Glimpses of oceanic lithosphere of the Challenger Deep forearc segment in the southernmost Marianas: The 143°E transect, 5800

Glimpses of oceanic lithosphere of the Challenger Deep forearc segment in the southernmost Marianas: The 143°E transect, 5800–4200 m

Published:2020-01 Issue:1 Volume:29 Page:
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Stern Robert J.¹^ORCID,Ohara Yas²³⁴,Ren Minghua⁵,Leybourne Matt⁶⁷,Bowers Brent¹

Affiliation:

1. Department of Geosciences University of Texas at Dallas Richardson Texas

2. Hydrographic and Oceanographic Department of Japan Tokyo Japan

3. Japan Agency for Marine‐Earth Science and Technology Yokosuka Japan

4. Department of Earth and Planetary Sciences Nagoya University Nagoya Japan

5. Department of Geoscience University of Nevada Las Vegas Nevada

6. Queen's Facility for Isotope Research (QFIR), Department of Geological Sciences and Geological Engineering Queen's University Kingston Ontario Canada

7. McDonald Institute, Canadian Particle Astrophysics Research Centre, Department of Physics Engineering Physics and Astronomy, Queen's University Kingston Ontario Canada

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12359

Reference37 articles.

1. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation

2. How to Create New Subduction Zones: A Global Perspective

3. Malaguana-Gadao Ridge: Identification and implications of a magma chamber reflector in the southern Mariana Trough

4. An updated digital model of plate boundaries

5. Distribution and origin of igneous rocks from the landward slopes of the Mariana Trench: Implications for its structure and evolution

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1. Tectonic and magmatic evolution of the southernmost Mariana convergent margin: Constraints from geochronology and geochemistry of the Challenger Deep sediments;Lithos;2024-12

2. Subduction initiation as recorded in the Izu-Bonin-Mariana forearc;Earth-Science Reviews;2023-11

3. Deep crustal structure across the Challenger Deep: Tectonic deformation and strongly serpentinized layer;Gondwana Research;2023-06

4. Peridotites with back-arc basin affinity exposed at the southwestern tip of the Mariana forearc;Progress in Earth and Planetary Science;2022-03-29

5. Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle;Communications Earth & Environment;2021-12