Heat Flow Anomalies near Trenches: Heat Transport by Fluid Circulation in Oceanic Crust-Reference-Cited by-同舟云学术

Heat Flow Anomalies near Trenches: Heat Transport by Fluid Circulation in Oceanic Crust

Published:2017 Issue:2 Volume:126 Page:147-161
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:Journal of Geography(Chigaku Zasshi)

Author:

YAMANO Makoto¹,KAWADA Yoshifumi²

Affiliation:

1. Earthquake Research Institute, The University of Tokyo

2. International Research Institute of Disaster Science, Tohoku University

Publisher

Tokyo Geographical Society

Subject

Materials Chemistry

Link

https://www.jstage.jst.go.jp/article/jgeography/126/2/126_126.147/_pdf

Reference48 articles.

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2. Ashi, J., Tokuyama, H., Ujiie, Y. and Taira, A. (1999): Heat flow estimation from gas hydrate BSRs in the Nankai Trough: Implications for thermal structures of the Shikoku Basin. Eos Transactions AGU, 80, Fall Meeting Supplement, Abstract F929-F930.

3. Cozzens, B.D. and Spinelli, G.A. (2012): A wider seismogenic zone at Cascadia due to fluid circulation in subducting oceanic crust. Geology, 40, 899-902.

4. Davis, E.E. (1989): Thermal aging of oceanic lithosphere. in Handbook of Seafloor Heat Flow edited by Wright, J.A. and Louden, K.E., CRC Press, 145-167.

5. Fisher, A.T. and Von Herzen, R.P. (2005): Models of hydrothermal circulation within 106 Ma seafloor: Constraints on the vigor of fluid circulation and crustal properties, below the Madeira Abyssal Plain. Geochemistry, Geophysics, Geosystems, 6(11), Q11001, doi:10.1029/2005gc001013.

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