Artigo Revisado por pares

The Paleoclimatic Signatures of Supergene Metal Deposits

2015; Mineralogical Society of America; Volume: 11; Issue: 5 Linguagem: Inglês

10.2113/gselements.11.5.317

ISSN

1811-5217

Autores

Paulo Vasconcelos, Martín Reich, David L. Shuster,

Tópico(s)

Geochemistry and Geologic Mapping

Resumo

Research Article| October 01, 2015 The Paleoclimatic Signatures of Supergene Metal Deposits Paulo M. Vasconcelos; Paulo M. Vasconcelos 1School of Earth Sciences, The University of QueenslandBrisbane, QLD 4072, AustraliaE-mail: p.vasconcelos@uq.edu.au Search for other works by this author on: GSW Google Scholar Martin Reich; Martin Reich 2Department of Geology, FCFM, Universidad de ChilePlaza Ercilla 803, Santiago, ChileE-mail: mreich@ing.uchile.cl3Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Santiago, Chile Search for other works by this author on: GSW Google Scholar David L. Shuster David L. Shuster 4Department of Earth and Planetary Science, University of California, Berkeley, CA 94720-4767, USAE-mail: dshuster@berkeley.edu5Berkeley Geochronology Center2455 Ridge Road, Berkeley, CA 94709, USA Search for other works by this author on: GSW Google Scholar Author and Article Information Paulo M. Vasconcelos 1School of Earth Sciences, The University of QueenslandBrisbane, QLD 4072, AustraliaE-mail: p.vasconcelos@uq.edu.au Martin Reich 2Department of Geology, FCFM, Universidad de ChilePlaza Ercilla 803, Santiago, ChileE-mail: mreich@ing.uchile.cl3Andean Geothermal Center of Excellence (CEGA), FCFM, Universidad de Chile, Santiago, Chile David L. Shuster 4Department of Earth and Planetary Science, University of California, Berkeley, CA 94720-4767, USAE-mail: dshuster@berkeley.edu5Berkeley Geochronology Center2455 Ridge Road, Berkeley, CA 94709, USA Publisher: Mineralogical Society of America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print ISSN: 1811-5209 © 2015 by the Mineralogical Society of America Elements (2015) 11 (5): 317–322. https://doi.org/10.2113/gselements.11.5.317 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Paulo M. Vasconcelos, Martin Reich, David L. Shuster; The Paleoclimatic Signatures of Supergene Metal Deposits. Elements 2015;; 11 (5): 317–322. doi: https://doi.org/10.2113/gselements.11.5.317 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyElements Search Advanced Search Abstract Supergene metal deposits host a comprehensive record of climate-driven geochemical reactions that may span the entire Cenozoic. Products of these reactions can be dated by a variety of radiogenic isotopic methods, such as 40Ar/39Ar, (U–Th)/He, U–Pb, and U-series. The frequency of mineral precipitation, determined by dating a representative number of samples of a particular mineral collected from distinct parts of the supergene ore body, reflects times in the geological past when weathering conditions were conducive to water–rock interaction. The frequency of mineral precipitation through time permits identifying periods in the geological past when climatic conditions were most conducive to chemical weathering and supergene ore genesis. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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