The slab–mantle wedge interface of an incipient subduction zone: Insights from the P – T – D evolution and petrological characteristics of the Dalrymple Amphibolite, Palawan Ophiolite, Philippines

Author:

Valera Gabriel Theophilus V.1,Kawakami Tetsuo1,Payot Betchaida D.2

Affiliation:

1. Department of Geology and Mineralogy, Graduate School of Science Kyoto University Kyoto Japan

2. National Institute of Geological Sciences University of the Philippines Diliman Quezon City Philippines

Funder

Japan Society for the Promotion of Science

Ministry of Education, Culture, Sports, Science and Technology

National Research Council of the Philippines

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Reference67 articles.

1. The subduction plate interface: rock record and mechanical coupling (from long to short timescales);Agard P.;Lithos,2018

2. Slabitization: mechanism controlling subduction development and viscous coupling;Agard P.;Earth‐Science Reviews,2020

3. Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation;Agard P.;Earth and Planetary Science Letters,2016

4. A simple and generalized P‐T‐V EoS for continuous phase transitions, implemented in EosFit and applied to quartz;Angel R. J.;Contributions to Mineralogy and Petrology,2017

5. EoSFit‐Pinc: A simple GUI for host‐inclusion elastic thermobarometry;Angel R. J.;American Mineralogist,2017

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