High-temperature fracturing and subsequent grain-size-sensitive creep in lower crustal gabbros: Evidence for coseismic loading followed by creep during decaying stress in the lower crust?-Reference-Cited by-同舟云学术

High-temperature fracturing and subsequent grain-size-sensitive creep in lower crustal gabbros: Evidence for coseismic loading followed by creep during decaying stress in the lower crust?

Published:2015-05 Issue:5 Volume:120 Page:3119-3141
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Okudaira Takamoto¹,Jeřábek Petr²,Stünitz Holger³,Fusseis Florian⁴

Affiliation:

1. Department of Geosciences; Osaka City University; Osaka Japan

2. Institute of Petrology and Structural Geology; Charles University; Prague Czech Republic

3. Department of Geology; University of Tromsø; Tromsø Norway

4. School of Geosciences; University of Edinburgh; Edinburgh UK

Funder

Research Council of Norway FRINAT program

University of Tromsø to H. S.

OCU Overseas Research Fellowship

MEXT KAKENHI

Czech Science Foundation research

U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JB011708/fullpdf

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4. The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages;Bhadra;Am. Mineral.,2007

5. Brittle-plastic deformation in initially dry rocks at fluid-present conditions: Transient behaviour of feldspar at midcrustal levels;Brander;Contrib. Mineral. Petrol.,2012

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