CHAPTER 6: GRANITES, MIGMATITES AND RESIDUAL GRANULITES: RELATIONSHIPS AND PROCESSES
Author:
Affiliation:
1. Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, MD 20742-4211, USA E-mail: mbrown@umd.edu
Publisher
Mineralogical Association of Canada
Link
https://pubs.geoscienceworld.org/books/edited-volume/chapter-pdf/6274625/sc38_ch06.pdf
Reference312 articles.
1. Segregation of leucogranite microplutons during syn-anatectic deformation – an example from the Taylor Valley, Antarctic;Allibone;J. Metamorphic Geol.,1992
2. Correlations between U, Th content and metamorphic grade in the western Namaqualand Belt, South Africa, with implications for radioactive heating of the crust;Andreoli;J. Petrol.,2006
3. The genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006
4. Thermal constraints on the emplacement rate of a large intrusive complex: the Manaslu leuco-granite, Nepal Himalaya;Annen;J. Petrol.,2006
5. Microstructure of deformation bands in porous sandstones at Arches National Park, Utah;Antonellini;J. Struct. Geol.,1994
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