我们的模式基于古地磁数据.古地磁研究使我们得以恢复古构造,进行岩相分析和构造动力学的详细研究.对于中亚地区依据其古生代时期历史演化的状况,我们分辨出下列地区(自北而南)哈萨克斯坦陆块,又可分成几个区带:吉尔吉斯—捷尔斯克伊、恰特卡尔—纳伦、桑开尔—阿苏吐鲁克、恰特卡尔和库拉明斯克,古土耳其斯坦大洋构造,分三个带:土耳其斯坦—阿赖、查拉夫善—土耳其斯坦和查拉夫善—吉萨尔,以及乌斯吐尔特—塔里木古陆,内有此古陆的中古生代南吉萨尔裂谷带. Our model is based on paleomagnetic data, and paleomagnetic studies allowed us to restore paleontology, conduct detailed studies of facies analysis and tectonic dynamics, and for Central Asia, based on historical evolution of the Paleozoic period, we discern the following regions (from North and South) Kazakhstan land block can be divided into several zones: Kyrgyz-Tezkay, Chakkar-Naryn, Sangkal-Azulu-Lukkhan, Chakkar and Kuraminsk, The ancient Turkestan oceans are structured in three zones: Turkestan-Aray, Charafus-Turkestan, and Charafus-Gisar, and the Ustuart-Talimu, Paleozoic South Gesar Rift Valley.