Trace element mass balance in hydrous adiabatic mantle melting: The Hydrous Adiabatic Mantle Melting Simulator version 1 (HAMMS1)

Abstract A numerical mass balance calculation model for the adiabatic melting of a dry to hydrous peridotite has been programmed in order to simulate the trace element compositions of basalts from mid‐ocean ridges, back‐arc basins, ocean islands, and large igneous provinces. The Excel spreadsheet‐ba...

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Bibliographic Details
Main Authors: Jun‐Ichi Kimura, Hiroshi Kawabata
Format: Article
Language:English
Published: Wiley 2014-06-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1002/2014GC005333
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