Crustal dense blocks in the fore-arc and arc region of Chilean ranges and their role in the magma ascent and composition: Breaking paradigms in the Andean metallogeny

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dc.contributor.authorYanez Carrizo, Gonzalo
dc.contributor.authorRivera Herrera, Orlando
dc.date.accessioned2025-01-23T21:12:19Z
dc.date.available2025-01-23T21:12:19Z
dc.date.issued2019
dc.description.abstractWe use Intermediate-to-short wavelength (20-150 km) gravity anomalies to investigate the role played by crustal scale dense blocks in the genesis of Cu ore deposits along the Andes. These dense blocks are widespread along the margin and located at the fore-arc, arc, and back-arc domains, including depths in the range of 12-18 km, and thickness of 5-8 km. The interplay of these dense blocks with long-lived Trans-Lithospheric-Faults (TLF) controls the emplacement, and most likely, provides the required fertile fluids for the Cu ore genesis. Dense blocks represent impervious crustal domains, surrounded by damage zones at the intersection with TLF systems. Concentration of seismicity, large Vp/Vs ratios, low gravity domains, active volcanism, and structural fabric, demonstrate that these damage zones are in fact the most likely places for magma as well as mineralized flow ascent and emplacement. Basic flow models in porous media show a flow path that migrates horizontally at the base of dense/impervious blocks until the high permeability edge flanks, where pressure gradients provide the ideal conditions for the upward and focusing hydrothermal fluid ascent. Although not fully addressed in this paper, evidence suggests that the interaction of subducting-related fluids and the mafic-dense block might produce a fertile fluid with a concentration of Cu.
dc.description.abstractIn contrast with the long-standing view of metallogenic belts of the same age and parallel to the trench axis, we propose a multi-age metallogenic cluster, along the periphery of dense blocks, and organized oblique to the margin, following the trend of a given TLF.
dc.fuente.origenWOS
dc.identifier.doi10.1016/j.jsames.2019.04.006
dc.identifier.issn0895-9811
dc.identifier.urihttps://doi.org/10.1016/j.jsames.2019.04.006
dc.identifier.urihttps://repositorio.uc.cl/handle/11534/100952
dc.identifier.wosidWOS:000472124000005
dc.language.isoen
dc.pagina.final66
dc.pagina.inicio51
dc.revistaJournal of south american earth sciences
dc.rightsacceso restringido
dc.subject.ods13 Climate Action
dc.subject.odspa13 Acción por el clima
dc.titleCrustal dense blocks in the fore-arc and arc region of Chilean ranges and their role in the magma ascent and composition: Breaking paradigms in the Andean metallogeny
dc.typeartículo
dc.volumen93
sipa.indexWOS
sipa.trazabilidadWOS;2025-01-12
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