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Magma flow within the Tavares pluton, northeastern Brazil: Compositional and thermal convection
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2001 (English)In: GEOLOGICAL SOCIETY OF AMERICA BULLETIN, ISSN 0016-7606, Vol. 113, no 4, 508-520 p.Article in journal (Refereed) Published
Abstract [en]

Crystallization coupled with gravity removal of depleted interstitial melt has long been recognized as a mechanism of magma differentiation. Similarly, heat released by synplutonic basaltic magma intrusions has long been recognized as capable of driving c

Place, publisher, year, edition, pages
ASSOC ENGINEERING GEOLOGISTS GEOLOGICAL SOCIETY AMER , 2001. Vol. 113, no 4, 508-520 p.
Keyword [en]
fluid dynamics; granite; magma chambers; magmatic; structures; SOUTH-MOUNTAIN BATHOLITH; CENTRAL SIERRA-NEVADA; FRACTIONAL CRYSTALLIZATION; EMPLACEMENT KINEMATICS; NOVA-SCOTIA; DIFFERENTIATION; GRANITES; CALIFORNIA; INTRUSION; FABRICS
Identifiers
URN: urn:nbn:se:uu:diva-37899OAI: oai:DiVA.org:uu-37899DiVA: diva2:65798
Note
Addresses: Weinberg RF, Univ Western Australia, Ctr Global Metallogeny, Nedlands, WA 6907, Australia. Univ Fed Pernambuco, Dept Geol, Recife, PE, Brazil. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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