A Reference Section Through Fast‐Spread Lower Oceanic Crust, Wadi Gideah, Samail Ophiolite (Sultanate of Oman): Trace Element Systematics and REE Crystallization Temperatures—Implications for Hybrid Crustal Accretion-Reference-Cited by-同舟云学术

A Reference Section Through Fast‐Spread Lower Oceanic Crust, Wadi Gideah, Samail Ophiolite (Sultanate of Oman): Trace Element Systematics and REE Crystallization Temperatures—Implications for Hybrid Crustal Accretion

Published:2022-03 Issue:3 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Müller Samuel¹^ORCID,Garbe‐Schönberg Dieter¹^ORCID,Koepke Jürgen²^ORCID,Hoernle Kaj¹³

Affiliation:

1. Institute of Geosciences Kiel University Kiel Germany

2. Institute of Mineralogy Hannover University Hannover Germany

3. GEOMAR Helmholtz Centre for Ocean Research Kiel Kiel 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/10.1029/2021JB022699

Reference158 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. Crustal thickness and Moho character of the fast-spreading East Pacific Rise from 9°42′N to 9°57′N from poststack-migrated 3-D MCS data

4. An examination of along-axis variation of magma chamber width and crustal structure on the East Pacific Rise between 13°30′N and 12°20′N

5. Trace element partitioning in plagioclase feldspar

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