Accretionary prisms of the Sikhote-Alin Orogenic Belt: Composition, structure and significance for reconstruction of the geodynamic evolution of the eastern Asian margin

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• 作者：I.V. Kemkin^a ; ^b ; ^{kemkin@fegi.ru} ; A.I. Khanchuk^a ; ^b ; R.A. Kemkina^a ; ^b
• 刊名：Journal of Geodynamics
• 出版年：2016
• 出版时间：December 2016
• 年：2016
• 卷：102
• 期：Complete
• 页码：202-230
• 全文大小：18045 K
• 卷排序：102

文摘

Accretionary prisms carry information about the succession of the geological events that took place at the convergent boundaries. Composition and structure of the Sikhote-Alin prisms are useful tools for the reconstruction of the stepwise geological history. The formation of the Sikhote-Alin orogenic belt includes two stages. First – accretion of the oceanic fragments due to the subduction of the paleo-Pacific plate. Second – subsequent intense deformation of the rocks under conditions of the transform continental margin.