A Textural and Mineralogical Study of the Shanzhuang Banded Iron Formation, Southeastern Margin of the North China Craton: Implications for the Overprint History of Hydrothermal Alteration and Supergenesis after Mineralization-Reference-Cited by-同舟云学术

A Textural and Mineralogical Study of the Shanzhuang Banded Iron Formation, Southeastern Margin of the North China Craton: Implications for the Overprint History of Hydrothermal Alteration and Supergenesis after Mineralization

Published:2020-02-13 Issue: Volume: Page:
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica ‐ English Edition

Author:

ZHANG Yan¹²³⁴,YU Xuefeng²³⁴,PENG Qiming¹,LI Dapeng²³⁴,LI Xiaowei¹,SHEN Kun²³⁴,ZHANG Shangkun²³⁴,SHAN Wei²³⁴

Affiliation:

1. School of Earth Science and ResourcesChina University of Geosciences Beijing 100083 China

2. Key Laboratory of Gold Mineralization Processes and Resources UtilizationMinistry of Land and Resources, Shandong Jinan 250013 China

3. Shandong Key Laboratory of Mineralization Geological Processes and Resources Utilization in Metallic Minerals Jinan 250013 China

4. Shandong Geological Sciences Institute, Shandong Jinan 250013 China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14505

Reference67 articles.

1. Trace element distribution, Co:Ni ratios and genesis of the big cadia iron-copper deposit, new south wales, australia

2. Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic, and Biospheric Processes

3. Oxygen overshoot and recovery during the early Paleoproterozoic

4. In-situ LA–ICP-MS trace elemental analyses of magnetite: The late Palaeoproterozoic Sokoman Iron Formation in the Labrador Trough, Canada

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