Formation of Igneous Layering in the Lower Oceanic Crust From the Samail Ophiolite, Sultanate of Oman-Reference-Cited by-同舟云学术

Formation of Igneous Layering in the Lower Oceanic Crust From the Samail Ophiolite, Sultanate of Oman

Published:2021-01 Issue:1 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:

Mock D.¹²^ORCID,Neave D. A.¹³^ORCID,Müller S.⁴^ORCID,Garbe‐Schönberg D.⁴,Namur O.⁵^ORCID,Ildefonse B.²^ORCID,Koepke J.¹

Affiliation:

1. Institut für Mineralogie, Leibniz Universität Hannover Hanover Germany

2. Géosciences Montpellier Université de Montpellier, CNRS, Université des Antilles Montpellier France

3. Department of Earth and Environmental Sciences The University of Manchester Manchester UK

4. Institut für Geowissenschaften, Christian‐Albrechts‐Universität zu Kiel Kiel Germany

5. Department of Earth and Environmental Sciences KU Leuven Leuven KU Belgium

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/10.1029/2020JB019573

Reference132 articles.

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

2. Deep and High-temperature Hydrothermal Circulation in the Oman Ophiolite--Petrological and Isotopic Evidence

3. Magma chambers in the Oman ophiolite: fed from the top and the bottom

4. Crystal aging and the formation of fine-scale igneous layering

5. The layered ultrabasic rocks of Rhum, Inner Hebrides;Brown G. M.;Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences,1956

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