Journal
JOURNAL OF GEOGRAPHY-CHIGAKU ZASSHI
Volume 119, Issue 6, Pages 1173-1196Publisher
TOKYO GEOGRAPHICAL SOC
DOI: 10.5026/jgeography.119.1173
Keywords
tectonic erosion; serpentinite melange; accretionary complex; continental crust; Pacific-type orogeny
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The Japanese Islands have long been considered to be the most evolved of all the island arcs in the oceans. A simple scenario has been implicitly accepted for the growth of the Japanese Islands: since subduction started sometime around 520 Ma, the TTG crust has increased over time in association with the steady-state growth of the accretionary prism in front. Here, we show very different dynamic growths of TTG crusts over time than previously thought, i.e., four times more TTG crusts than at present must have gone into the deep mantle due to tectonic erosion, which occurred six times since subduction was initiated at 520 Ma. Tectonic erosion is a major process that has controlled the development history of the Japanese islands. It can be traced as a serpentinite melange belt, which indicates the upper boundary of past extensive tectonic erosion.
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