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地球学报  2002 

阿尔金断裂:几何学、性质和生长方式

Keywords: 阿尔金断裂,逆冲序列,扩展,左行走滑,生长方式

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Abstract:

阿尔金断裂具有线性与弧形相叠加的几何学特征及强烈的时空不均一性,阿尔金断裂是一条同时具有逆冲、左行走滑和正滑复杂力学性质的巨型断裂系。走滑作用和正滑作用的主要时期分别为白垩纪-新生代和上新世一第四纪,逆冲作用则是晚古生代以来一直起主导作用的变形事件(大约305Ma以来)。阿尔金断裂的形成与其两侧地块的强烈不均一变形(阿尔金山腹地以收缩变形为主,祁连地块以逆冲扩展为主)有关,它经历了分段破裂、逐段连接和逐渐扩展的动力学过程,其形成与祁连地块中的上叠式逆冲序列和青藏高原隆升同步,随着自南而北逆冲扩展和青藏高原

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