Dynamic sedimentology of orogenic belts is an important aspect for the research on continental dynamics and geology of orogenic belts.
造山带动力沉积学是造山带地质学和大陆动力学研究的重要方面。
Sedimentology plays an important role in the analysis of orogenic stratigraphy and lithofacies, but more attention should be paid to the close relation between sedimentology and tectonics.
沉积学在造山带地层和岩相分析中具巨大作用，应更多强调构造与沉积学的紧密结合。
The authors think that most of the stratigraphy of the orogenic belts can be recovered for the studies of sedimentology and lithofacies.
本文认为造山带绝大多数地层体可进行沉积学的恢复。
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