Geochemical Characterization of the Oman Crust‐Mantle Transition Zone, OmanDP Holes CM1A and CM2B-Reference-Cited by-同舟云学术

Geochemical Characterization of the Oman Crust‐Mantle Transition Zone, OmanDP Holes CM1A and CM2B

Published:2022-04 Issue:4 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Kourim F.¹^ORCID,Rospabé M.²^ORCID,Dygert N.³^ORCID,Chatterjee S.⁴^ORCID,Takazawa E.⁴,Wang K.‐L.¹⁵^ORCID,Godard M.⁶^ORCID,Benoit M.⁷,Giampouras M.⁸,Ishii K.⁴,Teagle D. A.‐H.⁹^ORCID,Cooper M.‐J.⁹^ORCID,Kelemen P.¹⁰^ORCID

Affiliation:

1. Institute of Earth Sciences Academia Sinica Taipei Taiwan

2. Research Institute for Marine Geodynamics (IMG) Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Yokosuka Japan

3. Department of Earth & Planetary Sciences University of Tennessee Knoxville TN USA

4. Department of Geology Faculty of Science Niigata University Niigata Japan

5. Department of Earth Sciences National Taiwan University Taipei Taiwan

6. Géosciences Montpellier CNRS Université Montpellier Montpellier France

7. Géosciences Environnement Toulouse (GET) Observatoire Midi‐Pyrénées Université de Toulouse CNRS IRD Toulouse France

8. Instituto Andaluz de Ciencias de la Tierra (IACT) Consejo Superior de Investigaciones Científicas Universidad de Granada Granada Spain

9. School of Ocean & Earth Science National Oceanography Centre Southampton University of Southampton Southampton UK

10. Lamont–Doherty Earth Observatory Columbia University Palisades NY USA

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/10.1029/2021JB022694

Reference132 articles.

1. The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both?

2. Synmagmatic normal faulting in the lower oceanic crust: Evidence from the Oman ophiolite

3. Ocean crust accretion along a high-temperature detachment fault in the Oman ophiolite: A structural and petrological study of the Bahla massif

4. Quantifying trace element disequilibria in mantle xenoliths and abyssal peridotites

5. Tectonic setting for the genesis of oceanic plagiogranites: evidence from a paleo-spreading structure in the Oman ophiolite

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1. Mineral and whole-rock geochemistry of high-Al podiform chromitites in the Fizh Massif of the Cretaceous Oman ophiolite: origin of hydrous N-MORB melts in a nascent forearc setting;Journal of the Geological Society;2023-10-25

2. Petrology and Geochemistry of the Neoproterozoic Tays Serpentinite, Arabian Shield: Insights into the Composition and Nature of Forearc Mantle;The Journal of Geology;2023-07-01

3. Geological records of transient fluid drainage into the shallow mantle wedge;Science Advances;2023-04-07

4. Preface: Special Issue on Ophiolites and Oceanic Lithosphere;Journal of Geophysical Research: Solid Earth;2023-04