcropped.In this paper,the characteristics of distribution of the strata,sequence,lithofacies and paleogeography,stratigraphic correlation as well as the dating are introduced emphatically.
Keywords:Dadonggou Sandy conglomerate Metamorphic rocks The late Permian  
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