Spatially and Geochemically Anomalous Arc Magmatism: Insights From the Andean Arc

نویسندگان

چکیده

While most volcanic arcs show a distinctive spatial relationship to subducting plates, there are many examples where volcanoes occur in anomalous locations. These commonly also geochemically relative the composition of more typical subduction-related rocks. Using Holocene South America as case study, we document and geochemical patterns along Andean belt. To determine whether variations anomalous, assess series indices that provide information on depth degree melting, role metasomatic subduction inputs melt generation. We use these parameters develop scoring system, with lowest highest scores indicating “typical” “anomalous” arc melting processes, respectively. Typical magmatism is defined melts generated sub-arc mantle wedge through slab-derived fluid metasomatism, or without contributions from subducted sediments. In contrast, volcanism appears relate geometric anomalies Nazca plate (e.g., beneath Sumaco, Laguna Blanca Payun Matru), areas affected by flow due proximity slab edge (Crater Basalt Volcanic Field). By establishing relationships between structure, propose similar fingerprints could be used explore magmatic response deformation and/or tearing older systems, particularly cases three-dimensional structure no longer detectable.

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ژورنال

عنوان ژورنال: Geochemistry Geophysics Geosystems

سال: 2021

ISSN: ['1525-2027']

DOI: https://doi.org/10.1029/2021gc009688