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This study area consists of fold-and-thrust fault belts, distributed in the back arc in northeast Japan.
The oblique nature of the collision provides a way to quantify the spatial and temporal distribution of strain from the deformation front to the back arc.
Ar Ar and U Pb ages constrain the back arc volcanism to have evolved between 163.9 ± 1.4 and 148.9 ± 1.2 Ma.
Results suggest that a possible rotation of stress direction from N40E-S40W to N-S occurred during the post-Miocene history of the Java back arc tectonic evolution.
Aeromagnetic data suggests that this basin may be imposed on a Ross age back arc region adjacent to the East Antarctic Craton.
and continued serpentine breakdown contributes to the Cl enrichment of back arc basin basalts (Kendrick et al., 2011).
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A back-arc basin is formed by the process of back-arc spreading, which begins when one tectonic plate subducts under (underthrusts) another.
Back-arc basin, submarine basin that forms behind an island arc.
They are also found in volcanic "back-arc" basins behind ocean trenches, where one tectonic plate is sliding beneath another.
(Spreading centres that form in back-arc basins are much shorter than those found along oceanic ridges, however).
There are two kinematic models of back-arc opening.
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