U–Pb SHRIMP detrital zircon dating of metamorphic rocks in north–central Chile (28°–33°S): Evidence for Carboniferous and Triassic metamorphism in a subduction setting
Author
dc.contributor.author
Hervé Allamand, Francisco
Author
dc.contributor.author
Calderón, M.
Author
dc.contributor.author
Fanning, C. M.
Author
dc.contributor.author
Pankhurst, R. J.
Author
dc.contributor.author
Navarro, J.
Admission date
dc.date.accessioned
2021-01-25T13:19:21Z
Available date
dc.date.available
2021-01-25T13:19:21Z
Publication date
dc.date.issued
2020
Cita de ítem
dc.identifier.citation
Journal of South American Earth Sciences 103 (2020) 102767
es_ES
Identifier
dc.identifier.other
10.1016/j.jsames.2020.102767
Identifier
dc.identifier.uri
https://repositorio.uchile.cl/handle/2250/178306
Abstract
dc.description.abstract
U-Pb SHRIMP detrital zircon dating of ten samples of metamorphic "basement" rocks in north-central Chile and one granitic rock, improve knowledge of sedimentary, metamorphic and plutonic events in this segment of the Andean margin. The oldest possible sedimentation ages (Ordovician) come from a micaschist at Huentelauquen (477 Ma) and a granofels from a migmatite at Las Cruces (470 Ma) whose garnet-bearing granitic neosome (ca. 320 Ma) is essentially coetaneous with the extensive Coast Range Batholith. The rest of the samples show probable Carboniferous or Late Triassic maximum depositional ages. The late Paleozoic low-to-medium grade metasedimentary components of the basement, interpreted as forming part of a paleo-accretionary complex, have detrital zircon age patterns with prominent Famatinian and Grenville-age peaks; these are much less prominent in the Late Triassic rocks. The latter were deformed and metamorphosed shortly after their deposition, although some do not show visible evidence of metamorphism. Contemporaneous Triassic sedimentary, metamorphic and igneous events are recorded in Mejillones Peninsula (22 degrees S) and in the Chonos archipelago (44 degrees-47 degrees S) but not in the 34 degrees-42 degrees S central Chile sector of the fossil accretionary complex. These events predate generalized Jurassic subduction beneath the western Gondwana continental margin that initiated the Andean orogenic cycle.
es_ES
Patrocinador
dc.description.sponsorship
Comisión Nacional de Investigación Científica y Tecnológica (CONICYT)
CONICYT FONDECYT
1130227
1180457
1161818
U–Pb SHRIMP detrital zircon dating of metamorphic rocks in north–central Chile (28°–33°S): Evidence for Carboniferous and Triassic metamorphism in a subduction setting