Fluid inclusion and stable isotope (O, H, C) constraints on the genesis of the Pedra Branca gold deposit, Troia Massif, Borborema Province, NE Brazil: An example of hypozonal orogenic gold mineralization

Author:

Grandjean da Costa Felipe,Luiz Klein Evandro,Harris ChrisORCID,Roopnarain Sherissa

Funder

CNPq

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference215 articles.

1. The paleoproterozoic NICO iron-oxide-cobalt-gold-bismuth deposit, Northwest Territories, Canada: evidence from isotope geochemistry and fluid inclusions;Acosta-Góngora;Precambr. Res.,2015

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3. Geologia, geoquímica e geocronologia da suíte intrusiva máfica–ultramáfica de Boa Viagem, Ceará, Brasil;Almeida,2014

4. Fluid mixing in the generation of isothermal gold mineralization in the Transvaal Sequence, Transvaal, South Africa;Anderson;Eur. J. Mineral.,1992

5. Cromititos do Complexo de Pedra Branca: química mineral e platinóides associados, Ceará, Brasil;Angeli,2009

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