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福建印支期强烈的抬升和伸展现象的地质事实已为广大地质工作者所公认。从抬升造陆作用、褶皱造山作用两方面探讨了印支运动的性质 ,认为印支运动的褶皱造山特征不明显 ,而隆升造陆特征显著。
The geological fact of the strong uplift and extension of Indosinian in Fujian Province has been recognized by the majority of geological workers. From the aspects of uplift and foreland formation and fold orogeny, the nature of Indosinian movement is discussed. The characteristics of fold orogen in Indosinian movement are not obvious, and the characteristics of uplift and land-making are significant.