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内蒙古达茂旗地区腮林忽洞组地层特征及时代讨论
引用本文:刘傲然,何凯,田立富.内蒙古达茂旗地区腮林忽洞组地层特征及时代讨论[J].沉积与特提斯地质,2014(1):47-54.
作者姓名:刘傲然  何凯  田立富
作者单位:石家庄经济学院,河北石家庄050031
摘    要:笔者对腮林忽洞组的岩石地层特征、层序地层、生物(叠层石)地层进行了深入研究。将腮林忽洞组划分为4个岩性段、7个三级层序;根据叠层石组合特征,建立了3个叠层石组合;结合前人获得的两件同位素年龄(207Pb/204Pb)数据,认为腮林忽洞组的时代应归属中元古代长城纪—蓟县纪。

关 键 词:腮林忽洞组  叠层石组合  层序地层  长城纪-蓟县纪  达茂旗
收稿时间:2012/10/12 0:00:00
修稿时间:2012/10/30 0:00:00

Discussions on the stratigraphy and ages of the Sailinhudong Formation in the Damaoqi region, Inner Mongolia
LIU Ao-ran,HE Kai,TIAN Li-fu.Discussions on the stratigraphy and ages of the Sailinhudong Formation in the Damaoqi region, Inner Mongolia[J].Sedimentary Geology and Tethyan Geology,2014(1):47-54.
Authors:LIU Ao-ran  HE Kai  TIAN Li-fu
Institution:( Shijiazhuang University of Economics, Sho'iazhuang 050031, Hebei, China)
Abstract:The present paper gives a detailed discussion about the lithostratigraphy,sequence stratigraphy and biostratigraphy(stromatolitic stratigraphy) of the Sailinhudong Formation in the Damaoqi region,Inner Mongolia,and separates the Sailinhudong Formation into four lithological members,seven third-order sequences and three stromatolitic assemblages.According to the existing 1:50 000 regional geological survey and mineral exploration,in reference to the previous data,especially the isotopic ages of 1456 ± 69 Ma and 1283 ± 59 Ma,the authors in this study contend that the Sailinhudong Formation should be traced back to the Changchengian to the Jixianian of the Mesoproterozoic.
Keywords:Sailinhudong Formation  stromatolitic assemblage  sequence stratigraphy  Changchengian-Jixianian  Damaoqi
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