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近几年来,黄汲清一直依照传统的旋迴对比法,强调用不整合及其反映的地壳运动期(即他所称的“旋迴”),并只限于“寒武纪以来地槽地带的”所谓“造山”运动旋迴,来划分大地构造区域和研究地壳发展规律。黄汲清认为,地壳运动的多期性(即黄的“多旋迴性”)是中国所特有的,而且特别强调是在—些不正常的、不合标准的、特殊的构造单元,即所谓“准地台”和所谓“准地槽”所专有的特征。
In recent years, Huang Ch’ing-ch’ing has always followed the conventional cycle-contrast method, emphasizing unconformity and the period of crustal movement it reflects (what he calls the “cycle”), and is limited to “the period of the Cambrian The so-called ”orogenic“ movement cycle, to divide the tectonic area and study the laws of crustal development. Huang Jiqing believes that the multiplicity of crustal movements (ie, the ”multi-cycle“ of yellowness) is peculiar to China, with a particular emphasis on - unusual, sub-standard and special tectonic units, so-called ”Quasi-platform“ and the so-called ”quasi-terrain groove" by the proprietary features.