Multiple-scale hydrothermal circulation in 135 Ma oceanic crust of the Japan Trench outer rise: Numerical models constrained with heat flow observations-Reference-Cited by-同舟云学术

Multiple-scale hydrothermal circulation in 135 Ma oceanic crust of the Japan Trench outer rise: Numerical models constrained with heat flow observations

Published:2015-08 Issue:8 Volume:16 Page:2711-2724
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Ray Labani¹²,Kawada Yoshifumi²³,Hamamoto Hideki²⁴,Yamano Makoto²

Affiliation:

1. CSIR-National Geophysical Research Institute; Hyderabad India

2. Earthquake Research Institute, University of Tokyo; Tokyo Japan

3. Japan Agency for Marine-Earth Science and Technology; Yokosuka Japan

4. Center for Environmental Science in Saitama; Kazo Japan

Funder

KAKENHI

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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4. Fundamentals of ridge crest topography;Davis;Earth Planet. Sci. Lett.,1974

5. Observations concerning the vigor of hydrothermal circulation in young oceanic crust;Davis;J. Geophys. Res.,1996a

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1. Pressure-driven processes explain the decreasing magnetization of the subducting oceanic crust in the Japan Trench;Communications Earth & Environment;2023-07-04

2. The Thermal Effects of Plate‐Bending‐Related Thickening of the Oceanic Crustal Aquifer in the Nankai Trough and Japan Trench Subduction Zones;Journal of Geophysical Research: Solid Earth;2019-02

3. Validation of the BASALT model for simulating off‐axis hydrothermal circulation in oceanic crust;Journal of Geophysical Research: Solid Earth;2017-08

4. Heat Flow Anomalies near Trenches: Heat Transport by Fluid Circulation in Oceanic Crust;Journal of Geography (Chigaku Zasshi);2017