Poromechanical and Crack Evolution of Olivine‐Rich Rock During Serpentinization
Abstract Serpentinization alters the strength, fracture behavior, and rheology of ultramafic rocks, yet the coupled evolution of mineral reactions, cracking, and mechanical softening remains poorly constrained. We experimentally simulated serpentinization in dunite at 220°C and 15 MPa for 14 and 30 days and compared the reacted specimens with dry heat ...
Ummu‐kulthum Lawal, Kiseok Kim
wiley +1 more source
Plate‐Scale Imaging of Eastern US Reveals Ancient and Ongoing Continental Deformation
Eastern North America was constructed over several Wilson cycles, culminating in the breakup of Pangea. Previous seismological imaging lacked the resolution to depict precisely how ancient tectonic boundaries manifest throughout the lithosphere, how ...
Brennan Brunsvik +2 more
doaj +1 more source
A metasomatized lithospheric mantle control on the metallogenic signature of post-subduction magmatism. [PDF]
Holwell DA +7 more
europepmc +1 more source
Experimental flow law for olivine at moderate T and PA first draft report on this subproject will be presented in the Draf Periodic report on month ...
openaire +1 more source
Nanoscale solid-fluid interaction and amphibole formation in the lithospheric mantle. [PDF]
Lange TP +7 more
europepmc +1 more source
Catastrophic shear-removal of subcontinental lithospheric mantle beneath the Colorado Plateau by the subducted Farallon slab. [PDF]
Hernández-Uribe D, Palin RM.
europepmc +1 more source
Lithological variations in the mantle source regions under mid-ocean ridges and ocean islands have been proposed to play a key role in controlling melt generation and basalt composition.
Maclennan, John, Shorttle, Oliver
core +1 more source
LITHOSPHERE MANTLE DENSITY BENEATH THE SIBERIAN CRATON [PDF]
Cherepanova, Yulia, Artemieva, Irina
openaire +2 more sources
Accretion of "young" Phanerozoic subcontinental lithospheric mantle triggered by back-arc extension-the case of the Ivrea-Verbano Zone. [PDF]
Ogunyele AC +4 more
europepmc +1 more source
Enrichment processes in the Patagonian lithospheric mantle.
Several mantle xenolith suites entrained in basalts from back arc mafic plateau in Patagonia were investigated. They appear to be affected by both depletion processes due to melt extraction and enrichment processes. These latter are related to metasomatic and refertilization melts that, migrating through the mantle, change its composition adding ...
Melchiorre, Massimiliano +3 more
openaire +1 more source

