Fluid tracing and evolution at micron-scale of shales in faulted lake basin: Evidence and constraints from in-situ analysis of analcime-Reference-Cited by-同舟云学术

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Fluid tracing and evolution at micron-scale of shales in faulted lake basin: Evidence and constraints from in-situ analysis of analcime

Published:2024-05 Issue: Volume:163 Page:106776
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Wang Junran,Liang Chao,Cao Yingchang,Song Shunyao,Liu Keyu,Yang Shengyu,Tian Jinqiang,Khan Danish,Xin Bixiao

Publisher

Elsevier BV

Reference78 articles.

1. Strontium isotopes and rare-earth element geochemistry of hydrothermal carbonate deposits from Lake Tanganyika, East Africa;Barrat;Geochimica et Cosmochimica Acta,2000

2. The distribution and stabilisation of dissolved Fe in deep-sea hydrothermal plumes: earth Planet;Bennett;Sci. Lett., v.,2008

3. Evolution of a hydrocarbon migration pathway along basin-bounding faults: evidence from fault cement[J];Boles;AAPG Bull.,2004

4. Geothermometry and water–rock interaction modelling at Hafralækur: possible implications of temperature and CO2 on hydrogeochemical changes previously linked to earthquakes in northern Iceland;Boschetti;Geothermics,2022

5. Zeolite beds in the green river formation;Bradley;Science,1928

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