1) damsite granite
坝区花岗岩
2) Xiba granite
西坝花岗岩
1.
Based on the detail studies on the petrology and geochemistry of Xiba granite body and porphyry in East Qinling, the deep dynamical process from final collision to orogeny within continent for the Qinling orogenic belt in the Mesozoic has been discussed.
通过秦岭西坝花岗岩体及邻区脉岩体的岩石学、地球化学研究 ,探讨了秦岭造山带中生代期间由全面碰撞转入陆内造山的深部动力学过程。
3) granite area
花岗岩区
1.
Based on measured data, it is analysed that runoff and sediment from hill slope in granite area is influenced by rainfall and maximum ten minutes rainfall density and forecast model of runoff rate and sediment yield from hill slope is established.
根据多年的实测资料，分析了降雨量和最大10分钟两强对花岗岩区坡面产流产沙的影响规律，提出了坡面产流产沙预测预报模型。
5) granite region
花岗岩地区
1.
Application of the surface nuclear magnetic resonance method to detecting groundwater in granite regions;
地面核磁共振找水方法在花岗岩地区的应用
2.
Influence of rainfall factors on preferential flow in the granite region of the Three Gorges of the Yangtze River;
长江三峡花岗岩地区降雨因子对优先流的影响
3.
Because of the universal occurrence of pipe flow, in the granite region, water discharge from soil cross section is much larger than that following Darcy Law(Tsukamoto,1988).
在花岗岩地区 ,由于管流的普遍存在 ,从土壤剖面流出的水量远远超出在达西法则定义下流出的水量。
6) granite area
花岗岩地区
1.
Calculation of carbon sink of granite area and its influencing factors;
花岗岩地区碳汇计算及影响因素研究
2.
Hydrogeochemical characteristics and mechanisms of granite area in Weixi, Yunnan Province;
云南维西花岗岩地区水文地球化学特征及形成机制研究
3.
From the following four aspects: drag forces, velocity, energy and sediment carrying capability of slope surface flow, the threshold gradient of slope surface erosion in the granite area in the south of china is discussed, and it is obtained the critical slope gradient is from 35 to 43 degree.
从坡面流拖曳力、流速、能量及挟沙力４ 个方面，分析了南方花岗岩地区坡面侵蚀临界坡度，得出其临界坡度为３５～４３
补充资料：安南坝自然保护区
安南坝自然保护区地处甘肃酒泉地区阿克塞哈萨克族自治县西部，与青海、新疆交界地带，属于阿尔金山北麓，库穆塔格沙漠以南的中亚内陆，海拔一般在2000m左右，最高可达2923m，气候类型属于温带干旱气候，干旱缺水是该地带自然地理环境的主要特点。 安南坝自然保护区面积39.6万㎡。
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