1) mountain uplift erosion
山脉隆升
1.
Several methods using basin sediment to constrain mountain uplift erosion are introduced.
简要介绍了盆地沉积物示踪山脉隆升剥蚀的几种方法并给以实例分析。
2) uplift-history of mountains
山脉隆升历史
1.
This paper mainly discusses the method of constraining on the uplift-history of mountains.
本文简要介绍了现今山脉隆升历史研究方法的现状 ,指出可以利用同位素作为气候变化的指数 ,以气候变化为桥梁来推断山脉隆升历史。
3) uplift and exhumation in the mountains
山脉隆升剥露
4) pulse uplift
脉动隆升
1.
In this paper,it is suggested that the activities of melt include: inducing shear zones or fault by changing the model of crustal stress;affecting the deformation of orogenic belts by accommodating large displacement between massifs;inducing the rapid pulse uplift of orogenic belts or extensional collapse.
熔体活动改变了地壳应力作用方式而诱发形成剪切带或断层；熔体活动调整块体间的位移而影响造山带的变形；熔体活动影响变形机制而诱发造山带的迅速脉动隆升或伸展滑塌。
5) mountain uplift
山体隆升
补充资料：台湾猕猴主要分布在中央山脉及海岸山脉
台湾猕猴主要分布在中央山脉及海岸山脉
台湾猕猴主要分布在中央山脉及海岸山脉
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条