The Banda Arc Collision Zone: Subduction Geometry Driving Island Arc Volcanism and Microplate Rotation
班达弧碰撞带：俯冲几何形态驱动岛弧火山活动与微板块旋转
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The Banda Arc in eastern Indonesia results from complex collision between the Indo-Australian Plate and Eurasian margins.
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Unlike linear subduction zones, its curved geometry forces microplates like Timor and Seram to rotate independently.
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