In the project ''Earth Materials and Earth Dynamics'' we linked fundamental and exploratory, experimental, theoretical, and computational research programs to shed light on the current and past states of the dynamic Earth. Our objective was to combine different geological, geochemical, geophysical, and materials science analyses with numerical techniques to illuminate active processes in the Earth. These processes include fluid-rock interactions that form and modify the lithosphere, non-linear wave attenuations in rocks that drive plate tectonics and perturb the earth's surface, dynamic recrystallization of olivine that deforms the upper mantle, development of texture in high-pressure olivine polymorphs that create anisotropic velocity regi...
One goal of high pressure mineralogy is to determine the composition of the earth's interior. This e...
Field studies of ophiolites (exhumed mantle from beneath mid-ocean ridges) suggest that melt transpo...
AbstractOur understanding of the chemical and physical structure of the mantle is driven by connecti...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheri...
Physical properties of rocks studied in the laboratory are useful to provide constraints on the dyna...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
Experimental petrology is the materials science of geophysical sciences. When packages of rock mater...
The paper is an overview of the current status on experimental petrology — its objectives and its ma...
The major results of research in the United States for 1971–1974 in the areas of static, high-pressu...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
During the two decades following the plate tectonic revolution, cartoons of mantle convection have ...
International audienceThis special issue in honour of the late Olivier Jaoul brings together contrib...
Since the acceptance of the theory of plate tectonics in the late 1960s, numerical and laboratory st...
Analog, or physical, models have been used to investigate problems in structural geology and tectoni...
One goal of high pressure mineralogy is to determine the composition of the earth's interior. This e...
Field studies of ophiolites (exhumed mantle from beneath mid-ocean ridges) suggest that melt transpo...
AbstractOur understanding of the chemical and physical structure of the mantle is driven by connecti...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheri...
Physical properties of rocks studied in the laboratory are useful to provide constraints on the dyna...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
Experimental petrology is the materials science of geophysical sciences. When packages of rock mater...
The paper is an overview of the current status on experimental petrology — its objectives and its ma...
The major results of research in the United States for 1971–1974 in the areas of static, high-pressu...
This is the final report of a three-year, Laboratory Directed Research and Development (LDRD) projec...
During the two decades following the plate tectonic revolution, cartoons of mantle convection have ...
International audienceThis special issue in honour of the late Olivier Jaoul brings together contrib...
Since the acceptance of the theory of plate tectonics in the late 1960s, numerical and laboratory st...
Analog, or physical, models have been used to investigate problems in structural geology and tectoni...
One goal of high pressure mineralogy is to determine the composition of the earth's interior. This e...
Field studies of ophiolites (exhumed mantle from beneath mid-ocean ridges) suggest that melt transpo...
AbstractOur understanding of the chemical and physical structure of the mantle is driven by connecti...