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Boletín de la Sociedad Geológica Mexicana Volumen 72, núm. 3, A090720, 2020 |
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New mineralogical data on platinum-group minerals from the Río Santiago alluvial placer, Esmeraldas province, Ecuador
Nuevos datos mineralógicos de los minerales del grupo del platino en los placeres aluviales del
Río Santiago, provincia de Esmeraldas, Ecuador
Gladys G. López-Males1, Thomas Aiglsperger2,*, Núria Pujol-Solà1, Joaquín A. Proenza1
1 Department de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona (UB), Martí i Franquès s/n, 08028, Barcelona, Spain.
2 Luleå University of Technology, Department of Civil Engineering and Natural Resources, Division of Geosciences and Environmental Engineering, SE 97187, Luleå, Sweden.
* Corresponding author: (T. Aiglsperger) This email address is being protected from spambots. You need JavaScript enabled to view it.
How to cite this article:
López-Males, G.G., Aiglsperger, T., Pujol-Solà, N., Proenza, J.A., 2020, New mineralogical data on platinum-group minerals from the Río Santiago alluvial placer, Esmeraldas province, Ecuador: Boletín de la Sociedad Geológica Mexicana, 72 (3), A090720. http://dx.doi.org/10.18268/BSGM2020v72n3a090720
Abstract
Mineralogical studies on platinum-group minerals found in placer deposits from the Río Santiago (Ecuador) are scarce. In this investigation, one sample collected from the Río Santiago alluvial placer was studied via a multi-disciplinary approach, including optical microscopy, scanning electron microscopy, electron microprobe, and Raman spectroscopy. Whole-rock geochemistry data of the sample confirms elevated Au and platinum-group elements contents and the chondrite-normalized pattern reveals pronounced positive Ir and Pt anomalies. Free grains of platinum-group minerals were separated via hydroseparation techniques and identified as: i) Pt-Fe alloy (Pt3Fe), ii) tulameenite (Pt2FeCu) and iii) hongshiite (PtCu). The most abundant platinum-group mineral is Pt-Fe alloy (85%) that occasionally hosts cuprorhodsite (CuRh2S4) inclusions. Although the primary source remains unknown, the geochemical and mineralogical data suggests that the source of platinum-group minerals in the Río Santiago alluvial placer is a mafic-ultramafic Ural-Alaska type complex. Possible primary sources are the mafic and ultramafic rocks found in the mafic basement of the coastal region and the Western Cordillera (Piñón, San Juan and Pallatanga units), which derive from the Late Cretaceous Caribbean Colombia Oceanic Plateau (CCOP).
Keywords: Pt-Fe alloy, Ecuador, PGM, placer deposit, Río Santiago.
