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- W2562729250 abstract "Cordilleran orogenic belts are formed primarily by processes associated with the subduction of oceanic plates beneath the edges of continental plates. On Earth today, the American Cordilleras, spanning one-third the circumference of the globe, represent the range of variations seen in older, less coherent cordilleran belts. The Alpine-Himalayan-New Guinean orogenic belt embodies Earth’s other great orogenic system and has formed by both collisional and cordilleran-style processes. Because of the abundance of oceanic lithosphere on this planet, it stands to reason that cordilleran-style orogenesis has been important throughout the portion of geological time during which plate tectonics has operated.Inasmuch as continental magmatic arcs lie at the heart of most cordilleran orogenic belts, their long-term (107–108 yr) behavior must be intimately tied to the diverse processes that collaborate with magmatism to build these great orogenic belts. Thus, changes in magma production through time, as recorded by cordilleran batholiths and volcanic piles, have implications for the broad web of tectonic, magmatic, metamorphic, mantle dynamic, and surface processes operating in cordilleran orogenic systems, as well as potential global climatic effects (McKenzie et al. 2016). For this reason sundry geoscientists, including petrologists, geophysicists, basin analysts, structural geologists, geomorphologists, geochronologists, and even climatologists, are paying unprecedented attention to the histories of cordilleran …" @default.
- W2562729250 created "2017-01-06" @default.
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- W2562729250 date "2017-01-01" @default.
- W2562729250 modified "2023-09-27" @default.
- W2562729250 title "Periodic activity in continental magmatic arcs" @default.
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- W2562729250 doi "https://doi.org/10.2138/am-2017-5908" @default.
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