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昆仑山
kunlun mountains
Glacio-Hydrological Characteristics of Gozha Glacier on South Slope of the West Kunlun Mountains 西昆仑山南坡郭扎冰川水文特征的分析 短句来源 Evolution of Glaciers and Environment in the West Kunlun Mountains During the Past 32 ka 西昆仑山32ka来的冰川与环境演变 短句来源 A Study of Strong Earthquake′s Tendency after the Earthquake (Ms=8.1)of the west Kunlun Mountains Pass 昆仑山口西8.1级地震后的强震趋势研讨 短句来源 Anomalies recorded by the digital deformation observation instruments at the Xuzhou Seismic Station prior to the M8.1 earthquake of 14 Nov. 2001 to the west of the Kunlun Mountains′ Pass 2001年11月14日昆仑山口西8.1级大震前徐州台数字化形变观测仪器记录的异常 短句来源 A discussion on the magnitude 8.1 earthquake to the west of the Kunlun Mountains′ Pass and the trend of its aftershock activity 有关昆仑山口西8.1级地震及其余震活动趋势的讨论 短句来源 更多 kunlun mountain
The coseismic horizontal displacement field caused by the Kunlun Mountain Ms8.1 earthquake is simulated by use of elastic finite element method and GPS observations,the coseismic apparent strain variation field and the coseismic dislocation of main active faults are calculated. 利用弹性有限元方法,结合GPS观测资料,模拟了昆仑山口西Ms8.1地震产生的同震水平位移场,计算了同震视应变变化场及主要活动断裂的同震错动。 短句来源 Remote anomalies of subsurface fluid before the Ms8.1 earthquake in west of Kunlun Mountain mouth and their significance 昆仑山口西Ms8.1地震前地下流体的远场异常及其意义 短句来源 The Continuous Discussion on the Prediction of the Great Earthquake (M_S=8.1)in the West of Kunlun Mountain Pass in 2001 2001年昆仑山口西8.1级大震预报的再讨论 短句来源 BOREHOLE STRAIN ANOMALY AT GAOTAI STATION BEFORE EARTHQUAKE OF M 8.1 IN WEST TO KUNLUN MOUNTAIN PASS 昆仑山口西Ms8.1地震前高台钻孔应变异常 短句来源 Analysis to the earthquake situation within 1to 3 years in mainland of China From the West Kunlun Mountain Pass M8.1 earthquake 由昆仑山口西8.1级地震分析中国大陆1～3年地震大形势 短句来源 更多 kunlun
Glacio-Hydrological Characteristics of Gozha Glacier on South Slope of the West Kunlun Mountains 西昆仑山南坡郭扎冰川水文特征的分析 短句来源 The coseismic horizontal displacement field caused by the Kunlun Mountain Ms8.1 earthquake is simulated by use of elastic finite element method and GPS observations,the coseismic apparent strain variation field and the coseismic dislocation of main active faults are calculated. 利用弹性有限元方法,结合GPS观测资料,模拟了昆仑山口西Ms8.1地震产生的同震水平位移场,计算了同震视应变变化场及主要活动断裂的同震错动。 短句来源 Evolution of Glaciers and Environment in the West Kunlun Mountains During the Past 32 ka 西昆仑山32ka来的冰川与环境演变 短句来源 Remote anomalies of subsurface fluid before the Ms8.1 earthquake in west of Kunlun Mountain mouth and their significance 昆仑山口西Ms8.1地震前地下流体的远场异常及其意义 短句来源 A Study of Strong Earthquake′s Tendency after the Earthquake (Ms=8.1)of the west Kunlun Mountains Pass 昆仑山口西8.1级地震后的强震趋势研讨 短句来源 更多 kunlun mountain pass
The Continuous Discussion on the Prediction of the Great Earthquake (M_S=8.1)in the West of Kunlun Mountain Pass in 2001 2001年昆仑山口西8.1级大震预报的再讨论 短句来源 BOREHOLE STRAIN ANOMALY AT GAOTAI STATION BEFORE EARTHQUAKE OF M 8.1 IN WEST TO KUNLUN MOUNTAIN PASS 昆仑山口西Ms8.1地震前高台钻孔应变异常 短句来源 Analysis to the earthquake situation within 1to 3 years in mainland of China From the West Kunlun Mountain Pass M8.1 earthquake 由昆仑山口西8.1级地震分析中国大陆1～3年地震大形势 短句来源 PRELIMINARY STUDY ON ANOMALOUS SEISMICITY PATTERN BEFORE M_S=8.1 EARTHQUAKE IN THE WEST OF KUNLUN MOUNTAIN PASS 昆仑山口西8.1级地震前地震活动异常图像初步研究 短句来源 TIP STRUCTURES OF THE WESTERN SEGMENT OF SURFACE RUPTURE ZONE OF THE M_S 8.1 WEST OF KUNLUN MOUNTAIN PASS EARTHQUAKE 昆仑山口西8.1级地震西破裂带尾端破裂特征 短句来源 更多 
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The Tieshidas Group in Qimantag, a branch of the East Kunlun Mountains, was classically considered the Caledonian basement, and classified into Middle-Upper Ordovician, Upper Ordovician or simply Lower Paleozoic.
