Concentric slow cooling of a low-P-high-T terrane: Evidence from 1600-1300 Ma mica dates in the 1780-1700 Ma Black Hills Orogen, South Dakota, U.S.A

American Mineralogist

Volumn 93, Issue 8-9, 2008, Pages 1215-1229

  Dahl, Peter S ^a   Foland, Kenneth A ^b  

^a KENT STATE UNIVERSITY   (United States)

^b OHIO STATE UNIVERSITY   (United States)

Author keywords

And lead; Argon; Argon retentivity of micas (field based); Geochronology; High temperature studies; Major and minor elements; Micas; Pegmatites; Radiogenic isotopes; Strontium

Indexed keywords

ARGON; BIOTITE; COOLING; GEOCHRONOLOGY; GRANITE; METAMORPHIC ROCKS; PHOSPHATE MINERALS; STRONTIUM;

CRYSTALLINE CORE; GRANITE EMPLACEMENT; HIGH TEMPERATURE; MAJOR AND MINOR ELEMENTS; PEGMATITES; RADIAL PATTERNS; RADIOGENIC ISOTOPES; REGIONAL PATTERN;

MICA;

ARGON-ARGON DATING; AUREOLE; COOLING; COUNTRY ROCK; GEOCHRONOLOGY; HIGH TEMPERATURE; MICA; P-T CONDITIONS; TEMPERATURE EFFECT; TERRANE; UPLIFT;

BLACK HILLS; NORTH AMERICA; SOUTH DAKOTA; UNITED STATES;

MICAS;

EID: 50849083531     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2008.2633     Document Type: Article

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