Rheology of Mg2 GeO4 olivine and spinel harzburgite: Implications for Earth's mantle transition zone-Reference-Cited by-同舟云学术

Rheology of Mg2 GeO4 olivine and spinel harzburgite: Implications for Earth's mantle transition zone

Published:2015-04-10 Issue:7 Volume:42 Page:2212-2218
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Shi F.¹²,Zhang J.¹,Xia G.²,Jin Z.¹,Green H. W.¹²^ORCID

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources; China University of Geosciences; Wuhan China

2. Department of Earth Sciences; University of California; Riverside California USA

Funder

U.S. National Science Foundation

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015GL063316/fullpdf

Reference43 articles.

1. Limitation on the mass exchange between the upper and lower mantle: The evolving convection regime of the Earth;Allègre;Earth Planet. Sci. Lett.,1997

2. Plastic flow of Mn2GeO4 I: Toward a rheological model of the Earth's transition zone

3. Density and composition of mantle and core;Birch;J. Geophys. Res.,1964

4. Possible flush instability in mantle convection at Archean-Proterozoic transition;Breuer;Nature,1995

5. Burnley , P. C. 1990 The effect of nonhydrostatic stress on the olivine-spinel transformation in Mg 2 GeO 4 Dep. of Earth Sciences, Univ. of California Riverside

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