西伯利亚、塔里木及哈萨克斯坦诸古板块中的微陆和地体构成了中亚十分复杂的拼贴构造（ｃｏｌｌａｇｅｔｅｃｔｏｎｉｃｓ）图案。古生代时，南天巴准洋一阿萨伊锡弧沟弧系和额尔齐斯洋一成田弧沟弧系构成了哈萨克斯坦板块的原型。塔里木板块陆壳块体在泥盆纪相对于阿萨伊锡岛弧的左行低角度斜俯冲和碰撞，造成此弧的解体、走滑堆叠和山弯构造。与此同时，成田岛弧南北两侧分别受到南天巴准洋和额尔齐斯洋的俯冲。在晚古生代晚期这两个沟弧系演变为哈萨克斯坦板块的基本构造单元。 The micro-continents and terraces in the Siberia, Tarim and Kazakhstan plates make up the very complex collage pattern in Central Asia. During the Paleozoic, the Nantianbaoyan-Assyrian tin arc ditch arc system and the Irtysh oceanic-arc ditch arc system formed the prototype of the Kazakhstan plate. The Tarim block continental crust diagonally subducted and collided at a low angle to the left of Devonian relative to the Aksai Island arc, resulting in the disintegration of this arc, the strike-slip stacking and the mountain bend. At the same time, both sides of the Narita Island arc are respectively subducted by the Quaternary Nanyanti Paleozoic and the Irtysh Ocean. In the late Late Paleozoic these two arc-arc systems evolved into the basic tectonic units of the Kazakhstan plate.