玛曲断裂位于东昆仑断裂带的最东段。
Maqu fault is the easternmost segment of the east Kunlun active fault.
东昆仑造山带基底主要形成于古元古代晚期。
东昆仑东段的钴矿床类型主要有喷流沉积型、矽卡岩型等。
The cobalt deposit types in east part of east Kunlun mountain mainly include spout deposition type and skarn type etc.
苦海汞矿床是位于东昆仑造山带南带东段上的大型含金汞矿床。
Kuhai gold-bearing mercury deposit is located in the southern orogenic belt of Eastern Kunlun.
测年结果为研究东昆仑造山带的演化历史提供了重要的年代学资料。
The dating results provide important data for the evolutionary history of the East Kunlun orogenic belt.
结果表明：增温异常条带在东昆仑断裂带不同段落上具有迁移特征。
The results shows:The thermally increasing anomaly belts were migrated in different segments of the east Kunlunshan fault.
在东昆仑中带，北西向韧性剪切带构成了区域构造格局的主要组成部分。
The NW SE ductile shear zones are the main part of the regional tectonic framework in the east of Kunlun Mountains.
其成研究区带隶属昆仑成矿省东昆仑前寒武、晚古生代、中生代金铜铅锌铁成矿带。
Metallogenic belt belong to the province of East Kunlun Precambrian, Paleozoic, Mesozoic gold and copper zinc iron ore belt.
驼路沟钴、金矿位于东昆仑褶皱系昆南断褶带内，产于晚古生代二叠系下统石英片岩中。
Tuoluogou cobalt and gold deposit is in the south of the east Kunlun drape. It formed in quartz schist in the forepant Permian of late vecent life.
这些火成岩组合有规律地分布在构造走廊域内，是揭示东昆仑造山带构造演化的关键所在。
These igneous assemblages are regularly distributed in the corridor and seem to be the key to revealing the tectonic evolution of the East Kunlun orogenic belt.
就目前研究状态而言。确定了早中泥盆世地层在东昆仑西段地区由西往东廷仲的位置。同时。
By the researching currently, the range of the Early-Middle Devonian strata ranging from west to east in west-middle section of east Kunlun Mt. is certained.
应用基于证据权模型，结合GIS空间分析技术评价东昆仑野马泉地区多金属矿产资源潜力。
Assessment on potentiality of the poly-metallic mineral resources in Yemaquan Area, Eastern Kunlun was performed, combining weights-of-evidence model with GIS spatial analysis technology.
东昆仑造山带具有软碰撞、多旋回的特点，造山带内的沉积盆地具有多物源和不同的大地构造背景。
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles. The sedimentary basins inside it have multi-sources and different tectonic backgrounds.
通过对东大滩—东温泉地区的路线地质观测与构造填图，在东昆仑南部发现晚新生代大型逆冲推覆构造系统。
A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.
该年龄与东昆中断裂附近的清水泉蛇绿岩的时代可以很好地对应起来，这为清水泉蛇绿岩带向西的延伸方向及东昆仑地区东段早古生代的构造演化提供了新的年代学证据。
This result thus provides new chronological evidence for the western extension of the Qingshuiquan ophiolite zone and the evolution of the eastern part of the east Kunlun region in Early Paleozoic.
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.
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.
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