The origins of orogenic belts and basins are two hot topics of current geoscience research.
造山带和盆地成因是当前地学研究的两个热点。
It has been generally considered that orogenic belts and basins are formed by different geodynamic mechanisms.
一般都认为造山带和盆地形成于不同的地球动力学环境。
The coupling relationships between sedimentary basins and orogenic belts refer to all of their interactions in their formation and evolution.
盘山系统形成演化过程中造山带和沉积盆地之间一切相互作用的总和即为盆山间的耦合关系。
The residual basins were deeply buried in Himalayan Period, and the Carboniferous System was piecemeal distributed in the depressed belts of orogenic zone.
喜山期残存盆地深埋，石炭系仅零星残存在造山带的低洼地带。
There is not only mosaic structures consisting of small blocks and giant orogenic belts, but also modern continental margin with trenchs, island arc and basins lasting for 20 000 km.
这里不仅有若干小地块与巍峨造山带形成的镶嵌组合，还有以沟、弧、盆并行发育的长达近20000km的现代大陆边缘。
There is not only mosaic structures consisting of small blocks and giant orogenic belts, but also modern continental margin with trenchs, island arc and basins lasting for 20 000 km.
这里不仅有若干小地块与巍峨造山带形成的镶嵌组合，还有以沟、弧、盆并行发育的长达近20000km的现代大陆边缘。
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