An evaporitic origin of the parent brines of Colombian emeralds; fluid inclusion and sulphur isotope evidence

Gaston Giuliani; Alain Cheilletz; Carlos Arboleda; Victor Carrillo; Felix Rueda; James H. Baker

Article navigation

Other| February 01, 1995

An evaporitic origin of the parent brines of Colombian emeralds; fluid inclusion and sulphur isotope evidence

Gaston Giuliani;

Gaston Giuliani

ORSTOM, Institut Francais de Recherche Scientifique pour le Developpement en Cooperation, Paris, France

Search for other works by this author on:

GSW

Google Scholar

Alain Cheilletz;

Alain Cheilletz

Search for other works by this author on:

GSW

Google Scholar

Carlos Arboleda;

Carlos Arboleda

Search for other works by this author on:

GSW

Google Scholar

Victor Carrillo;

Victor Carrillo

Search for other works by this author on:

GSW

Google Scholar

Felix Rueda;

Felix Rueda

Search for other works by this author on:

GSW

Google Scholar

James H. Baker

Search for other works by this author on:

GSW

Google Scholar

Author and Article Information

Gaston Giuliani

ORSTOM, Institut Francais de Recherche Scientifique pour le Developpement en Cooperation, Paris, France

Alain Cheilletz

Carlos Arboleda

Victor Carrillo

Felix Rueda

James H. Baker

Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie

First Online: 02 Mar 2017

Online ISSN: 1617-4011

Print ISSN: 0935-1221

European Journal of Mineralogy (1995) 7 (1): 151–165.

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

You could not be signed in. Please check your email address / username and password and try again.

Shibboleth Sign In

OpenAthens Sign In

Institutional Sign In

An evaporitic origin of the parent brines of Colombian emeralds; fluid inclusion and sulphur isotope evidence

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

An evaporitic origin of the parent brines of Colombian emeralds; fluid inclusion and sulphur isotope evidence

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

This Feature Is Available To Subscribers Only