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A Review of the Bentong-Raub Suture vis-à-vis New Insight of the Tectonic Evolution of Malay Peninsula,South East Asia

引用

Acta Geologica Sinica(English Edition) 2016年第5期90卷 1865-1886页

作者： Aftab Alam KHAN Mustaffa Kamal SHUIB Department of Geology University of Malaya Department of Geology University of Dhaka

Genesis of the so-called Bentong-Raub Suture of Malay Peninsula does not fit to the model of subduction-related *** has evolved from transpression tectonics resulting closure and exhumation of the inland basin which underwent extensive back-arc extension during *** having similar thickness（average-35 km） below entire Malay Peninsula nagate collision of two separate continental blocks rather supports single continental block that collided with South China continental block during *** subduction of intervening sea（Proto South China Sea） below Malay Peninsula resulted in widespread I- and S-Type granitization and volcanism in the back-arc basins during *** occurrence of Permo-triassic Pahang volcanics of predominantly rhyolitic tuff suggest its derivation from back-arc ***-arc extension,basin development and sedimentation of the central belt of the peninsula continued until Cretaceous.A-Type granite of metaluminous to peraluminous character indicates their emplacement in an intraplate tectonic *** Peninsula suffered an anticlockwise rotation due to the rifting of Luconia-Dangerous Grounds from the east Asia in the Late Cretaceous-Early *** ductile and brittle deformation including crustal segmentation,pull-apart fracturing and faulting occurred during the closure and exhumation of the basins developed in the peninsula during Late Cretaceous-Early *** shortening in the central belt of the peninsula has been accomodated through strike-slip displacement,shearing and uplift.

关键词： Bentong-Raub fault intra-plate tectonics triassic back-arc extension Cretaceoustranspression Malay Peninsula

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