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• W2038654852 abstract "It is observed that active inter-arc basins are found only where the subducted plate can interact with the plate behind the trench. This condition exists where trenches are terminated or offset by transform faults or where large variations in subduction rates occur. Shear coupling between the two juxtaposed plates across a transform or strike-slip fault creates a tensional regime behind the island arc. Differential subduction velocities will couple the plate motions across both the more slowly subducting trench and across the intervening fracture zone. If the trench axis is assumed to move more slowly than a plate, inter-arc basin spreading may be initiated to conserve area." @default.
• W2038654852 created "2016-06-24" @default.
• W2038654852 creator A5070677278 @default.
• W2038654852 date "1978-05-01" @default.
• W2038654852 modified "2023-09-24" @default.
• W2038654852 title "Inter-arc basins: A kinematic model" @default.
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• W2038654852 doi "https://doi.org/10.1029/gl005i005p00325" @default.
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