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Abstract:

Located in the Sierras Pampeanas (the broken-foreland of the Pampean flat slab segment in the southern Central Andes), the Cerro Tiporco volcanic field shows Neogene hydrothermal activity linked to migration of arc-magmatism into the foreland. Late Neogene deposits comprise epithermal vein systems emplaced in Precambrian—Early Palaeozoic igneous-metamorphic basement, Late Miocene sedimentary rocks and Early Pliocene volcaniclastic rocks. Mineralization consists of calcareous onyx, aragonite and calcite veins as well as travertine deposits. Onyx and aragonite occur as fill of low-displacement nearly vertical reverse-sinistral faults striking NW, and nearly horizontal dilatant fractures. The latter consist of load-removal induced fractures affecting the igneous-metamorphic rocks, as well as bedding planes in the Late Miocene sediments. The presence of veins recording multiple fracture episodes and crack-and-seal growth of veins suggests relatively low differential stress and supralithostatic fluid pressure, as well as cyclic changes in pore pressure and high mineral-deposition/fracture-opening ratio. These conditions support a mechanism of fault-valve behaviour during onyx and aragonite vein emplacement. The fault-valve mechanism involves fractures associated with impermeable barriers between environments with different fluid pressure. Faulting generated an appreciable directional permeability triggering fluid migration from the highest to the lowest pressure region, with subsequent deposition and sealing that started a new pressurization-faulting-sealing cycle. Late aragonite and calcite veins suggest a change in kinematics indicating the onset of tectonic-load conditions. © 2016 Elsevier Ltd

Registro:

Documento: Artículo
Título:A transient fault-valve mechanism operating in upper crustal level, Sierras Pampeanas, Argentina
Autor:Japas, M.S.; Urbina, N.E.; Sruoga, P.; Garro, J.M.; Ibañes, O.
Filiación:Departamento de Ciencias Geológicas, Instituto de Geociencias Básicas, Aplicadas y Ambientales (IGeBA, CONICET-UBA), Universidad de Buenos Aires, Pabellón II, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, C1428EHA, Argentina
Departamento de Geología, Universidad Nacional de San Luis, Ejército de los Andes 950, San Luis, provincia de San Luis D5700HHW, Argentina
CONICET-SEGEMAR (Servicio Geológico Minero Argentino), Parque Tecnológico Miguelete, Av. Gral. Paz 5445, Edifício 25, San Martín, provincia de Buenos Aires B1650WAB, Argentina
Palabras clave:Calcareous onyx; Crack and seal vein growth; Fault-valve behaviour; Sierra de San Luis; Sierras Pampeanas broken-foreland; Tertiary volcanic belt; aragonite; calcite; fault; tectonic setting; Tertiary; upper crust; vein (geology); volcanic belt; Argentina; San Luis; Sierra de San Luis [Sierras Pampeanas]; Sierras Pampeanas; Onyx
Año:2016
Volumen:101
Página de inicio:142
Página de fin:154
DOI: http://dx.doi.org/10.1016/j.jog.2016.06.004
Título revista:Journal of Geodynamics
Título revista abreviado:J. Geodyn.
ISSN:02643707
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02643707_v101_n_p142_Japas

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Citas:

---------- APA ----------
Japas, M.S., Urbina, N.E., Sruoga, P., Garro, J.M. & Ibañes, O. (2016) . A transient fault-valve mechanism operating in upper crustal level, Sierras Pampeanas, Argentina. Journal of Geodynamics, 101, 142-154.
http://dx.doi.org/10.1016/j.jog.2016.06.004
---------- CHICAGO ----------
Japas, M.S., Urbina, N.E., Sruoga, P., Garro, J.M., Ibañes, O. "A transient fault-valve mechanism operating in upper crustal level, Sierras Pampeanas, Argentina" . Journal of Geodynamics 101 (2016) : 142-154.
http://dx.doi.org/10.1016/j.jog.2016.06.004
---------- MLA ----------
Japas, M.S., Urbina, N.E., Sruoga, P., Garro, J.M., Ibañes, O. "A transient fault-valve mechanism operating in upper crustal level, Sierras Pampeanas, Argentina" . Journal of Geodynamics, vol. 101, 2016, pp. 142-154.
http://dx.doi.org/10.1016/j.jog.2016.06.004
---------- VANCOUVER ----------
Japas, M.S., Urbina, N.E., Sruoga, P., Garro, J.M., Ibañes, O. A transient fault-valve mechanism operating in upper crustal level, Sierras Pampeanas, Argentina. J. Geodyn. 2016;101:142-154.
http://dx.doi.org/10.1016/j.jog.2016.06.004