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The origin of Cu/Au ratios in porphyry-type ore deposits

Author
HALTER, Werner E1 ; PETTKE, Thomas1 ; HEINRICH, Christoph A1
[1] Isotope Geochemistry and Mineral Resources, Department of Earth Sciences, Swiss Federal Institute of Technology (ETH), ETH Zentrum NO, 8092 Zürich, Switzerland
Source

Science (Washington, D.C.). 2002, Vol 296, Num 5574, pp 1844-1846 ; Illustration ; ref : 24 ref

CODEN
SCIEAS
ISSN
0036-8075
Scientific domain
Multidisciplinary
Publisher
American Association for the Advancement of Science, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Analyse chimique Chambre magmatique Circulation hydrothermale Cuivre Exsolution Fer Gîte hydrothermal Inclusion Minéralisation Or Phase fluide Plasma couplé inductivement Porphyry copper Silicate Spectrométrie masse Sulfure Spectrométrie ICP
Keyword (en)
chemical analysis magma chambers hydrothermal circulation copper exsolution iron hydrothermal deposits inclusions mineralization gold fluid phase inductively coupled plasma porphyry copper silicates mass spectroscopy sulfides
Keyword (es)
Análisis químico Cámara magmática Cobre Exsolución Hierro Inclusión Mineralización Oro Fase fluida Cobre porfídico Silicato Espectrometría masa Sulfuro
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01B Geochemistry / 001E01B03 Soil and rock geochemistry

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01E Metallic and non-metallic deposits / 001E01E02 Metal geology

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
13713301

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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