Granite ascent in convergent orogenic belts: testing a model

Geology

Volumn 26, Issue 8, 1998, Pages 711-714

  Solar, Gary S ^a  

^a Bldg 142   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BINARY ALLOYS; DEFORMATION; LEAD ALLOYS; METAMORPHIC ROCKS; MONAZITE; PHOSPHATE MINERALS; SILICATE MINERALS; URANIUM ALLOYS; ZIRCON;

CONFIDENCE LIMIT; CRUSTAL ANATEXIS; CRUSTAL-SCALE SHEAR ZONES; CRYSTALLIZATION AGE; HIGH-GRADE METAMORPHIC ROCKS; REGIONAL METAMORPHISMS; SPATIAL RELATIONSHIPS; SYNTECTONIC GRANITES;

GRANITE;

GRANITE; MAGMATISM; OROGENIC BELT;

UNITED STATES;

EID: 84879879867     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1998)026<0711:GAICOB>2.3.CO;2     Document Type: Article

References (2)

1. Bradley, D., Tucker, R. D., and Lux, D., 1996, Early Emsian position of the Acadian orogenic front in Maine: Geological Society of America Abstracts with Programs, v. 28, no. 7, p. A-500.
2. Brown, M., 1994, The generation, segregation, ascent, and emplacement of granite magma: The migmatite-to-crustally-derived granite connection in thickened orogens: Earth Science Reviews, v. 36, p. 83-130.