摘要
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。
In Fujian Province, there were intensive uplift and extension movements in the Indosinian epoch, the geological evidences of which have met with more and more geologist's recognition. The paper focuses on the discussion of the Indosinian Movement's characters from the uplift epeirogenic movement and the folding orogenic movement. It is considered that during the Indosinian Movement the characteristics of the folding orogenic movement in Fujian Province are unconspicuous and the characteristics of the uplift epeirogenic movement are obvious.
出处
《福建地质》
2001年第2期87-90,共4页
Geology of Fujian
