Most Granitoid Rocks are Cumulates: Deductions from Hornblende Compositions and Zircon Saturation
Abstract
Cumulate processes in granitic magma systems are thought by some to be negligible and by others to be common and widespread. Because most granitic rocks lack obvious evidence of accumulation, such as modal layering, other means of identifying cumulate rocks and estimating proportions of melt lost must be developed. The approach presented here utilizes major and trace element compositions of hornblende to estimate melt compositions necessary for...
Paper Details
Title
Most Granitoid Rocks are Cumulates: Deductions from Hornblende Compositions and Zircon Saturation
Published Date
Nov 1, 2019
Journal
Volume
60
Issue
11
Pages
2227 - 2240
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