Age and magnetic fabric of the Três Córregos granite batholith: Evidence for Ediacaran transtension in the Ribeira Belt (SE Brazil)

International Journal of Earth Sciences

Volumn 102, Issue 6, 2013, Pages 1563-1581

  Salazar, Carlos A ^a,b   Archanjo, Carlos J ^a   Rodrigues, Sérgio W de O ^c   Hollanda, Maria Helena B M ^a   Liu, Dunyi ^d  

^a UNIVERSITY OF SÃO PAULO   (Brazil)

^b FEDERAL UNIVERSITY OF AMAZONAS   (Brazil)

^c STATE UNIVERSITY OF RIO DE JANEIRO   (Brazil)

^d INSTITUTE OF MINERAL RESOURCES   (China)

Author keywords

Anisotropy of magnetic susceptibility; Granite; Ribeira belt; SE Brazil; U Pb zircon geochronology

Indexed keywords

BATHOLITH; CONTINENTAL ARC; EDIACARAN; EMPLACEMENT; FLUORITE; GEOCHRONOLOGY; HOST ROCK; MAGNETIC ANISOTROPY; MAGNETIC FABRIC; METASEDIMENTARY ROCK; PLUTON; SHRIMP DATING; STRAIN RATE; STRIKE-SLIP FAULT; UPPER CRUST; URANIUM-LEAD DATING; ZIRCON;

BRAZIL; RIBEIRA BELT;

EID: 84881610294     PISSN: 14373254     EISSN: 14373262     Source Type: Journal    
DOI: 10.1007/s00531-013-0908-2     Document Type: Article

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