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Tectonic pumping of pervasive granitic melts
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Solid Earth Geology.
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences. Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences, Solid Earth Geology. Berggrundsgeologi.
2001 (English)In: TECTONOPHYSICS, ISSN 0040-1951, Vol. 332, no 4, 387-402 p.Article in journal (Refereed) Published
Abstract [en]

Finite element 2D models are used to study how tectonic stresses pump pervasive granitic melts within migmatites. We start by assuming elliptical melt-filled veins (of different orientations) interconnected by the assumption that they share the same press

Place, publisher, year, edition, pages
2001. Vol. 332, no 4, 387-402 p.
Keyword [en]
pervasive granitic melts; migmatization; vein network; EXPERIMENTAL DEFORMATION; FRACTURE PROPAGATION; CONTINENTAL-CRUST; SEGREGATION; MAGMAS; ASCENT; MANTLE; EMPLACEMENT; SIMULATION; GENERATION
Identifiers
URN: urn:nbn:se:uu:diva-37877OAI: oai:DiVA.org:uu-37877DiVA: diva2:65776
Note
Addresses: Simakin A, Russian Acad Sci, Inst Expt Mineral, Chernogolovka 142432, Moscow District, Russia. Univ Uppsala, Hans Ramberg Tect Lab, Dept Earth Sci, SE-75236 Uppsala, Sweden.Available from: 2007-04-12 Created: 2007-04-12 Last updated: 2011-01-14

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