Application of mineral thermometers and barometers to granitoid igneous rocks: The Etive Complex, W Scotland

M. Moazzen; G. T R Droop

doi:10.1007/s00710-004-0059-z

Application of mineral thermometers and barometers to granitoid igneous rocks: The Etive Complex, W Scotland

M. Moazzen, G. T R Droop

Research output: Contribution to journal › Article › peer-review

Abstract

The Etive complex, one of the Caledonian 'Newer Granites' of Scotland, is a ring complex of Devonian age, ranging in composition from pyroxene-diorite to leucogranite. Six samples, representing the major rock units in the southern parts of the Etive complex were chosen for mineral chemical studies and for estimation of the pressure and temperature conditions of magmatic crystallisation. Application of Al- in-hornblende barometry and crossite contents of amphiboles indicates a pressure

Original language	English
Pages (from-to)	27-53
Number of pages	26
Journal	Mineralogy and Petrology
Volume	83
Issue number	1-2
DOIs	https://doi.org/10.1007/s00710-004-0059-z
Publication status	Published - Jan 2005

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title = "Application of mineral thermometers and barometers to granitoid igneous rocks: The Etive Complex, W Scotland",

abstract = "The Etive complex, one of the Caledonian 'Newer Granites' of Scotland, is a ring complex of Devonian age, ranging in composition from pyroxene-diorite to leucogranite. Six samples, representing the major rock units in the southern parts of the Etive complex were chosen for mineral chemical studies and for estimation of the pressure and temperature conditions of magmatic crystallisation. Application of Al- in-hornblende barometry and crossite contents of amphiboles indicates a pressure",

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AU - Droop, G. T R

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AB - The Etive complex, one of the Caledonian 'Newer Granites' of Scotland, is a ring complex of Devonian age, ranging in composition from pyroxene-diorite to leucogranite. Six samples, representing the major rock units in the southern parts of the Etive complex were chosen for mineral chemical studies and for estimation of the pressure and temperature conditions of magmatic crystallisation. Application of Al- in-hornblende barometry and crossite contents of amphiboles indicates a pressure

U2 - 10.1007/s00710-004-0059-z

DO - 10.1007/s00710-004-0059-z

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IS - 1-2

ER -

Application of mineral thermometers and barometers to granitoid igneous rocks: The Etive Complex, W Scotland

Abstract

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