High-grade localized metasomatic alteration of the granitic gneiss surrounding a clinopyroxene-rich pegmatoid dyke: Söndrum stenhuggeriet, Halmstad, SW Sweden

Author:

Harlov D. E.12,Van Den Kerkhof A.3,Johansson L.4

Affiliation:

1. GeoForschungsZentrum Potsdam; Telegrafenberg D-14473 Potsdam Germany

2. Department of Geology; University of Johannesburg; P.O. Box 524 Auckland Park 2006 South Africa

3. Geowissenschaftliches Zentrum der Universität Göttingen; Goldschmidtstrasse 3 D-37077 Göttingen Germany

4. Department of Geology; University of Lund; Sölvegatan 12 SE-22362 Lund Sweden

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Reference77 articles.

1. Geochronology and structural setting of the 1.38 Ga Torpa granite; implications for charnockite formation in SW Sweden;Åhäll;Geologiska Föreningens i Stockholm Förhandlingar,1997

2. Sveconorwegian (-Grenvillian) deformation, metamorphism and leucosome formation in SW Sweden, SW Baltic Shield; constraints from a Mesoproterozoic granite intrusion;Andersson;Precambrian Research,1999

3. Reequilibration of fluid inclusions: bulk-diffusion;Bakker;Lithos,2009

4. CaCl2-hydrate nucleation in synthetic fluid inclusions;Baumgartner;Chemical Geology,2009

5. Dehydration melting and water-saturated melting of basaltic and andesitic greenstones and amphibolites at 1, 3, and 6.9 kb;Beard;Journal of Petrology,1991

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