柴达木盆地北缘结绿素一红山地区古新统至中新统沉积相<sup>&#x0002A;</sup>

古地理学报 ›› 2006, Vol. 8 ›› Issue (3): 377-388.

• 岩相古地理学及沉积学 • 上一篇下一篇

柴达木盆地北缘结绿素一红山地区古新统至中新统沉积相^*

金振奎¹, 齐聪伟¹, 薛建勤², 王春生¹

1 中国石油大学(北京)资源与信息学院,北京 102249;
2 中国石油青海油田公司,甘肃敦煌 736202

收稿日期:2005-10-04 修回日期:2005-12-02 出版日期:2006-06-01 发布日期:2006-06-01
作者简介:金振奎,男,1963年3月生,1983年毕业于华东石油学院,现为中国石油大学(北京)教授,主要从事沉积学研究工作。
基金资助:
*国家973项目(编号2002CB211702-2)资助

Sedimentary facies of the Paleocene Miocene in Jieli su Hongshan area in north margin of Qaidam Basin

Jin Zhenkui¹, Qi Congwei¹, Xue Jiangin², Wang Chunsheng¹

1 China University of Petroleum (Beijing),Beijing 102249;
2 PetroChina Qinghai Oilfield Company, Dunhuang 736202, Gansu

Received:2005-10-04 Revised:2005-12-02 Online:2006-06-01 Published:2006-06-01
About author:Jin Zhenkui, born in 1963, graduated from East China Petroleum Institute in 1983. Now he is a professor of China University of Petroleum Beijing and is mainly engaged in sedimentology.

摘要/Abstract

摘要： 根据柴达木盆地北缘露头剖面、钻井剖面的地层学和岩石学研究所取得的各种定量及定性资料,采用冯增昭教授倡导的单因素分析多因素综合作图法,编制了柴达木盆地北缘结绿素—红山地区古新统—始新统、渐新统和中新统的各种单因素图和沉积相图。这是首次将定量的沉积相研究方法应用于柴达木盆地的古新统至中新统。结绿素—红山地区古新统至中新统发育2种沉积相类型,即冲积扇和辫状河。其中辫状河可划分为砾质辫状河和砂质辫状河。古新世—始新世发育冲积扇—辫状河—湖泊沉积体系,渐新世—中新世发育辫状河—湖泊沉积体系。从古新世到中新世,柴达木盆地北缘经历了由大规模冲积扇沉积到辫状河沉积的演化过程。

关键词: 柴达木盆地, 古新统至中新统, 沉积相, 单因素分析多因素综合作图法, 定量

Abstract: On the basis of all kinds of stratigraphic and petrologic data of outcrop and well sections, the maps of single factors and sedimentary facies of the Paleocene Eocene, Oligocene and Miocene were compiled with the single factor analysis and multifactor comprehensive mapping method proposed by Professor Feng Zengzhao. It is the first time to apply this method to study sedimentary facies of the Paleocene Miocene in the Qaidam Basin. There are two types of sedimentary facies in this region: the alluivial fan and the braided fluvial river. The latter is further sub-divided into gravelly and sandy braided fluvial facies. The sedimentary systems were alluvial fan braided fluvial river-lacustrine depositional systems during the Paleocene-Eocene, and braided fluvial river-lacustrine depositional systems during the Oligocene-Miocene. From Paleocene to Miocene, the sedimentary facies evolved from the extensive alluvial fan to the braided fluvial river environment.

Key words: Qaidam Basin, Paleocene-Miocene, sedimentary facies, single factor analysis and multifactor comprehensive mapping method, quantitative

中图分类号:

P5122

金振奎, 齐聪伟, 薛建勤, 王春生. 柴达木盆地北缘结绿素一红山地区古新统至中新统沉积相^*[J]. 古地理学报, 2006, 8(3): 377-388.

Jin Zhenkui, Qi Congwei, Xue Jiangin, Wang Chunsheng. Sedimentary facies of the Paleocene Miocene in Jieli su Hongshan area in north margin of Qaidam Basin[J]. JOPC, 2006, 8(3): 377-388.

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