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地球科学进展  2011, Vol. 26 Issue (9): 1006-1014    DOI: 10.11867/j.issn.1001-8166.2011.09.1006
新学科·新技术·新发现     
宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型
李向东1,2,何幼斌2,张铭记3,刘训1,姚建新1
1.中国地质科学院地质研究所,北京 100037;2.长江大学地球科学学院,湖北 荆州 434023;3. 中国石油东方地球物理公司东部勘探事业部,陕西 西安 710021
Sedimentary Types of Internal-wave and Internal-tide Deposits of Middle Ordovician, Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous Region, China
Li Xiangdong1,2, He Youbin2, Zhang Mingji3, Liu Xun1, Yao Jianxin1
1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. School of Geoscience, Yangtze University, Jingzhou 434023, China;3. Changqing Division of East Exploration Department, BPG CNPC, Xi′an 710021, China
 全文: PDF(646 KB)  
摘要:

内波、内潮汐沉积是深水沉积研究中一个非常年轻的研究领域,自发现到现在仅仅20年时间,对其沉积类型的研究目前尚未涉及。以宁夏香山群徐家圈组中的内波、内潮汐沉积为对象,详细描述了深水环境中形成的双向交错层理、单向交错层理、复合流层理及具有波状纹层、束状纹层和交错纹层透镜体的交错层理,并探讨了其成因机制,识别出了短周期内波沉积。在此基础之上,结合已有的内波、内潮汐沉积鉴别标志,从沉积构造的角度对内波、内潮汐沉积类型进行了探讨。将内波、内潮汐沉积分为短周期内波沉积、内潮汐沉积和叠加内波沉积。鉴于内潮汐形成机制的独特性和海洋物理学中内波的研究现状,三者仍统称为内波、内潮汐沉积。

关键词: 短周期内波沉积内潮汐沉积沉积构造香山群    
Abstract:

The study of internal-wave and internal-tide deposits is a very young research field with twenty years of history in the deep-water deposition, and there is no study on its sedimentary types. Here, we forcus on the internal-wave and internal-tide deposits developed in Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous Region and describe related sedimentary structures in detail. We interpret combined-flow-ripple lamination and the cross beddings with undulatory laminations, offshooting laminations and cross-laminated lenses as combined-flow and oscillatory flow generated by short-period internal waves respectively. According to these new interpretations and the interpretations of deep-water bidirectional cross-beddings and unidirectional crossbeddings in literatures, we attribute internal-wave and internal-tide deposits to short-period internal-wave deposits, internal-tide deposits and interaction internal-wave deposits. Here, we use internal-wave and internal-tide deposits instead of internal-wave deposits because of the special origin and research status of internal tides.

Key words: Short-period internal-wave deposits    Sedimentary structures    Xiangshan Group    Internal-tide deposits
收稿日期: 2010-08-24 出版日期: 2011-10-10
:  P512.32  
基金资助:

国家自然科学基金项目“宁夏香山群内波、内潮汐沉积及其伴生沉积研究”(编号:40672071)和“鄂尔多斯盆地西缘中奥陶统深水牵引流沉积研究”(编号:41072086);中国地质科学院地质研究所基本科研项目“宁夏香山群复杂水动力条件下浊流沉积特征研究”(编号:J1110)资助.

通讯作者: 李向东   
作者简介: 李向东(1973-),男,陕西蓝田人,博士后,主要从事深水沉积及其应用研究. E-mail:lixiangdong614@163.com
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引用本文:

李向东,何幼斌,张铭记,刘训,姚建新. 宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型[J]. 地球科学进展, 2011, 26(9): 1006-1014.

Li Xiangdong, He Youbin, Zhang Mingji, Liu Xun, Yao Jianxin. Sedimentary Types of Internal-wave and Internal-tide Deposits of Middle Ordovician, Xujiajuan Formation, Xiangshan Group, Ningxia Autonomous Region, China. Advances in Earth Science, 2011, 26(9): 1006-1014.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2011.09.1006        http://www.adearth.ac.cn/CN/Y2011/V26/I9/1006

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