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[PDF][PDF] Rheology of the upper mantle and the mantle wedge: A view from the experimentalists
G Hirth, D Kohlstedf - Geophysical monograph-american …, 2003 - soest.hawaii.edu
In this manuscript we review experimental constraints for the viscosity of the upper mantle.
We first analyze experimental data to provide a critical review of flow law parameters for …
We first analyze experimental data to provide a critical review of flow law parameters for …
A Cenozoic record of deep oceanic Zn isotopic composition in ferromanganese crusts
M Zhao, N Planavsky, X Wang, Y Zhang… - American Journal of …, 2023 - ajsonline.org
Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …
Strength of the lithosphere: Constraints imposed by laboratory experiments
DL Kohlstedt, B Evans… - Journal of Geophysical …, 1995 - Wiley Online Library
The concept of strength envelopes, developed in the 1970s, allowed quantitative predictions
of the strength of the lithosphere based on experimentally determined constitutive equations …
of the strength of the lithosphere based on experimentally determined constitutive equations …
Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere
G Hirth, DL Kohlstedt - Earth and Planetary Science Letters, 1996 - Elsevier
The influence of water on the dynamics of the oceanic upper mantle is re-evaluated based
on recent experimental constraints on the solubility of water in mantle minerals and earlier …
on recent experimental constraints on the solubility of water in mantle minerals and earlier …
S.-I. Karato 2008. Deformation of Earth Materials. An Introduction to the Rheology of Solid Earth. x+ 463 pp. Cambridge, New York, Melbourne: Cambridge University …
EH Rutter - Geological Magazine, 2010 - cambridge.org
Archean passive margins. In When Did Plate Tectonics Begin on Planet Earth?(eds KC
Condie & V. Pease.), pp. 149–56. Geological Society of America Special Paper no. 440 …
Condie & V. Pease.), pp. 149–56. Geological Society of America Special Paper no. 440 …
Mantle melting and melt extraction processes beneath ocean ridges: evidence from abyssal peridotites
Y Niu - Journal of Petrology, 1997 - academic.oup.com
This paper presents the results of the first quantitative petrological modelling of abyssal
peridotites. The mantle beneath a ridge may be considered as two regions:(1) the melting …
peridotites. The mantle beneath a ridge may be considered as two regions:(1) the melting …
Effect of pore geometry on VP/VS: From equilibrium geometry to crack
Y Takei - Journal of Geophysical Research: Solid Earth, 2002 - Wiley Online Library
Seismic wave velocities of melt or aqueous fluid containing systems are studied over a wide
range of pore shapes, including oblate spheroids, tubes, cracks, and an equilibrium …
range of pore shapes, including oblate spheroids, tubes, cracks, and an equilibrium …
A review of melt migration processes in the adiabatically upwelling mantle beneath oceanic spreading ridges
We review physical and chemical constraints on the mechanisms of melt extraction from the
mantle beneath mid–ocean ridges. Compositional constraints from MORB and abyssal …
mantle beneath mid–ocean ridges. Compositional constraints from MORB and abyssal …
High‐temperature deformation of dry diabase with application to tectonics on Venus
SJ Mackwell, ME Zimmerman… - Journal of Geophysical …, 1998 - Wiley Online Library
We have performed an experimental study to quantify the high‐temperature creep behavior
of natural diabase rocks under dry deformation conditions. Samples of both Maryland …
of natural diabase rocks under dry deformation conditions. Samples of both Maryland …
Water, partial melting and the origin of the seismic low velocity and high attenuation zone in the upper mantle
The common belief that the seismic low velocity and high attenuation zone (the
asthenosphere) is caused by the presence of a small amount of melt is not supported by …
asthenosphere) is caused by the presence of a small amount of melt is not supported by …