藏南地区

  • 网络south tibet
藏南地区藏南地区
  1. 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 .

  2. 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 " .

  3. 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