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From granulite fluids to quartz-carbonate megashear zones: The gold rush

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Date

2014

Authors

Fu, Bin
Touret, Jacques L.R.

Journal Title

Journal ISSN

Volume Title

Publisher

Elsevier

Abstract

At peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed by large amounts of two key low water activity fluids: (i) high-density CO2 and/or (ii) concentrated saline solutions. These fluids are either internally-derived,

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Keywords

Citation

URI

http://hdl.handle.net/1885/18796

Collections

ANU Research Publications

Source

Geoscience Frontiers (Previously Earth Science Frontiers)

Type

Journal article

Book Title

Entity type

Access Statement

Open Access

License Rights

DOI

10.1016/j.gsf.2014.03.013

Restricted until

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01_Fu_From_granulite_fluids_to_2014.pdf (2.18 MB)

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