The retrogradeP–T–tpath for low‐pressure granulites from the Reynolds Range, central Australia: petrological constraints and implications for low‐P/high‐Tmetamorphism-Reference-Cited by-同舟云学术

The retrogradeP–T–tpath for low‐pressure granulites from the Reynolds Range, central Australia: petrological constraints and implications for low‐P/high‐Tmetamorphism

Published:1998-06 Issue:4 Volume:16 Page:511-529
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:Journal of Metamorphic Geology

Author:

BUICK I. S.¹,CARTWRIGHT I.¹,HARLEY S. L.¹

Affiliation:

1. ¹ Department of Earth Sciences & Victorian Institute of Earth and Planetary Sciences (VIEPS), La Trobe University, Bundoora, Victoria 3083, Australia (email: ), ² Department of Earth Sciences & VIEPS, Monash University, Clayton, Victoria 3168, Australia, ³ Grant Institute of Geology, Department of Geology and Geophysics, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW , Scotland, UK

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1998.00152.x

Reference55 articles.

1. Experimental investigation and application of garnet granulite equilibria

2. Fluid—Rock Interaction during Low-Pressure Polymetamorphism of the Reynolds Range Group, Central Australia

3. BuickI. S.FreiR.&CartwrightI.1998;The timing of high‐temperature retrogression in the Reynolds Range central Australia: constraints from single mineral Pb–Pb dating.Contributions to Mineralogy and Petrology(submitted)

4. Cordierite as a monitor of fluid and melt H2O contents in the lower crust: An experimental calibration

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