藏南

另外，据藏南地区的SKS波分裂时间延迟很小的特点，推测藏南地幔中可能不存在各向异性，也就是没有足够的热源使各向异性矿物的品格重新定位。

From the tiny time delay in SKS splitting in the area , it is inferred that the partial mel-ting may not exist in the mantle due to the lack of enough heating for the reorientation of anisotropic minerals .

藏南的上地幔盖层则可能发生以正断层为主的脆性变形。

Brittle deformation might occur in the uppermost mantle of southern Xizang .

藏南岗巴-定日地区花岗岩单元特征及构造环境

The granite units and their tectonic settings in the Gamba-Tingri zone , southern Xizang

藏南中生代以来硅质沉积物的微组构特征及其地质意义微生物在进入地下水时，水质几乎与普通地下水相同。

Microbial when entering groundwater , water quality almost as identical as common groundwater .

藏南亚东地区前寒武纪结晶岩系以往统称为“聂拉木群”。

The Precambrian crystalline rock series in the Yadong area is previously called " the Nyalam Group " .

在青藏高原的地球物理考察中，用本仪器先后在藏南、藏北五个点进行了连续数月的野外地磁测量。

The instrument has been used for continuous field observations in five localities in the north and south of Xizang .

藏南拉轨岗日带展布着串珠状变质核杂岩，其内出露的淡色花岗岩体构成北喜马拉雅淡色花岗岩带。

Leucogranites , distributed in the core or detachment of the MCC , form the famous northern Himalayan leucogranites belt .

藏南特提斯喜马拉雅带中段二叠纪&白垩纪的火山活动（Ⅰ）：分布特点及其意义

Permian to Cretaceous volcanic activities in the central segment of the Tethyan Himalayas ( I ): distribution characteristics and significance

藏南沉积硅质岩与锑、金多金属等矿化关系密切，成矿流体和热水流体有很强的相关性。

The cherts have a close relationship with Sb 、 Au polymetallic mineralization and ore-forming fluid correlates strongly with hydrothermal water .

同藏南8个表土样花粉分析结果相比较，现代花粉雨反映了森林和草原植被的不同。

As compared with 8 surface sample pollen analysis of Southern Xizang Plateau , vegetational variations between the steppe and forest are evident in the modern pollen rain .

从分布的生境来看，盘菌多发生于藏东南、藏东和藏南的森林区域，尤以冷杉林和硬叶栎林中居多，一些种类在该区域的发生表现出特殊的生态学特性。

Most of them distributed mainly in forest in the southeastern , the eastern and the southern of Xizang , especially presented in fir forests and woods of hard - leaf oak .

札达盆地与高喜马拉雅断块隆起存在盆&山耦合关系，藏南谷地基底断块的翘板式运动是形成盆地的主要控制因素。

There are a basin range coupling between the Zanda basin and the high Himalaya region . The seesaw type tectonic movement of the basement fault block in the south of the plateau is the primary control factor for the basin forming .