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内蒙古哲斯敖包茅口期生物礁特征
引用本文:李尚林,王训练,徐兴永,张海军,刘旭东,李进文.内蒙古哲斯敖包茅口期生物礁特征[J].沉积学报,2004,22(3):434-442.
作者姓名:李尚林  王训练  徐兴永  张海军  刘旭东  李进文
作者单位:1.中国地质大学地球科学与资源学院 北京 100083;
基金项目:国家自然科学基金 , 中国地质调查局地质调查项目 , 中国科学院实验室基金 , 1∶5万区调联测项目
摘    要:内蒙古哲斯敖包茅口期发育典型的生物礁。礁体呈东西向展布,在空间上可明显地划分出后礁相、礁核相及前礁相。礁核相包括礁坪带、礁冠带和礁前缘带。各相带相互位置关系表明当时礁体南侧为滨岸方向,北侧为广海方向。礁体中化石极为丰富,可识别出不同的生物组合。生物组合的空间分布明显受生物礁相带控制,它们之间均为横向关系,反映了生物组合与水动力环境的统一性。

关 键 词:哲斯敖包    生物礁    茅口期
文章编号:1000-0550(2004)03-0434-09
收稿时间:2003-06-29
修稿时间:2003年6月29日

Characteristics of the Maokou'an Reef in the Zhesiaobao, Inner Mongolia
LI Shang-lin,WANG Xun-lian,XU Xing-yong,ZHANG Hai-jun,LIU Xu-dong,LI Jin-wen.Characteristics of the Maokou''''an Reef in the Zhesiaobao, Inner Mongolia[J].Acta Sedimentologica Sinica,2004,22(3):434-442.
Authors:LI Shang-lin  WANG Xun-lian  XU Xing-yong  ZHANG Hai-jun  LIU Xu-dong  LI Jin-wen
Institution:1.China University of Geosciences, Beijing 100083;2.Institute of Marine Geology, Chinese Academy of Sciences, Qingdao Shandong 266071;3.Institute of Crustal Dynamics, China Seismological Bureau, Beijing 100085;4.Institute of Mineral Resources,Chinese Academy of Geological Sciences, Beijing 100037
Abstract:Typical reefs are discovered in the Maokou'an deposits of Zhesiaobo, Inner Mongolia. They extend from east to west, and can be divided into backreef facies, reef front facies and reef core facies clearly. Reef flat, reef crest and reef front margin can be recognized in the reef core facies. The relationship among the various facies suggests that southern part of the reefs are landward, and the northern part seaward. The reefs are very rich in fossils, in which different bioassemblages can be distinguished. The spatial distribution of those assemblages seems to be controlled by facies belts of reefs, and they may exchange laterally from one to another.
Keywords:reefs  Maokou'an Stage  Zhesiaobo
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