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MODEL FOR THE GENESIS OF YOUNG CONTINENTAL-ARC SHOSHONITES IN THE TALAMANCA CORDILLERA, COSTA RICA

dc.contributor.authorAlfaro, Aristides Jose
dc.contributor.chairGazel, Esteban
dc.contributor.committeeMemberWhite, Bill
dc.contributor.committeeMemberKeranen, Kade
dc.date.accessioned2021-12-20T20:34:22Z
dc.date.available2021-12-20T20:34:22Z
dc.date.issued2021-08
dc.description106 pages
dc.description.abstractAristides José Alfaro Gálvez investigated the Late Cenozoic magmatism of the Talamanca Cordillera, Southern Central America. Six to five Ma continental-arc shoshonites and other high-K rocks crop out among the summits of that region. Their trace element composition (Sr~1700 ppm at Rb~120 ppm concentrations) suggests a genesis related to subduction processes rather than lower crustal melting. This work integrates Monte Carlo simulations of trace element geochemistry and isotopic evidence in order to explain the origin of these highly enriched continental arc igneous rocks. The main conclusion is that the trace element budget of the Talamanca arc rocks requires the input of an incompatible element-enriched component, similar in composition to the Cocos Island Province (Pacific Ocean), as a result of slab melting of subducted seamounts.
dc.identifier.doihttps://doi.org/10.7298/8j0s-qr88
dc.identifier.otherAlfaro_cornell_0058O_11205
dc.identifier.otherhttp://dissertations.umi.com/cornell:11205
dc.identifier.urihttps://hdl.handle.net/1813/110379
dc.language.isoen
dc.subjectCentral America
dc.subjectContinental crust
dc.subjectShoshonite
dc.subjectSlab melting
dc.subjectSubduction
dc.subjectTalamanca cordillera
dc.titleMODEL FOR THE GENESIS OF YOUNG CONTINENTAL-ARC SHOSHONITES IN THE TALAMANCA CORDILLERA, COSTA RICA
dc.typedissertation or thesis
dcterms.licensehttps://hdl.handle.net/1813/59810
thesis.degree.disciplineGeological Sciences
thesis.degree.grantorCornell University
thesis.degree.levelMaster of Science
thesis.degree.nameM.S., Geological Sciences

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