Mineralogical and geochemical characteristics of K-bentonites from the Late Ordovician to the Early Silurian in South China and their geological significance-Reference-Cited by-同舟云学术

Mineralogical and geochemical characteristics of K-bentonites from the Late Ordovician to the Early Silurian in South China and their geological significance

Published:2018-03-23 Issue:1 Volume:54 Page:514-528
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Ge Xiangying¹²^ORCID,Mou Chuanlong²³,Wang Chengshan¹,Men Xin²³,Chen Chao²⁴,Hou Qian²^ORCID

Affiliation:

1. China University of Geosciences (Beijing); Beijing China

2. Chengdu Institute of Geology and Mineral Resources; Chengdu China

3. Shandong University of Science and Technology; Qingdao China

4. China University of Geosciences (Wuhan); Wuhan China

Funder

China Geological Survey Project

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/gj.3201/fullpdf

Reference101 articles.

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3. Geochemistry of Upper Ordovician metabentonites and their cognate apatite microphenocrysts from Norway and Sweden;Batchelor;GFF,2014

4. The Lower Silurian Osmundsberg K-bentonite. Part I: Stratigraphic position, distribution, and palaeogeographic significance;Bergström;Geological Magazine,1998

5. Nomenclature, stratigraphy chemical fingerprinting, and real distribution of some middle Ordovician bentonites in Baltoscandia;Bergström;GFF,1995

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