Can trace element distributions in migmatites be used as analogues in understanding petrogenesis of anatectic granites

Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy

Volumn 24, Issue 3, 1999, Pages 295-298

  Nabelek, P I ^a   Bartlett, C ^a   Glascock, M ^a  

^a UNIVERSITY OF MISSOURI   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ANATEXIS; GRANITE; MIGMATITE; PETROGENESIS; TRACE ELEMENT;

EID: 0032781910     PISSN: 14641895     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1464-1895(99)00032-0     Document Type: Article

References (11)

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2. Brown, M. and D'Lemos, R.S., The caledonian granites of mancellia, northeast armorican massif of France: Relationship to the St. Malo migmatite belt, petrogenesis and tectonic setting, Precamb. Res., 51, 393-427, 1991.
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8. Nabelek, P.I., Quartz-sillimanite leucosomes in high-grade schists, Black Hills, South Dakota: A perspective on the mobility of A1 in high-grade metamorphic rocks, Geology, 25, 995-998, 1997.
9. Nabelek, P.I. and Bartlett, C.D., Petrologic and geochemical links between the post-collisional Proterozoic Harney Peak leucogranite, South Dakota, USA, and its source rocks, Lithos, In press, 1998.
10. Nabelek, P.I., Russ-Nabelek, C., and Haeussler, G.T., Stable isotope evidence for the petrogenesis and fluid evolution in the Proterozoic Harney Peak leucogranite, Black Hills, South Dakota, Geochim.Cosmochim. Acta, 56, 403-417, 1992.
11. Power, G.M., Geochemical differences between the cadomian granites of Mancellia and the St. Malo migmatites, Armorican Massif, France, J. Geol. Soc. London, 150, 465-468, 1993.