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Deep seismic reflection profile across the juncture zone between the Tarim Basin and the West Kunlun Mountains
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Evidence is found for the northward subduction of the northwest marginal lithosphere of the Qinghai-Tibetan Plateau and its collision with Tarim lithosphere beneath the West Kunlun Mountains.
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The lithosphere image of the face-to-face subduction and collision determines the coupling relationship between the Tarim Basin and the West Kunlun Mountains at the lithosphere scale and reflects the process of continent-continent collision.
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In the Kunlun Mountains Pass area, all the landform, structure, sedimentary facies and assembladge of organisms show that a violent tectonic movement occurred between 1.1-0.7 MaB.
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Temporal and spatial rupture process of the great Kunlun Mountain Pass earthquake of November 14, 2001 from the GDSN long period
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Gravity variation before Kunlun mountain pass western MS=8.1 earthquake
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A discussion on corioli force effect and aftershock activity tendency of the M=8.1 Kunlun Mountain Pass earthquake on Nov.
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b) The fault of the M=8.1 Kunlun Mountain earthquake on Nov.
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In the paper, the feature of strong earthquake orderly distribution in time, space and intensity before the Western Kunlun Mountain Pass M=8.1 earthquake is preliminarily studied.
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The Middle Kunlun fault (F10), which is the main structure of the Kunlun fault zone, is a high angle, super-deep fault.
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Based on the conductive structure of the profile, the southern part of the Middle Kunlun fault belongs to the Tibetan plateau, but it is not certain whether the northern part of the Middle Kunlun fault belongs to the Tibetan plateau.
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Three Late Triassic plate sutures, namely, the Longmu Co-Shuanghu suture, Kunlun-Qinling suture and Xijinwulan-Jinshajiang suture, have been recognized on the Qinghai-Tibet plateau.
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The Kunlun Platform was situated in the south, where there were two small lands.
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Shuttle imaging radar-C (SIR-C) detection for the Cenozoic volcanoes in West Kunlun, China
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Temporal and spatial rupture process of the great Kunlun Mountain Pass earthquake of November 14, 2001 from the GDSN long period
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Gravity variation before Kunlun mountain pass western MS=8.1 earthquake
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A discussion on corioli force effect and aftershock activity tendency of the M=8.1 Kunlun Mountain Pass earthquake on Nov.
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In the paper, the feature of strong earthquake orderly distribution in time, space and intensity before the Western Kunlun Mountain Pass M=8.1 earthquake is preliminarily studied.
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The November 14, 2001 west of Kunlun Mountain Pass earthquake: An earthquake with unsaturated surface wave magnitude
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