Pervasive crustal reworking along the proto-Andean margin of northern Peru and southern Ecuador: Insights from U-Pb, geochemical, and isotopic analyses of zircon
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引用次数: 0
Abstract
Continental growth at convergent margins is the result of complex interactions between mantle additions and crustal reworking. This study examines the pre-Andean tectono-magmatic evolution of the central-northern Andean margin (∼1°S to ∼6°S) using U-Pb geochronology, trace element analysis, and εHf(t) and δ18O isotopic data from zircons embedded within detrital and bedrock samples. U-Pb dating revealed two primary clusters: a Late Neoproterozoic population (640–550 Ma) associated with the Brasiliano/Pan-African orogeny and a Permian–Triassic population (280–200 Ma) associated with the Gondwanides orogeny. There were also two minor clusters at ∼960 Ma and ∼345 Ma. Zircon grains dating between 1000 and 200 Ma crystallized during repeated episodes of crustal reworking, characterized by highly evolved εHf(t) signatures (−10 to −30) at 640–510 Ma that are indicative of ancient Amazonian cratonic sources, with no evidence of Pampean or Famatinian contributions. The results also show a marked increase in juvenile input during the Carboniferous (380–310 Ma), followed by predominantly continental input as indicated by persistently high δ18O values up to 220 Ma. Although the U-Pb age spectra of these samples are similar to that of the central Andes, isotopic and geochemical data reveal that the central-northern Andean margin evolved within a tectonic context that is more closely aligned with central-eastern Gondwana (i.e., central Africa and eastern South America) rather than typical Andean settings.
期刊介绍:
Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields:
-Economic geology, metallogenesis and hydrocarbon genesis and reservoirs.
-Geophysics, geochemistry, volcanology, igneous and metamorphic petrology.
-Tectonics, neo- and seismotectonics and geodynamic modeling.
-Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research.
-Stratigraphy, sedimentology, structure and basin evolution.
-Paleontology, paleoecology, paleoclimatology and Quaternary geology.
New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.