昆仑山由东、中、西昆仑三部分组成。
The Kunlun Mountains comprise the East, Middle and West Kunlun Mountains.
论证了西昆仑地区的胜利桥岩体是一个复式岩基。
The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
块状硫化物矿床是西昆仑地区重要的铜矿床类型之一。
Massive sulfide ore deposit is a very important copper deposit type in west of Kunlun.
MVT型铅锌矿是西昆仑地区重要的铅锌矿床类型之一。
MVT leadzinc deposit is a very important leadzinc deposit type in west of Kunlun.
在西昆仑山北部的调查区内，都有钙-碱性的深成岩体出露。
In the investigation region, in the northern part of the West Kunlun Mountains calc-alkaline plutonic rocks are exposed.
同时还认为，西昆仑造山带在古生代具有多岛洋构造格局的特点。
It also believed that the West Kunlun orogenic belt had the tectonic framework characteristic of many island ocean in Paleozoic.
这对研究西昆仑山早前寒武纪陆壳增生及构造演化提供了重要的地质资料。
This study supplies new geological data for research of the early Precambrian crust growth and tectonic evolution of Western Kunlun.
进一步研究表明，西昆仑山地区西段中晚更新世至少经历了3次强烈的隆升。
Further study suggests that the western of the west Kunlun Mountains in the Mid-late Pleistocene has undergone at least 3 times strong upheaval.
西昆仑山前晚新生代地貌与沉积特征记录了西昆仑山及青藏高原西北缘的隆升过程。
The late Cenozoic geomorphologic and sedimentary features in the west Kunlun Mountain front record the uplift process of the west Kunlun Mountains and the western margin of the Qinghai-Tibet Plateau.
综合西昆仑的区域地质和已有的铜矿研究成果，认为该区具有形成大型铜矿床的地质背景。
Based on the studies of regional geology and existing copper deposits, it is indicated that there is favorable geologic setting for a large-scale copper deposit in west Kunlun.
新疆西昆仑奥依塔克-恰尔隆拗陷带内阿克塔什-萨落依成矿带发现多处火山岩型块状硫化物铜矿床。
Lots of volcanic-hosted massive sulfide deposits were found along the Aketashi-Saluoyi metallogenic belt in the Aoyitake-Qiaerlong rifted depression within the West Kunlun Mountains of Xinjiang.
西昆仑以其强烈的构造变形、频繁的岩浆活动、漫长的地质演化历史及特殊的大地构造环境而具有得天独厚的成矿地质条件。
Magmation was frequent, tectonic deformation was violent, the history of geological evolvement was long and geological condition of producing mineral was good in West Kunlun.
西昆仑赛力亚克混杂堆积由形态、颜色和大小各异的沉积岩块体以及黑色泥质粉砂岩夹灰紫绿色钙质页岩、泥灰岩和层凝灰岩的基质组成。
The Saliyak melange consists of dark-gray to black muddy and silty microclastic rock with intercalation of grayish purple and grayish green calcareous and muddy shale, marl and tuff.
本文系统研究了西昆仑-喀喇昆仑地区晚古生代-早中生代地层的岩石组合及其分布特征，结合所含的生物组合特征绘制了研究区泥盆纪、石炭纪、早中二叠世及三叠纪的岩相古地理略图。
The late Paleozoic-early Mesozoic strata in the Western Kunlun-Karakorum area are main research object and the accreting orogenic theory is used for structural analysis in this paper.
作为尝试，对昆仑山口西m(下标s) 8.1地震触发的北京地区断层活动进行了反演。
As an attempt, we inverse the assumingly active faults' slips triggered by the m (subscript s) 8.1 Kunlun Mountain earthquake over Beijing area.
根据昆仑山口西8.1级地震前后GPS测点的位移速率，用弹性模型公式计算了地壳应变参数。
Based on the velocities of GPS sites before and after the M8.1 Kunlunshan earthquake, the crustal strain parameters are calculated with the elastic model.
根据昆仑山口西地震测线断层围陷波的观测结果，可推断该处破裂面宽度为300m左右，远远大于地表破裂带的宽度。
Based on the fault zone trapped waves observed in Kunlun Mountain Pass region, the width of the rupture plane is deduced to be about 300 m and is greater than that on the surface.
在北昆仑库尔良的西邻库地发现有铜（镍）硫化物矿，未见北昆仑地区发现铜（镍）硫化物矿的报导。
So far. sulfide ore of copper (nickel) was discovered on the west of Kudi in Kuerliang of the North Kunlun, but no one got the report that the ore was found in the area of North Kunlun.
玛尼7.9级地震对昆仑山口西8.1级地震的触发作用及动力背景初探。
Study of Triggering Action Between Mani(M_S7.9) and Kunlun(M_S8.1) Great Earthquakes and Their Dynamic Background.
玛尼7.9级地震对昆仑山口西8.1级地震的触发作用及动力背景初探。
Study of Triggering Action Between Mani(M_S7.9) and Kunlun(M_S8.1) Great Earthquakes and Their Dynamic Background.
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