Time Markers for the Evolution and Exhumation History of a Late Palaeozoic Paired Metamorphic Belt in North-Central Chile (34°-35°30'S)

6533b86efe1ef96bd12cb543

RESEARCH PRODUCT

Time Markers for the Evolution and Exhumation History of a Late Palaeozoic Paired Metamorphic Belt in North-Central Chile (34°-35°30'S)

Stuart N. Thomson Stuart N. Thomson Jan R. Wijbrans Jo-anne Wartho Francisco Hervé Alfred Kröner Arne P. Willner

subject

Series (stratigraphy)Accretionary wedge Paleozoic North central Metamorphic rock /dk/atira/pure/sustainabledevelopmentgoals/life_below_water Paleontology Geophysics Geochemistry and Petrology Oceanic crust Foliation (geology)SDG 14 - Life Below Water Accretion (geology)Geology

description

A multi-method geochronological approach is applied to unravel the dynamics of a paired metamorphic belt in the Coastal Cordillera of central Chile. This is represented by high-pressure - low-temperature rocks of an accretionary prism (Western Series), and a low-pressure- high-temperature overprint in the retro-wedge with less deformed metagreywackes (Eastern Series) intruded by magmas of the coeval arc. A pervasive transposition foliation formed in metagreywackes and interlayered oceanic crust of the Western Series during basal accretion near metamorphic peak conditions (∼350-400°C, 7-11 kbar) at 292-319 Ma (

year	journal	country	edition	language
2005-04-22	Journal of Petrology

10.1093/petrology/egi036 https://doi.org/10.1093/petrology/egi036

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