水土流失其实是一种主要的侵蚀地貌演化过程。
Water and soil loss is an important landforms evolution course.
水土流失，其实是一种主要的侵蚀地貌演化过程。
Water and soil loss is an important physiognomy evolution course.
借助于GIS的空间分析功能，对路南石林巴江流域的地貌演化阶段进行了定量研究。
The paper, by the means of the spatial analysis function of GIS, makes a quantitative research on the stage of geomorphologic evolution in Bajiang drainage basin.
三江并流地带的地貌演化与青藏高原的阶段性隆升有关，而且与东南亚地貌演化关系也较为密切。
The landforms evolvement of the Three Rivers Flow Area has relationship with the stagical rise of the Qinghai-Xizang plateau, and it respects to the landforms evolvement of the South and East Asia.
基岩河道流域地区的地貌演化定量化研究在构造-气候-表面过程关系的探讨中具有十分重要的意义。
The quantitative research of geomorphologic evolution in bedrock channel fluvial landscape plays a significant role in the discussion of the relationship among tectonics, climate, and surface process.
地貌类型多样，气候复杂，为岩溶植被的形成、演化提供了基本的“物质”条件。
The various topographic types and complicated climate provide importment conditions for formation and development of karst vegetation.
桂林喀斯特是世界峰林和峰丛喀斯特景观的典型代表地之一，其代表了地球上一种独特的地貌形态和自然地理特征，具有同时态系统演化的特点；
Guilin karst is a typical landscape in the world with peak forest plain and peak clusters depression, a unique landform style, geographical feature and systematic evolution feature of synchronism.
地貌形成与演化主要受南海新生代两次海底扩张控制。
The two seafloor spreadings of the South China Sea controlled the origin and evolvement of geomorphic types of the study area.
本文运用信息域方法、协同学理论建立了地貌系统演化的一般方程。
By using the Methodology of Information Domain and Synergetics Theory, a general equation of geomorphic systemative evolution has been established in this paper.
该断裂带在山前带和山麓坡的构造地貌、微地文期演化历史方面存在着明显的分段变异。
Between these two segments there have been significant variations in mountain front and piedmont slope tectonic geomorphology. as well as in evolutional history of micro-physiographic stages.
它记录了中生代古火山发生、演化的历史，也展示了一亿年来地质作用所形成的深谷、峰林，有“造型地貌博物馆”之称。
It records the Mesozoic ancient volcano occurred, evolutionary history, also shows 100 million years geological formation of deep canyons, peak forest, have "modelling landform museum," said.
该段河谷地貌的形成演化受构造运动和气候等影响。
The geomorphology of river valleys in Gyaca sector has been controlled by tectonic movement and climate.
该段河谷地貌的形成演化受构造运动和气候等影响。
The geomorphology of river valleys in the Gyaca region has controlled by tectonic movement and climate.
该段河谷地貌的形成演化受构造运动和气候等影响。
The geomorphology of river valleys in the Gyaca region has controlled by tectonic movement and climate.
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