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Título
Morphological and compositional analysis of alluvial gold: The Fresnedoso gold placer (Spain)
Autor(es)
Palabras clave
Gold placer
Orogenic gold deposits
Morphological analysis
Laterite
Moraleja Cenozoic basin
Iberian Massif
Fecha de publicación
2020
Editor
ELSEVIER
Citación
Kelvin dos Santos Alves, Santos Barrios Sánchez, Juan Gómez Barreiro, Raúl Merinero Palomares, José Manuel Compaña Prieto, Morphological and compositional analysis of alluvial gold: The Fresnedoso gold placer (Spain), Ore Geology Reviews, Volume 121, 2020, 103489, ISSN 0169-1368, https://doi.org/10.1016/j.oregeorev.2020.103489. (https://www.sciencedirect.com/science/article/pii/S0169136820300184)
Resumen
[EN]The Fresnedoso creek gold placer (FGP) in the Moraleja Basin (W Iberian Massif) has been investigated in terms
of morphological, textural and compositional evolution of gold particles. A mixture of two populations has been
identified being coherent with primary sources located at a proximal (2.5–10 km), and distal (20–50 km) range.
Shape and compositional evidences suggest recycling of paleoplacers (tertiary) has to be considered to some
extend. Primary laminar morphologies point to lode deposits in small-flat veins hosted in the metasediments of
the Schist Greywacke Complex. All these features suggest the Fresnedoso creek gold placer is a deposit constituted
by with mono- and polycyclic particles. Transport distance – Flattening indexes (CFI, Shilo) models have
been tested and result in useful information for exploration of undiscovered deposits, even with a limited dataset.
Compositional analysis of gold particle morphotypes has revealed that the Fresnedoso gold is a AuAg
bimetallic alloy. Textural and compositional groups include: type 1 (Au1 = Au88-94Ag12-6), type 2 (Au2 = Au99
Ag1) and type 3 (Au3 ~ Au99Ag1). Variations in composition of type 1 (Particle's cores) could reflect differences
in primary composition, spatial dispersion of sources or secondary processes, but fit within the compositional
range of orogenic gold deposits. Secondary processes have been explored to explain compositional heterogeneity
in the particles. Gold type 2 (rim) and 3 (micro-aggregates) represents two different de-alloying stages, from
initial Ag-leaching at the rim and/or through grain-boundaries and microfractures (Au2), to complete resetting
of primary chemical imprint, pervasive porous texture and Au re-precipitation with Fe-OOH and clays (Au3). A
model is proposed which combines: Ag de-alloying enhanced in a Cl-Fe rich environment (lateritic) and the
deformation/recrystallization processes related to mechanical cold-work in the river load-bed during transport.
URI
ISSN
0169-1368
DOI
10.1016/j.oregeorev.2020.103489
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