Multi‐Stage Hydrothermal Veins in Layered Gabbro of the Oman Ophiolite: Implications for Focused Fluid Circulation in the Lower Oceanic Crust-Reference-Cited by-同舟云学术

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Multi‐Stage Hydrothermal Veins in Layered Gabbro of the Oman Ophiolite: Implications for Focused Fluid Circulation in the Lower Oceanic Crust

Published:2021-08 Issue:8 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Zhang Chao¹²^ORCID,Koepke Jürgen²^ORCID,Wolff Paul Eric²,Horn Ingo²,Garbe‐Schönberg Dieter³^ORCID,Berndt Jasper⁴

Affiliation:

1. Department of Geology State Key Laboratory of Continental Dynamics Northwest University Xi'an China

2. Institut für Mineralogie Leibniz Universität Hannover Hannover Germany

3. Institut für Geowissenschaften Christian‐Albrechts‐Universität zu Kiel Kiel Germany

4. Institut für Mineralogie Westfälische Wilhelms‐Universität Münster Münster Germany

Funder

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022349

Reference158 articles.

1. Crustal diopsidites from the northern Oman ophiolite: Evidence for hydrothermal circulation through suboceanic Moho

2. Three-dimensional Evolution of Melting, Heat and Melt Transfer in Ascending Mantle beneath a Fast-spreading Ridge Segment Constrained by Trace Elements in Clinopyroxene from Concordant Dunites and Host Harzburgites of the Oman Ophiolite

3. The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex

4. Seafloor hydrothermal systems: Physical, chemical, biological, and geological interactions;Alt J. C.,1995

5. Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256

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1. Dynamics of the oceanic dike–gabbro transition revealed by petrology and geochemistry of the Yunzhug ophiolite, central Tibet;Contributions to Mineralogy and Petrology;2024-05

2. Multistage and diverse melt-mantle interaction in dunite-harzburgite channel systems beneath oceanic slow-ultraslow spreading centers: Evidence from the Xigaze ophiolite (Tibet);Lithos;2024-03

3. Origin of Fe‐Ca‐Metasomatism in Exhumed Mantle Rocks at the MARK Area (23°N, ODP Leg 153) and Implications on the Formation of Ultramafic‐Hosted Seafloor Massive Sulfide Deposits;Geochemistry, Geophysics, Geosystems;2023-09

4. Paleo‐Permeability Structure of the Crustal Section of the Samail Ophiolite Based on Automated Detection of Veins in X‐Ray CT Core Images From the Oman Drilling Project;Geochemistry, Geophysics, Geosystems;2023-06

5. Seafloor hydrothermal circulation at a rifted margin of the South China Sea: Insights from basement epidote veins in IODP Hole U1502B;Lithos;2023-05

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