The Ductile‐to‐Brittle Transition Recorded in the Balmuccia Peridotite Body, Italy: Ambient Temperature for the Onset of Seismic Rupture in Mantle Rocks-Reference-Cited by-同舟云学术

The Ductile‐to‐Brittle Transition Recorded in the Balmuccia Peridotite Body, Italy: Ambient Temperature for the Onset of Seismic Rupture in Mantle Rocks

Published:2020-02 Issue:2 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Ueda Tadamasa¹²^ORCID,Obata Masaaki¹,Ozawa Kazuhito²,Shimizu Ichiko¹²^ORCID

Affiliation:

1. Division of Earth and Planetary Sciences, Graduate School of ScienceKyoto University Kyoto Japan

2. Department of Earth and Planetary Science, School of ScienceThe University of Tokyo Tokyo Japan

Funder

Ministry of Education, Culture, Sports, Science and Technology

Japan Society for the Promotion of Science

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/10.1029/2019JB017385

Reference77 articles.

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4. Pyroxene-carbonate reactions in the upper mantle

5. Geothermobarometry in Four-phase Lherzolites II. New Thermobarometers, and Practical Assessment of Existing Thermobarometers

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