Tracing fault‐related fluids using in situ trace elements: A case study in Upper Cambrian dolostone in Gucheng area, Tarim Basin, NW China-Reference-Cited by-同舟云学术

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Tracing fault‐related fluids using in situ trace elements: A case study in Upper Cambrian dolostone in Gucheng area, Tarim Basin, NW China

Published:2021-02-16 Issue:6 Volume:56 Page:3301-3313
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Lu Ziye¹,Li Yingtao²,Zhang Shaonan¹,Ye Ning¹^ORCID,Zhu Bei¹,Lu Chaojin³^ORCID,Ding Xiaoqi⁴,Huang Baiwen¹

Affiliation:

1. School of Geoscience and Technology Southwest Petroleum University Chengdu China

2. Sinopec Petroleum Exploration and Production Research Institute Beijing China

3. Department of Marine Geosciences Rosenstiel School of Marine and Atmospheric Science, University of Miami Miami Florida USA

4. College of Energy Chengdu University of Technology Chengdu China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4105

Reference73 articles.

1. Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

2. Rare earth elements in mussel shells of the Mytilidae family as tracers for hidden and fossil high-temperature hydrothermal systems

3. Comparative study of yttrium and rare-earth element behaviours in fluorine-rich hydrothermal fluids

4. Comparison of the partitioning behaviours of yttrium, rare earth elements, and titanium between hydrogenetic marine ferromanganese crusts and seawater

5. Rare earth element fractionation in metamorphogenic hydrothermal calcite, magnesite and siderite

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Evolution of diagenetic fluids in the deeply buried, upper Ediacaran Dengying Formation, Central Sichuan Basin, China;Australian Journal of Earth Sciences;2022-10-26

2. Non-hydrothermal saddle dolomite in Upper Cambrian dolostones of Tarim Basin: evidence from C–O–Sr isotopic and in-situ trace elemental studies;Carbonates and Evaporites;2022-07-20

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