Structurally controlled fluid flow during contact metamorphism in the Ritter Range pendant, California, USA

Structurally controlled fluid flow during contact metamorphism in the Ritter Range pendant, California, USA

The mineralogy and O-isotope geochemistry of siliceous limestones from the Ritter Range pendant constrain the geometry and amount of fluid flow during contact metamorphism associated with emplacement of a pluton of the Sierra Nevada Batholith.

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Veröffentlicht in:Contributions to mineralogy and petrology 1998-02, Vol.130 (3-4), p.358-378
Hauptverfasser: Ferry, John M., Sorensen, Sorena S., Rumble III, Douglas
Format: Artikel
Sprache:eng
Schlagworte:
Chemistry
Fluid flow
Fluids
Geochemistry
Geology
Metamorphism
Mineralogy
Minerals
Petrology
Online-Zugang:Volltext
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Beschreibung
Zusammenfassung:The mineralogy and O-isotope geochemistry of siliceous limestones from the Ritter Range pendant constrain the geometry and amount of fluid flow during contact metamorphism associated with emplacement of a pluton of the Sierra Nevada Batholith.
ISSN:0010-7999
1432-0967
DOI:10.1007/s004100050371