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茅山山脉东麓的砾岩层位和时代
引用本文:徐学思 胡连英. 茅山山脉东麓的砾岩层位和时代[J]. 江苏地质, 1998, 22(1): 19-22
作者姓名:徐学思 胡连英
作者单位:江苏省地质调查研究院(徐学思),江苏省地震局(胡连英)
摘    要:通过对茅山东麓砾岩层的实地研究,以5条剖面的岩性、产状和生物等特征为依据,将砾岩分为三类,并分别论述其层位时代。提出了与前人不同的观点。

关 键 词:砾岩  地层岩性  新生代  浦口组  江苏茅山

Horizon and Time of Conglomerate in Eastern Maoshan, Jiangsu Province
Xu XuesiGeological Survey of Jiangsu Province,Nanjing,Hu LianyingSeismological Bureau of Jiangsu Province,Nanjing. Horizon and Time of Conglomerate in Eastern Maoshan, Jiangsu Province[J]. Jiangsu Geology, 1998, 22(1): 19-22
Authors:Xu XuesiGeological Survey of Jiangsu Province  Nanjing  Hu LianyingSeismological Bureau of Jiangsu Province  Nanjing
Affiliation:Xu XuesiGeological Survey of Jiangsu Province,Nanjing,210018 Hu LianyingSeismological Bureau of Jiangsu Province,Nanjing,210014
Abstract:The field investigation on conglomerate in eastern Maoshan Mountain shows that the conglomerate can be divided into three types:1.cobblestone located at the top and bottom or interbed of purple sand stone of Paleocene Funing Formation; 2.microconglomerate, interlayered by clay layer, with white and brownish red nodules of Micoene Dongxuanguan Formation; 3.Lower Pleistocenebasaltic cobblestone. Lithologic and fossil features as well as occurrences of five local sections lead to a consideration different from that formerly prevalent for Pukou Formation in Maoshan Mountain. Therefore, the new pointview has important significance for the study of neotectonism in the area.
Keywords:Conglomerate Stratigraphic lithology Cenozoic era Pukou Formation Maoshan Mountain  Jiangsu
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