Sedimentary Characteristics of the Fourth Member of Cretaceous Nenjiang Formation in the Southern Songliao Basin, Northeast of China

被引:0
|
作者
Wang, Jinkai [1 ,2 ]
Zhang, Jinliang [1 ,3 ]
Xie, Jun [1 ,2 ]
机构
[1] Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China
[3] Beijing Normal Univ, Fac Geog Sci, Beijing 100875, Peoples R China
关键词
Songliao basin; Sedimentary; River delta; Rock facies;
D O I
10.1007/978-3-030-01452-0_38
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The lithology of the fourth member of the Cretaceous Nenjiang formation (K(2)n(4)) in southern Songliao Basin is mainly mudstone. The proportion of sandstone is about 10% which is mainly composed of lithic feldspar sandstone. The carbonate content of sandstone is very high with an average of 25%. The clay minerals are mainly illite/montmorillonite (I/M) mixed layer. In the studied area, 9 single lithofacies types and 5 combination lithofacies types were identified and described in detail. The subfacies type of K(2)n(4) in the studied area is delta front which includes four microfacies: underwater distributary channel, mouth bar, sand sheet and interdistributary. During this period, the lake basin gradually shrank, the delta continued to push south, and the sand bodies were lingual to the south with their thickness gradually decreasing.
引用
收藏
页码:159 / 162
页数:4
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