Hydrothermal gold mineralization at the Hira Buddini gold mine, India: Constraints on fluid evolution and fluid sources from boron isotopic compositions of tourmaline

Mineralium Deposita

Volumn 43, Issue 4, 2008, Pages 421-434

  Krienitz, M S ^a   Trumbull, R B ^a   Hellmann, A ^b   Kolb, J ^c   Meyer, F M ^b   Wiedenbeck, M ^a  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^b RWTH AACHEN UNIVERSITY   (Germany)

^c GEOLOGICAL SURVEY OF DENMARK AND GREENLAND   (Denmark)

Author keywords

Boron isotopes; Dharwar craton; India; Orogenic gold deposits; Tourmaline

Indexed keywords

BIMODAL ASSOCIATION; BORON ISOTOPE; FLUID INCLUSION; GOLD; GOLD MINE; GREENSTONE BELT; HYDROTHERMAL DEPOSIT; HYDROTHERMAL FLUID; HYDROTHERMAL SYSTEM; I-TYPE ROCK; ISOTOPIC COMPOSITION; MINERALIZATION; SOURCE ROCK; TOURMALINE; VOLATILIZATION;

ASIA; DHARWAR CRATON; EURASIA; INDIA; SOUTH ASIA;

EID: 43049131064     PISSN: 00264598     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00126-007-0172-0     Document Type: Article

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