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central tibet
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  西藏中部
     Dynamic Monitoring of Soil Erosion Based on RS and GIS in Central Tibet
     基于RS和GIS的西藏中部地区土壤侵蚀动态监测
短句来源
     A discussion of some problems of stratigraphy in central Tibet
     西藏中部若干地层问题讨论
短句来源
     The strain rate field in the Qiangtang region, central Tibet, also shows nearly equal amount of NNE compression and NWW extension at about 2×10 -8 a -1 , reflecting active faulting along a group of conjugate strike-slip faults oriented northeasterly and northwesterly, possibly resulted from the north-south compression and eastward ductile flow in the asthenosphere.
     西藏中部羌塘地区主应变率场显示均衡的约 2× 10 -8a-1北北东向挤压和北西西向拉张 ,反映本地区一系列走向北东和北西的共轭剪切断裂的活动 ,可能源于南北向挤压和软流层内东向塑性流的驱动。
短句来源
     Effect of Straw Returning on Soil Moisture of Degenerated Farmland in Central Tibet
     秸秆还田对西藏中部退化农田土壤水分的影响
短句来源
     Applying RS and GIS,the method and order of dynamic monitoring of soil erosion were expounded in central Tibet. Classifical system and intensity analysis model of soil erosion are founded, and maps of soil erosion intensity of 1990 and 1995 are composed respectively.
     阐述应用RS和GIS相结合的方法在西藏中部地区进行土壤侵蚀动态监测研究的方法和流程,建立了土壤侵蚀分类系统和强度分析模型,分别编制1990年和1995年的土壤侵蚀强度图。
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  西藏中部地区
     Dynamic Monitoring of Soil Erosion Based on RS and GIS in Central Tibet
     基于RS和GIS的西藏中部地区土壤侵蚀动态监测
短句来源
     Microbial characteristics of straw-amended degraded soils in central Tibet and its effect on soil fertility.
     西藏中部地区退化土壤秸秆还田的微生物变化特征及其影响
短句来源
     Applying RS and GIS,the method and order of dynamic monitoring of soil erosion were expounded in central Tibet. Classifical system and intensity analysis model of soil erosion are founded, and maps of soil erosion intensity of 1990 and 1995 are composed respectively.
     阐述应用RS和GIS相结合的方法在西藏中部地区进行土壤侵蚀动态监测研究的方法和流程,建立了土壤侵蚀分类系统和强度分析模型,分别编制1990年和1995年的土壤侵蚀强度图。
短句来源
  西藏中部农田
     Microbes Characteristics of Soil Rehabilitation in Central Tibet
     西藏中部农田土壤复退过程中的生物学特征
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  “central tibet”译为未确定词的双语例句
     THE INTENSITY AND EPICENTER OF THE 2004 M_S 5.6 DUNG CO EARTHQUAKE AND THE RELATION WITH ACTIVE FAULTING IN CENTRAL TIBET
     2004年西藏懂错M_S 5.6地震的宏观烈度调查与控震构造分析
短句来源
     Our results reveal that(1) the crustal thickness is 65±5km beneath the central Tibet. On the average,the Moho in Qiangtang is 5~6km shallower than that in Lhasa terrane.
     结果显示:(1)沿着INDEPTH-Ⅲ剖面,地壳厚度整体变化不大,均为65±5km,其中拉萨地块Moho界面埋深较羌塘地体要深约5~6km.
短句来源
     The Moho depth of Qiangtang block situated at the central Tibet plateau is 74 km,and changed to 67 km slowly outward,but changed to 50km rapidly at the margins.
     中心地带的羌塘地体莫霍面深度达74 km,向四周慢慢变浅至67 km左右,边缘地区突然变浅至50km左右.
短句来源
     Ria copper deposit southeast(about 100km)of Coqin county city in western central Tibet plateau includes two mineralization types.
     青藏高原中-西部措勤县城东南(约100km)的日阿铜矿区发育两种矿化类型,一种是与二长花岗斑岩岩株有关的夕卡岩型铜矿化,另一种是与辉绿玢岩脉有关的细脉浸染型(斑岩型)铜矿化。
短句来源
     To study the resistivity structure of crust and upper mantle beneath northern and central Tibet,furthermore,discuss thermal behavior of north and central Tibet lithosphere,super-wide band magnetotelluric sounding profiles named line 500 and line 600 which belongs to INDEPTH(Ⅲ) were finished in 1998 and 1999.The line 500 is from Dêqên to Longwei Co,and the line 600 is from Nagqu to Golmud.
     为了研究西藏中、北部壳、幔导电性结构,讨论高原中、北部岩石圈热状态,1998年和1999年(INDEPTH(Ⅲ)-MT)在西藏中、北部完成了德庆—龙尾错(500线)和那曲—格尔木(600线)超宽频带大地电磁深探测剖面的研究.
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  central tibet
In this research, weather data and evaporation models are used to determine the climatic cause of a recent water-balance change in Ahung Co, a lake in central Tibet.
      
Reviews; Luciano Petech, Central Tibet and the Mongols.
      
The origin of cultivated Tatary buckwheat, the hybrid origin of weedy Tatary buckwheat and of the wild populations from central Tibet and northern Pakistan are discussed.
      
This study focuses on the meso-regional pattern of rangeland ecotypes in Central Tibet in relation to population density.
      
