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dc.contributor.advisor Yule, J. Douglas en
dc.contributor.author Hebeler, Aaron Keith en
dc.date.accessioned 2015-07-24T18:01:02Z en
dc.date.available 2015-07-24T18:01:02Z en
dc.date.copyright 2010 en
dc.date.issued 2010-08 en
dc.identifier.uri http://hdl.handle.net/10211.3/142909 en
dc.description Includes bibliographical references (leaves 71-76) en
dc.description California State University, Northridge. Department of Geological Sciences. en
dc.description.abstract The Mw 7.6 Kashmir earthquake and its surface rupture of the Balakot-Bagh fault, considered by many to be inactive prior to 2005, underscored the need to better understand the active tectonics of the northwest Himalaya and raised concern that other unrecognized active faults may occur in the region. The Riasi fault, by all accounts a close relative to the Balakot-Bagh fault, occurs ~150 km along strike to the southeast of the 2005 rupture. Both are reverse faults that place tightly folded Precambrian limestone over Pliocene and younger non-marine strata. (See more in text.) en
dc.description.statementofresponsibility by Aaron Keith Hebeler en
dc.format application/pdf en
dc.format image/jpeg en
dc.format.extent ix, 92 pages en
dc.language.iso en en
dc.publisher California State University, Northridge en
dc.rights.uri http://scholarworks.csun.edu//handle/10211.2/286 en
dc.subject.other Dissertations, Academic -- CSUN -- Geology. en
dc.title Middle holocene surface rupture of the Riasi fault, Kashmir, India en
dc.type Thesis en
dc.type Map en
dc.date.updated 2015-07-24T18:01:02Z en
dc.contributor.department Geological Sciences en
dc.description.degree M.S. en
dc.contributor.committeemember Miranda, Elena en
dc.contributor.committeemember Heermance, Richard en
dc.contributor.committeeMember Miranda, Elena en
dc.contributor.committeeMember Heermance, Richard en
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