Stable isotope constraints on the mechanism of fluid flow during contact metamorphism around the Marulan Batholith, NSW, Australia-Reference-Cited by-同舟云学术

Stable isotope constraints on the mechanism of fluid flow during contact metamorphism around the Marulan Batholith, NSW, Australia

Published:2000-06 Issue: Volume:69-70 Page:291-295
ISSN:0375-6742
Container-title:Journal of Geochemical Exploration
language:en
Short-container-title:Journal of Geochemical Exploration

Author:

Buick I.S,Cartwright I

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference5 articles.

1. Permeability generation and resetting of tracers during metamorphic fluid flow: implications for advection–dispersion models;Cartwright;Contrib. Mineral. Petrol.,1998

2. Skarn development from limestones adjacent to the Glenrock Granodiorite, Marulan batholith, New South Wales, Australia;Chenhall;Aust. J. Earth Sci.,1993

3. Models for coupled fluid flow, mineral reaction and isotopic alteration during contact metamorphism: The Notch Peak aureole;Ferry;Utah Am. Mineral.,1991

4. Oxygen isotope geothermometers for metamorphic rocks;Matthews;J. Met. Geol.,1994

5. Calculation of oxygen isotope fractionations in hydroxyl-bearing silicates;Zheng;Earth Planet. Sci. Lett.,1993

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