引用本文:胡建中, 潘永胜.内蒙古固阳渣尔泰山群层序地层与复合海平面变化[J].沉积与特提斯地质,2001,(2):91-100.[点击复制]
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内蒙古固阳渣尔泰山群层序地层与复合海平面变化
胡建中,潘永胜
0
(1. 中国地质大学 地球科学与资源学院, 北京 10083;
2. 山西省 214 地质队, 山西 运城 044100)
摘要:
通过内蒙古固阳渣尔泰山群的岩性、岩相和相序研究,对其进行了层序分析和层序划分,识别出一级、二级、三级层序界面,包括海侵沟蚀面和暴露-淹没复合型层序界面。共划分出1个超层序,3个大层序和8个层序。总结出渣尔泰山群的不同古地理背景如碎屑滨岸、台缘碳酸盐岩与碎屑岩混积、碳酸盐台地、台前斜坡和陆棚盆地层序发育模式以及内部构成特征,并探讨了复合海平面变化以及对层序发育和演化的控制作用。
关键词:  层序界面  海侵沟蚀面  暴露-淹没复合型界面  复合海平面变化  渣尔泰山群
DOI:
附件
投稿时间:2001-02-19
基金项目:
Sequence stratigraphy and composite sea-level changes in the Zha'ertaishan Group, Guyang, Inner Mongol
HU Jian-zhong, PAN Yong-sheng
(1. Faculty of Earth Science and Resources, China University of Geosciences, Beijing 100083, China;
2. No. 214 Geological Party, Y uncheng 044100, Shanxi, China)
Abstract:
Stratigraphic sequences and sequence boundaries are divided for the Zha'ertaishan Group, Guyang, Inner Mongol on the basis of lithological, sedimentary facies and facies sequence approaches.The sequence boundaries consist of the first-, second- and third-o rder sequence boundaries, including transgressive ravinement surfaces and composite exposure-drow ning bounding surfaces. With different scales of sequence boundaries as bounding surfaces, the following sequences have been recognized for the Group:one supersequence, three megasequences and eight sequences.The models for the sequence development and architecture are presented for the different paleogeographic settings of the Zha'ertaishan Group, i. e. siliciclastic shoreline, mixed platform-margin carbonate rocks and siliciclastic rocks, carbonate platform, foreslope and shelf-basin sequences. In addition, the composite sea-level changes and their controls on the sequence development and evolution are also treated in this paper.
Key words:  sequence boundary  transgressive ravinement surface  composite exposuredrow ning bounding surface  composite sea-level change  Zha'ertaishan Group

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