The Cadillac Mountain intrusive complex, Maine: The role of shallow-level magma chamber processes in the generation of A-type granites

Memoir of the Geological Society of America

Volumn 191, Issue , 1997, Pages 397-418

  Wiebe, Robert A ^a   Holden, Jonathan B ^a,e   Coombs, Michelle L ^b,f   Wobus, Reinhard A ^b   Schuh, Kathleen J ^c,g   Plummer, Benjamin P ^d,f  

^a FRANKLIN AND MARSHALL COLLEGE   (United States)

^b WILLIAMS COLLEGE   (United States)

^c 931 College Mall   (United States)

^d WASHINGTON AND LEE UNIVERSITY   (United States)

^e Univ of New Hampshire   (United States)

^f University of North Carolina ^*  (United States)

^g University of North Carolina at Chapel Hill   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BASALT; FELDSPAR; LANDFORMS; MICA;

A-TYPE GRANITE; CHEMICAL TRANSFORMATIONS; GRANITIC MAGMAS; HIGH FIELD STRENGTH ELEMENTS; INCOMPATIBLE ELEMENT; MAFIC ENCLAVES; SHALLOW DEPTHS; SILICIC MAGMAS;

GRANITE;

A-TYPE ROCK; BASALT; DIORITE; FRACTIONATION; GABBRO; GRANITE; LAYERED INTRUSION; MAGMA CHAMBER;

CADILLAC MOUNTAIN; MAINE; UNITED STATES;

EID: 0042906073     PISSN: 00721069     EISSN: None     Source Type: Book Series    
DOI: 10.1130/0-8137-1191-6.397     Document Type: Article

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