Therefore, this paper thought that Mazha-Kangxiwa-Subashi suture zone experienced Sinian to Early Silurian evolvement of Proto-Tethys and Devonian to Early Triassic evolution of the Palaeo-Tethys ;
由此本文认为麻扎-康西瓦-苏巴什结合带经历了震旦-早志留世的原特提斯洋的演化和中泥盆世-早三叠世的古特提斯洋的演化；
The MIFA, as a fractal geometry method, is used to study the Silurian reservoir of Tazhong area in this paper.
MIFA法就是一种定量的分形几何学方法。 本文应用MIFA法对塔里木盆地塔中地区志留系储层孔隙结构进行了研究。
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