Structure, Rheology and Permeability of Partially Molten Rocks at Low Melt Fractions-Reference-Cited by-同舟云学术

Structure, Rheology and Permeability of Partially Molten Rocks at Low Melt Fractions

Published:2013-03-18 Issue: Volume: Page:103-121
ISSN:2328-8779
Container-title:Mantle Flow and Melt Generation at Mid-Ocean Ridges
language:
Short-container-title:

Author:

Kohlstedt David L.

Publisher

American Geophysical Union

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/GM071p0103/fullpdf

Reference86 articles.

1. Magma migration beneath an ocean ridge;Ahem;Earth Planet. Set. Lett.,1979

2. Critical phenomena in the meology of partially melted rocks;Arzi;Tectonophys.,1978

3. High-temperature creep of olivine single crystals: 1. Mechanical results for buffered samples;Bai;J. Geophys. Res.,1991

4. A unifying theory of the stability of penetrating liquid phases and sintering pores;Beere;Acta Metall.,1975

5. Experimental investigation of the theology and structure of partially molten lherzolite deformed under upper mantle pressures and temperatures;Botch;EOS, Trans. Am. Geophys. Union,1990

Cited by 43 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Surface Effects;Thermodynamics in Earth and Planetary Sciences;2020

2. Experimental evidence supports mantle partial melting in the asthenosphere;Science Advances;2016-05-06

3. Electrical conductivity of lawsonite and dehydrating fluids at high pressures and temperatures;Geophysical Research Letters;2015-09-18

4. Semibrittle deformation and partial melting of perthitic K‐feldspar: An experimental study;Journal of Geophysical Research: Solid Earth;2014-04

5. Geochemistry of the Oceanic Crust;Frontiers in Geochemistry;2011-04-20