Zobrazeno 1 - 9
of 9
pro vyhledávání: '"E. Marc Parmentier"'
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Author Posting. © American Geophysical Union, 2020. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Solid Earth
Autor:
Yan Liang, E. Marc Parmentier
Publikováno v:
Journal of Petrology. 51:125-152
Autor:
Kelin Wang, S. Lin, E. Marc Parmentier, Amandine Marie Cagnioncle, Richard F. Katz, Mark D. Behn, Marc Spiegelman, Claire A. Currie, Scott D. King, Peter E. van Keken, Jiangheng He
Publikováno v:
Physics of the Earth and Planetary Interiors. 171:187-197
We have developed a suite of benchmarks to facilitate the comparison of numerical models for the dynamics and thermal structure of subduction zones. The benchmark cases are based on a thermomechanical approach in which the slab is prescribed kinemati
Publikováno v:
Geophysical Research Letters. 37
High-porosity dunite channels are important pathways for melt migration in the mantle. To better understand the first order characteristics of the high-porosity melt channel and its associated peridotite lithologies in an upwelling mantle, we conduct
Publikováno v:
Science (New York, N.Y.). 321(5897)
Mars' crustal magnetic field was most likely generated by dynamo action in the planet's early history. Unexplained characteristics of the field include its strength, concentration in the southern hemisphere, and lack of correlation with any surface f
Publikováno v:
Journal of Geophysical Research. 96:20933
The present study assesses the mantle diapir models of corona origin using the basic characteristics of coronas: relatively raised topography, annuli of compressional ridges, volcanism, and peripheral trough. Both rising and and sinking diapirs are m
Autor:
E. Marc Parmentier, D. L. Bindschadler
Publikováno v:
Journal of Geophysical Research. 95:21329
The crust and mantle of Venus can be represented by a model of a layered structure stratified in both density and viscosity. This structure consists of a brittle-elastic upper crustal layer; a ductile weaker crustal layer; a strong upper mantle layer
Publikováno v:
Geophysical Research Letters. 13:681-684
We have formulated a new class of plate-bending equations which simulates the flexure of the lithosphere at mid-ocean ridges. The stress-accumulation effect in a growing (moving and thickening) lithosphere significantly changes the flexural behavior.
Publikováno v:
Physics of Fluids. 20:2012
Microscopic observations of the flow of fresh canine blood in a separated region formed by a step in a polyurethane surface have been made. These observations show the formation of large clumps of freely floating aggregates of platelets. These clumps