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板块构造学说的问世,使人们对若干地质现象有了新的认识,作为板块运动特征之一的混杂堆积,是大陆地质工作者需要十分重视的一个对象。 1972年9月李春昱在《试谈“板块构造”》一文中,曾提到西秦岭自甘肃临潭、合作向西到青海玛沁、花石峡一带,可能存在石炭、二迭、三迭系混杂堆积。这里通过目前掌握的有限资料,谈谈混杂堆积的概念以及对其地质意义的初步认识,同时介绍一个可能属于混杂堆积
The advent of plate tectonics has given people a new understanding of a number of geological phenomena. As one of the characteristics of plate tectonics, it is an object to which geologic workers in China need to attach great importance. In September 1972, Li Chunyu said in his article “Tectonic Tectonics” "Since the Qinling Range from Lintan, Gansu Province, westward to Maqin and Huashixiag area in Qinghai, there may be a mixture of Carboniferous, Permian and Triassic accumulation. Here by the limited information available at the moment, talk about the concept of mixed accumulation and its initial understanding of the geological significance, while introducing a may belong to the mixed accumulation