Population and rangelands in Central Tibet: a GIS-Based Approach
      
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The Meridonal structural zones in western China have been rarely repor- ted,despite their wide distribution. They may be divided into six zones: a)Sichuan-Yunnan—East Qinghai lake zone; b)West Yunnan—West Qinghai lake zone; c)East Tibet—West Gansu zone; d)Central Tibet—East Xinjiang zone; e)Mt.Jolmolungma—Mt.Friendship zone; f)West Tibet—West Xinjiang zone. These zones are characterized by:(a)Presence of large superposed folds and basement faults;(b)Complex mechanical properties,often with...

The Meridonal structural zones in western China have been rarely repor- ted,despite their wide distribution. They may be divided into six zones: a)Sichuan-Yunnan—East Qinghai lake zone; b)West Yunnan—West Qinghai lake zone; c)East Tibet—West Gansu zone; d)Central Tibet—East Xinjiang zone; e)Mt.Jolmolungma—Mt.Friendship zone; f)West Tibet—West Xinjiang zone. These zones are characterized by:(a)Presence of large superposed folds and basement faults;(b)Complex mechanical properties,often with the compressive,tensile and shear structural features present in the same stru- ctural zone;(c)A long development and repeated activity,having suffered an E-W compression during the decline of the Latitudinal structural zone; (d)Awider development in central Asia beyond the limits of the western China,and a long,discontinued northward or southward extension. The meridional structural zones in western China are parts of those of the whole earth.They may originate from a change of the rate of the Earth's rotation.

中国西部经向构造体系可划分六个构造带,以4°—5°间距贯穿全区,并向两端延伸,应属全球经向构造体系的组成部分。笔者依据最新地质及地球物理资料,论述了他们的分布特征及其成因机制,并指出它们在地壳演化和寻找有用矿产方面的意义。

In this paper the results of computer simulation of the effect of hydrothermal convection along faults, as well as the occurrences of faults, mountain relief and contrast in thermal conductivity of sedimantery basin and basement rocks as four major conditioning factors on the distribution of conductive surface heat flow in eight original and seven combined models are reported. The model designing and parameter selection are mainly based on the observed surface heat flow of conductive-convective type in some...

In this paper the results of computer simulation of the effect of hydrothermal convection along faults, as well as the occurrences of faults, mountain relief and contrast in thermal conductivity of sedimantery basin and basement rocks as four major conditioning factors on the distribution of conductive surface heat flow in eight original and seven combined models are reported. The model designing and parameter selection are mainly based on the observed surface heat flow of conductive-convective type in some geothermal areas in the North-Central Tibet. However, the correction for convective component is not directly involved here, instead, a much profounder single-factor and multifactor model investigation is implemented. In order to reach better applicability of the simulation results a series of dimensionless parameters such as α = K1/K2 (where K1 and K2 stand for thermal conductivities of basement rocks and sedimentary basin, respectively), β = qy/q (where qy and q signify the vertical component of surf ace heat flow and basal heat flux at the bottom of the model, respectively), and r = L/H (where L and H are the distance from the left boundary of the model and height of the mountain, respectively) are adopted. The analysis of the simulation results shows that in the light of their importance the above-mentioned four factors can be arranged in the following order: convection velocity-occurrences of faults-contrast in thermal conductivities of medium-topogrphic effect.

本文对8个初始模型和7个组合模型中沿断层的水热对流、断层产状、山体地形和沉积盆地与基岩热导率反差等四个影响因素对传导型地表热流分布的影响进行了计算机模拟研究。模型设计和参数的选值以西藏中北部一些地热区实测的传导-对流型热流为主要参考依据,但不直接涉及对流组分的校正,而着眼于更广泛的单因子和多因素的模型研究。分析中采用无量纲参数:α=(K_1)/(K_2)(K_1和K_2分别为基岩和沉积盆地的热导率),β=(q_1)/(q_2)(q_1和q_2分别为地表热流的垂向分量和模型的底部热流)以及γ=L/H(L和H分别为离模型左侧边界的距离和山体的高度),以求更广的普适性。对模拟结果的分析表明,上述四项影响因素依其重要性可排序为对流强度—断层倾角—介质热导率反差—地形效应。

Gyaring Co fault zone across Xainza and central Tibet had been formed before late Cretaceous period,and has been reactivated with right lateral motion since Quaternary.The fault zone consists of four subparallel faults in an arrangement of right stepping en echelon,and three pull-apart basins,occupied by Zigui Co,Gyaring Co and Waang Co respectively,are formed in righ-step like.Gyaring Co fault zone is one of main seis-mogenic fault in central Tibetean plateau.At least four surface ruptures associated...

Gyaring Co fault zone across Xainza and central Tibet had been formed before late Cretaceous period,and has been reactivated with right lateral motion since Quaternary.The fault zone consists of four subparallel faults in an arrangement of right stepping en echelon,and three pull-apart basins,occupied by Zigui Co,Gyaring Co and Waang Co respectively,are formed in righ-step like.Gyaring Co fault zone is one of main seis-mogenic fault in central Tibetean plateau.At least four surface ruptures associated with earthquake have occurred clearly along the fault zone since Holocene,with the segmentation of activity along the fault zone.

格林错断层带是一条晚白垩纪以前形成,第四纪以来具明显活动性质的右旋走滑断层。断层带由4条次级走滑断层呈右行右阶羽列排列而成,在两条次级走滑断层的连接部位分别形成孜桂错、格林错、瓦昂错拉分区。格林错断层带是西藏中部地区的主要发震断层之一,全新世以来,至少有4期地震地表破裂沿该断层带发生。第四纪晚期,断层具明显的分段活动性质,并且断层活动有从北西向南东、向南迁移的迹象。

 
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