Terminal paleoproterozoic ooidal ironstone from north China: A sedimentary response to the initial breakup of columbia supercontinent

被引：19
|
作者：
Tang, Dongjie [1 ,2 ]
Shi, Xiaoying [1 ,3 ]
Liu, Dianbo [3 ]
Lin, Yitian [3 ]
Zhang, Chuanheng [3 ]
Song, Gaoyuan [3 ]
Wu, Jinjian [3 ]
机构：
[1] State Key Laboratory of Biological and Environmental Geology, China University of Geosciences, Beijing,100083, China
[2] Institute of Earth Sciences, China University of Geosciences, Beijing,100083, China
[3] School of Earth Sciences and Resources, China University of Geosciences, Beijing,100083, China
来源：
Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences | 2015年 / 40卷 / 02期
关键词：
Compilation and indexing terms; Copyright 2025 Elsevier Inc;
D O I：
10.3799/dqkx.2015.022
中图分类号：
学科分类号：
摘要：
Aluminum oxide - Sedimentology - Kaolinite - Tectonics - Iron - Energy dispersive spectroscopy - Alumina - Deposition - X ray diffraction
引用
收藏
页码：290 / 304
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