Significance of Trace Elements in Marine Shale Pyrite for Reconstructing the Sedimentary Environment: A Case Study of Niutitang and Hongshuizhuang Formations-Reference-Cited by-同舟云学术

Significance of Trace Elements in Marine Shale Pyrite for Reconstructing the Sedimentary Environment: A Case Study of Niutitang and Hongshuizhuang Formations

Published:2021-11-01 Issue:11 Volume:5 Page:3210-3225
ISSN:2472-3452
Container-title:ACS Earth and Space Chemistry
language:en
Short-container-title:ACS Earth Space Chem.

Author:

Wang Xiwei¹^ORCID,Shi Miao²,Zhang Jinchuan¹^ORCID,Pang Yu³,Zhao Yichao⁴

Affiliation:

1. School of Energy Resources, China University of Geosciences, Beijing 100083, China

2. School of Gemology and Materials Science, Hebei GEO University, Shijiazhuang 050031, China

3. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China

4. Exploration and Development Research Institute, PetroChina Southwest Oil & Gasfield Company, Chengdu 610041, China

Funder

Natural Science Foundation of Hebei Province

National Natural Science Foundation of China

Science and Technology Project of Hebei Education Department

Publisher

American Chemical Society (ACS)

Subject

Space and Planetary Science,Atmospheric Science,Geochemistry and Petrology

Link

https://pubs.acs.org/doi/pdf/10.1021/acsearthspacechem.1c00280

Reference75 articles.

1. Pyrite framboids and their development: a new conceptual mechanism

2. Palaeoceanographic redox environments for the lower Cambrian Hetang Formation in South China: Evidence from pyrite framboids, redox sensitive trace elements, and sponge biota occurrence

3. Pyrite framboid size distribution as a record for relative variations in sedimentation rate: An example on the Toarcian Oceanic Anoxic Event in Southiberian Palaeomargin

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