Universidad de Granada Digibug

Repositorio Institucional de la Universidad de Granada >
1.-Investigación >
Departamentos, Grupos de Investigación e Institutos >
Departamento de Didáctica de Ciencias Experimentales >
DDCE - Artículos >

Please use this identifier to cite or link to this item: http://hdl.handle.net/10481/28429

Title: Extremely negative and inhomogeneous sulfur isotope signatures in Cretaceous Chilean manto-type Cu–(Ag) deposits, Coastal Range of central Chile
Authors: Carrillo-Rosúa, Javier
Boyce, Adrian J.
Morales-Ruano, Salvador
Morata, Diego
Roberts, Stephen
Munizaga, Francisco
Moreno-Rodríguez, Verónica
Issue Date: 13-Jul-2013
Abstract: Chilean manto-type (CMT) Cu(-Ag) hydrothermal deposits share a characteristic association of volcano-sedimentary Jurassic to Lower Cretaceous host rocks, style of mineralization, ore and associated mineralogy and geochemistry, with ore grades typically >1%Cu, that make this family of deposits significant and interesting, both academically and economically. Although often stratabound, geological evidence supports an epigenetic origin for these deposits. We present a detailed stable isotope study of La Serena and Melipilla-Naltahua Lower Cretaceous deposits, central Chile, which reveals extremely negative δ34S values, to -50‰, which are among the lowest values found in any ore deposit. In addition, the range of δ34S values from sulfides in the two areas is very wide: -38.3 to -6.9‰ in La Serena, and -50.4 to -0.6‰ in Melipilla-Naltahua. These new data significantly extended the reported range of δ34S data for CMT deposits. Co-existing sulfates range from 7.9 to 14.3‰, and are exclusive to La Serena deposit. The wide sulfide isotopic range occurs at deposit and hand specimen scale, and suggests a polygenic sulfur source for these deposits, where bacteriogenic sulfide dominates. While sulfur isotope data for the bulk of Jurassic CMT deposits, northern Chile, suggests a predominant magmatic source in their origin (mean = -2.7 ± 1.9‰, 1σ), contributions of a magmatic component is only likely to be involved at Melipilla-Naltahua deposit. The δ13C values obtained for calcites associated with the mineralization range from -20.1 to 0.2‰ also suggesting polygenic carbon sources, with the likely strong involvement of degradation of organic matter and leaching of limestone. Two different genetic models, with involvement of hydrocarbon, are proposed for both areas. For Melipilla-Naltahua, a two-step model can be developed as follows: 1) Framboidal pyrite growth, with very low δ34S, formed by bacterial sulfate reduction in an open system, and with diagenetic degradation of oil-related brines, leaving pyrobitumen. 2) Cu-bearing stage, replacing of framboidal pyrite, inheriting depleted sulfur as low as -50.4‰, together with sulfides directly precipitated from a hydrothermal fluid with δ34S close to 0‰. For La Serena, a single step model fits best, without framboidal pyrite generation. Cu-bearing sulfides were precipitated mainly in veins where Cu plus base metal-bearing hydrothermal fluids mixed with H2S generated by bacterial sulfate reduction in the host rocks. Isotopic evidence clearly illustrates that bacterial activity, perhaps enhanced by hydrothermal activity, was fed by hydrocarbon brines and sulfate remobilized from continental evaporites. It is possible that variable ecological conditions led to different extents of isotopic fractionation, adding to the typical sulfur isotopic heterogeneity of such bacterial systems. For both areas, the Cu-bearing stage occurred during the peak to waning stages of the very low-grade metamorphism that affected the Lower Cretaceous sequence.
Sponsorship: Departamento de Didáctica de las Ciencias Experimentales (Universidad de Granada)
Departamento de Mineralogía y Petrología (Universidad de Granada)
Instituto Andaluz de Ciencias de la Tierra (CSIC-Universidad de Granada)
Scottish Universities Environmental Research Centre, SUERC
Departamento de Geología, (Universidad de Chile)
Andean Geothermal Center of Excellence CEGA-FONDAP (Universidad de Chile)
School of Ocean and Earth Science, National Oceanography Centre (University of Southampton)
Publisher: Elsevier
Description: El artículo original ha sido publicado por Ore Geology Reviews, de la Editorial Elsevier, disponible en: http://www.sciencedirect.com/science/article/pii/S0169136813001443 El enlace vía DOI es: http://dx.doi.org/10.1016/j.oregeorev.2013.06.013
Keywords: Manto type deposits
Depósitos de tipo Manto
CMT deposits
Sulfur isotopes
Isótopos de azufre
Bacterial sulfate reduction
Sufato reducción bacteriana
Coastal Range
Cordillera de la costa
URI: http://hdl.handle.net/10481/28429
ISSN: 0169-1368
Rights : Creative Commons Attribution-NonCommercial-NoDerivs 3.0 License
Citation: Carrillo-Rosúa, J., Boyce, A. J., Morales-Ruano, S., Morata, D., Roberts, S., Munizaga, F., & Moreno-Rodríguez, V. (2014). Extremely negative and inhomogeneous sulfur isotope signatures in cretaceous chilean manto-type Cu–(Ag) deposits, Coastal Range of central Chile. Ore Geology Reviews, 56(0), 13-24. doi:http://dx.doi.org/10.1016/j.oregeorev.2013.06.013
Appears in Collections:DDCE - Artículos

Files in This Item:

File Description SizeFormat
Carrillo-Rosua_et_al_2014_Extremly_sulfur.pdf932.81 kBAdobe PDFView/Open
Recommend this item

This item is licensed under a Creative Commons License
Creative Commons

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.


Valid XHTML 1.0! OpenAire compliant DSpace Software Copyright © 2002-2007 MIT and Hewlett-Packard - Feedback

© Universidad de Granada