xil

Characteristic of existing glacial development in the Hoh Xil region , Qinghai-Xizang Plateau

青藏高原可可西里地区现代冰川发育特征

Preliminary Study of Hydrochemistry and Sedimentary Characteristics of Salt Lakes in Eastern Hoh Xil Region

青海可可西里东部盐湖水化学及沉积特征初步研究

Fundamental characteristics of Miocene volcanic active belt in the northern margin of Hoh Xil

可可西里北缘中新世火山活动带的基本特征

The cushion plant in the Hoh Xil area of Qinghai

青海可可西里地区垫状植物

Through the comparative experiment , the optimum rooting conditions for Sour jujube and Xil ü jujube were studied .

通过试验比较，探明了酸枣和西吕枣的最佳生根条件。

Discovery of Triassic Norian strata in the Hoh Xil Lake area , western Qinghai , and its geological significance

青海西部可可西里湖地区晚三叠世诺利期地层的厘定及其意义

The Remote Sensing Research of HOH Xil 's Structural Features and Preservation Condition of Oil and Gas ; Relationship between Groundwater and Hydrocarbon Accumulation-Preservation in Sedimentary Basin

可可西里盆地构造特征及其对油气保存条件的遥感研究沉积盆地地下水与油气成藏-保存关系

The degree of research on the Hoh Xil basin has been raised greatly and the history of the uplift of the western Yunnan Plateau has been reconstructed .

大幅度提高了可可西里盆地研究程度，重塑了滇西高原隆升史；

2009-12-07 According to the Qinghai Provincial Meteorological Bureau recently , the first automatic weather station has been built in the Hoh Xil Nature Reserve , northwest China 's Qinghai Province .

2009年12月07日青海省气象局最近表示，可可西里自然保护区建成了首个自动气象站。

The Triassic Bayan Har Mountain Group is the best developed marine sedimentary strata in the Hoh Xil Lake area , mainly distributed in the Hoh Xil-Bayan Har sedimentary basin .

三叠纪巴颜喀拉山群是可可西里湖地区最为发育的海相沉积地层，主要分布于可可西里-巴颜喀拉沉积盆地内。

The altitude of Hoh Xil region might have exceeded 2000m in early-middle Miocene . Thus the higher altitude influenced the planetary system of winds , which in turn prevented the moist air into the inland from the ocean and caused the dry climate .

推测可可西里地区中新世早-中期海拔高度已超过了2000m，并已超过影响行星风系的临界值，阻挡了来自海洋湿润气流进入内陆，导致气候变干。

Lhasa Block to the north basin and the Hoh Xil Block to the south of basin are squeezing into the Qiangtang basin ; the large scale low velocity bodies occur beneath the basin has been interpreted to be originated from the going-up of temperature or upwelling of the mantle .

南侧的拉萨地体和北侧的可可西里地体正向羌塘盆地下挤入；盆地下方大规模的低速体可能是源自温度升高，也可能是地幔物质上涌的结果。