Right lateral oblique slip movements followed by post-Ottawan (1050-1020 Ma) orogenic collapse along the Carthage-Colton shear zone: Data from the Dana Hill metagabbro body, Adirondack Mountains, New York

Memoir of the Geological Society of America

Volumn 197, Issue , 2004, Pages 357-378

  Johnson, Eric L ^a   Goergen, Eric T ^b   Fruchey, Benjamin L ^c  

^a HARTWICK COLLEGE   (United States)

^b UNIVERSITY OF MISSOURI   (United States)

^c UNIVERSITY OF WYOMING   (United States)

Author keywords

Granulite; Grenville; Shear zone

Indexed keywords

DEFORMATION; FELDSPAR;

ADIRONDACK LOWLANDS; ADIRONDACK MOUNTAINS; GRANULITE; GRENVILLE; METASEDIMENTARY BELT; OROGENIC COLLAPSE; SHEAR ZONE; STRUCTURAL LEVELS;

STRUCTURAL GEOLOGY;

IGNEOUS INTRUSION; METAGABBRO; METAMORPHISM; METASEDIMENTARY ROCK; OROGENIC BELT; SHEAR ZONE; SLIP RATE;

ADIRONDACK MOUNTAINS; NEW YORK [UNITED STATES]; UNITED STATES;

EID: 84870791350     PISSN: 00721069     EISSN: None     Source Type: Book Series    
DOI: 10.1130/0-8137-1197-5.357     Document Type: Article

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