dc.contributor.advisor	Penniston-Dorland, Sarah
dc.contributor.advisor	Walker, Richard J.
dc.contributor.advisor	French, Melodie
dc.contributor.author	Grabiec, Justine G.
dc.contributor.department	Geology	en_US
dc.date.accessioned	2017-02-15T19:35:26Z
dc.date.available	2017-02-15T19:35:26Z
dc.date.issued	2017-02-15
dc.description.abstract	This is a proposal for research conducted on a fault in the Catalina Schist on Santa Catalina Island, California. By analyzing samples from the fault via geochemical, petrographic, petrological, and structural methods, the origins of the rock within the fault will be compared to the rock containing the fault in order to understand implications regarding the mechanisms by which the fault formed as well as the origin of the fault rock. Methods include X-ray fluorescence, electron probe microanalysis, highly siderophile element geochemistry using thermal ionization mass spectrometry and inductively couple plasma mass spectrometry, and petrography.	en_US
dc.identifier	https://doi.org/10.13016/M25833
dc.identifier.uri	http://hdl.handle.net/1903/19161
dc.language.iso	en_US	en_US
dc.relation.isAvailableAt	Digital Repository at the University of Maryland
dc.relation.isAvailableAt	University of Maryland (College Park, Md)
dc.subject	geochemistry, Catalina Schist, highly siderophile elements, X-ray fluorescence, deformation microstructures, metamorphic petrology	en_US
dc.title	Origins of the Cottonwood Canyon fault rock in the Catalina Schist	en_US
dc.type	Research proposal	en_US

Origins of the Cottonwood Canyon fault rock in the Catalina Schist

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