Zobrazeno 1 - 10
of 238
pro vyhledávání: '"David L. Kohlstedt"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 9, Pp n/a-n/a (2023)
Abstract We investigated the co‐evolution of melt, shape, and crystallographic preferred orientations (MPOs, SPOs, and CPOs) in experimentally deformed partially molten rocks, from which we calculated the influence of MPO and CPO on seismic anisotr
Externí odkaz:
https://doaj.org/article/572c6cce8bbb402899e0c60e5a60e827
Traditionally, investigations of the rheology and deformation of the lithosphere (the rigid or mechanically strong outer layer of the Earth, which contains the crust and the uppermost part of the mantle) have taken place at one scale in the laborator
To study the mechanical behavior of polymineralic rocks, we performed deformation experiments on two‐phase aggregates of olivine (Ol) + ferropericlase (Per) with periclase fractions (fPer) between 0.1 and 0.8. Each sample was deformed in torsion at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3ae321a846580974c8e8fbd421ceec3d
https://www.repository.cam.ac.uk/handle/1810/348722
https://www.repository.cam.ac.uk/handle/1810/348722
To study the microstructural evolution of polymineralic rocks, we performed deformation experiments on two‐phase aggregates of olivine (Ol) + ferropericlase (Per) with periclase fractions (fPer) between 0.1 and 0.8. Additionally, single‐phase sam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::734f06818b7411e8a39b5133d08812d9
https://www.repository.cam.ac.uk/handle/1810/348720
https://www.repository.cam.ac.uk/handle/1810/348720
Publikováno v:
Geochemistry, Geophysics, Geosystems. 20:2985-2996
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Publikováno v:
Prof. Pec
To investigate channelization during migration of a reactive melt, we performed a series of Darcy-type experiments in which an alkali basalt infiltrated partially molten harzburgites and lherzolites at a confining pressure of 300 MPa, temperatures of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ba69faf67f966f4a689527ca2d92c56
https://hdl.handle.net/1721.1/133164
https://hdl.handle.net/1721.1/133164