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王汉卿撰写《中国纬向带褶皱构造研究》的思路,始于阅读“东西复杂构造带和南北构造带”(李四光,1959)一文。作者于20世纪60年代至80年代分别在南岭和西秦岭地区从事构造体系、地质矿产资源的调查研究工作,通过阅览多幅1∶20万地质图和野外观察、综合研究,于1984年夏—秋将西秦岭地区澄江、晚加里东、海西、印支期4期以海相沉积地层为主的褶皱构造,按其延伸方向、形态特征、排列方式分析对比,发现具有“隔期相似,邻(原著为临,下同——编者注)期相异”的特征。
Wang Han-qing’s thought of writing a study on the zonal fold structure in China started with a reading of “The East-West Complex Tectonic Belt and the North-South Structural Belt” (Li Siguang, 1959). In the 1960s and the 1980s, he worked in the investigation of tectonic systems and geological mineral resources in the Nanling and West Qinling areas respectively. After reading a series of 1: 200,000 geological maps and field observations and comprehensive studies, - Qiujiang fold sedimentary facies of the Chengjiang, Late Caledonian, Hercynian and Indosinian phases in the western Qinling area were analyzed and compared according to their extensional direction, morphological characteristics and arrangement, and they were found to be similar , The adjacent (original Pro, the same below - Editor’s Note) different periods "feature.