分析造山带中盆地系的板块构造时，需要将靠近作用与分离作用仔细区分开来。
Plate tectonic analysis of basin systems interspersed in orogenic belts requires that the effects of approximation be carefully distinguished from those of separation.
这种地槽的形成与造山作用的循环可以以一种简单和自然的方式与板块构造的海洋开合理论结合起来。
The cycle of geosyncline formation and orogeny can be integrated with the plate tectonics concept of opening and closing oceans in a simple and natural way.
这些证据为华南的三叠纪造山作用和构造演化模式提供了强有力的支持。
These evidences provide forceful support for tectonic interpretation of the Triassic orogeny and the tectonic evolution model in South China.
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