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AMER GEOPHYSICAL UNIONCitation
Tibetan Magmatism Database 2017, 18 (11):4229 Geochemistry, Geophysics, GeosystemsRights
© 2017. American Geophysical Union. All Rights Reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
A database containing previously published geochronologic, geochemical, and isotopic data on Mesozoic to Quaternary igneous rocks in the Himalayan-Tibetan orogenic system are presented. The database is intended to serve as a repository for new and existing igneous rock data and is publicly accessible through a web-based platform that includes an interactive map and data table interface with search, filtering, and download options. To illustrate the utility of the database, the age, location, and Hf-t composition of magmatism from the central Gangdese batholith in the southern Lhasa terrane are compared. The data identify three high-flux events, which peak at 93, 50, and 15 Ma. They are characterized by inboard arc migration and a temporal and spatial shift to more evolved isotopic compositions. Plain Language Summary A new database with a web-based interface is presented that contains compiled geochronologic, geochemical, and isotopic data on igneous rocks in the Himalaya-Tibetan orogen.Note
6 month embargo; published online: 3 November 2017.ISSN
15252027Version
Final published versionSponsors
National Science Foundation [EAR-1008527]Additional Links
http://doi.wiley.com/10.1002/2017GC007217ae974a485f413a2113503eed53cd6c53
10.1002/2017GC007217