Can the Magmatic Conditions of the Martian Nakhlites be Discerned via Investigation of Clinopyroxene and Olivine Intracrystalline Misorientations?

Can the Magmatic Conditions of the Martian Nakhlites be Discerned via Investigation of Clinopyroxene and Olivine Intracrystalline Misorientations?

Deformation is a near ubiquitous process that is observed within nearly all naturally forming rocks. Electron backscatter diffraction (EBSD) is a technique that enables slip-systems (a form of plastic deformation) to be inferred from intracrystalline misorientations at a comparable scale to the repr...

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Bibliographic Details
Main Authors: Griffin, S., Daly, L., Piazolo, S., Forman, Lucy, Cohen, B.E., Lee, M.R., Trimby, P.W., Baumgartner, R.J., Benedix, Gretchen, Hoefnagels, B.
Format: Journal Article
Language:English
Published: AMER GEOPHYSICAL UNION 2022
Subjects:
Science & Technology
Physical Sciences
Geochemistry & Geophysics
EBSD
nakhlite
slip-systems
Mars
olivine
clinopyroxene
HIGH-TEMPERATURE DEFORMATION
LATTICE PREFERRED ORIENTATIONS
SINGLE-CRYSTAL CLINOPYROXENES
SLIP SYSTEMS
UPPER-MANTLE
B-TYPE
PLASTIC-DEFORMATION
SEISMIC ANISOTROPY
DYNAMIC RECRYSTALLIZATION
WATER-CONTENT
Online Access:http://hdl.handle.net/20.500.11937/94372

Internet

http://hdl.handle.net/20.500.11937/94372

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