Show simple item record

dc.contributor.advisorPenniston-Dorland, Sarah
dc.contributor.advisorWalker, Richard J.
dc.contributor.advisorFrench, Melodie
dc.contributor.authorGrabiec, Justine G.
dc.date.accessioned2017-02-15T19:35:26Z
dc.date.available2017-02-15T19:35:26Z
dc.date.issued2017-02-15
dc.identifierhttps://doi.org/10.13016/M25833
dc.identifier.urihttp://hdl.handle.net/1903/19161
dc.description.abstractThis 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.language.isoen_USen_US
dc.subjectgeochemistry, Catalina Schist, highly siderophile elements, X-ray fluorescence, deformation microstructures, metamorphic petrologyen_US
dc.titleOrigins of the Cottonwood Canyon fault rock in the Catalina Schisten_US
dc.typeResearch proposalen_US
dc.relation.isAvailableAtDigital Repository at the University of Maryland
dc.relation.isAvailableAtUniversity of Maryland (College Park, Md)
dc.contributor.departmentGeologyen_US


Files in this item

Thumbnail
Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record