Recent mapping and seismic survey reveal that intensive compression during the Early Cenozoic in the Qiangtang block of the central Tibetan Plateau formed an extensive complex of thrust sheets that moved relatively so...Recent mapping and seismic survey reveal that intensive compression during the Early Cenozoic in the Qiangtang block of the central Tibetan Plateau formed an extensive complex of thrust sheets that moved relatively southward along several generally north-dipping great thrust systems. Those at the borders of the ~450 km wide block show it overrides the Lhasa block to the south and is overridden by the Hohxil-Bayanhar block to the north. The systems are mostly thin-skinned imbricate thrusts with associated folding. The thrust sheets are chiefly floored by Jurassic limestone that apparently slid over Triassic sandstone and shale, which is locally included, and ramped upward and over Paleocene-Eocene red-beds. Some central thrusts scooped deeper and carried up Paleozoic metamorphic rock, Permian carbonate and granite to form a central uplift that divides the Qiangtang block into two parts. These systems and their associated structures are unconformably overlain by little deformed Late Eocene-Oligocene volcanic rock or capped by Miocene lake beds. A thrust system in the northern part of the block, as well as one in the northern part of the adjacent Lhasa block, dip to the south and appear to be due to secondary adjustments within the thrust sheets. The relative southward displacement across this Early Cenozoic mega thrust system is in excess of 150 km in the Qiangtang block, and the average southward slip-rate of the southern Qiangtang thrusts ranged from 5.6 mm to 7.4 mm/a during the Late Eocene-Oligocene. This Early Cenozoic thrusting ended before the Early Miocene and was followed by Late Cenozoic crustal extension and strike-slip faulting within the Qiangtang block. The revelation and understanding of these thrust systems are very important for the evaluation of the petroleum resources of the region.展开更多
The Jiarong Tibetan traditional residence is a characteristic regional architecture, located in a high-intensity, high-altitude and cold area, with geographic identification, and is a typical representative of this et...The Jiarong Tibetan traditional residence is a characteristic regional architecture, located in a high-intensity, high-altitude and cold area, with geographic identification, and is a typical representative of this ethnic group. It has also become an important tourist destination and has important research value. The research used the methods of field survey surveying and mapping to conduct field survey and surveying on 20 buildings in Xisuo Village, a traditional village in the Jiarong Tibetan area. Measure building plans, elevations, and building sections, and collect measurement data for statistical analysis. The results show that the average total height of the building is 10.08 m, the average total building span is 12.44 m, the average total depth is 10.87 m, and the squareness is 0.87. The square shape of the building is more in line with the seismic requirements of high-intensity areas and the local terrain environment<span style="font-family:Verdana;">.<span style="font-family:Verdana;"> The maximum window-wall ratio in the building is 0.18 south for the second floor, and 0.025 west for the first floor. Smaller window-to-<span style="font-family:Verdana;"> <span style="font-family:Verdana;">wall ratios have better adaptability to high-altitude cold areas<span style="font-family:Verdana;">.<span style="font-family:Verdana;"> The height of the building beam section is generally from 0.17 m to 0.32 m, and the average Beam span-depth ratio is 0.10. The building space construction has a good match with the properties of wood materials. These conclusions quantitatively analyze the characteristics of stone-built houses in high-intensity, high-altitude and cold areas, supplement the research on ethnic regional architecture, and provide materials and references for the design, repair and update of related buildings.展开更多
不同语体阅读知觉广度的研究由来已久,研究重心多集中于拼音文字和表意文字,已有研究表明阅读知觉广度存在语言加工的特异性。藏语作为拼音文字,同时具有表意文字的特征,是阅读知觉广度研究尚未涉及的语言材料。因此,藏语阅读知觉广度...不同语体阅读知觉广度的研究由来已久,研究重心多集中于拼音文字和表意文字,已有研究表明阅读知觉广度存在语言加工的特异性。藏语作为拼音文字,同时具有表意文字的特征,是阅读知觉广度研究尚未涉及的语言材料。因此,藏语阅读知觉广度的范围尚不清楚,藏语阅读知觉广度是否也表现出语言加工的特异性也有待证实。为了探测藏语阅读知觉广度的大小,使用Eye Link 1000 Plus型眼动记录仪,以35名在校藏族大学生为被试,采用经典的移动窗口范式,设计了7种窗口(5、9、13、17、21、25和整行)。结果发现,L2R2-L12R12在所有指标的观测值上均存在显著差异,L4R4-L12R12在总注视次数、总注视时间和向右眼跳幅度三个指标的观测值上存在显著差异,L6R6-L12R12在向右眼跳幅度指标的观测值上存在显著差异,L8R8-L12R12在所有指标的观测值上均不存在显著差异,达到了基准水平。结果支持藏族大学生藏语阅读知觉广度的右侧范围大约是注视点右侧4~8个字符的空间。阅读知觉广度存在语言加工的特异性。展开更多
基金financially supporting the research under grants No.1212011221111,Sinoprobe-02-01 and 2006DFB21330 respectively
文摘Recent mapping and seismic survey reveal that intensive compression during the Early Cenozoic in the Qiangtang block of the central Tibetan Plateau formed an extensive complex of thrust sheets that moved relatively southward along several generally north-dipping great thrust systems. Those at the borders of the ~450 km wide block show it overrides the Lhasa block to the south and is overridden by the Hohxil-Bayanhar block to the north. The systems are mostly thin-skinned imbricate thrusts with associated folding. The thrust sheets are chiefly floored by Jurassic limestone that apparently slid over Triassic sandstone and shale, which is locally included, and ramped upward and over Paleocene-Eocene red-beds. Some central thrusts scooped deeper and carried up Paleozoic metamorphic rock, Permian carbonate and granite to form a central uplift that divides the Qiangtang block into two parts. These systems and their associated structures are unconformably overlain by little deformed Late Eocene-Oligocene volcanic rock or capped by Miocene lake beds. A thrust system in the northern part of the block, as well as one in the northern part of the adjacent Lhasa block, dip to the south and appear to be due to secondary adjustments within the thrust sheets. The relative southward displacement across this Early Cenozoic mega thrust system is in excess of 150 km in the Qiangtang block, and the average southward slip-rate of the southern Qiangtang thrusts ranged from 5.6 mm to 7.4 mm/a during the Late Eocene-Oligocene. This Early Cenozoic thrusting ended before the Early Miocene and was followed by Late Cenozoic crustal extension and strike-slip faulting within the Qiangtang block. The revelation and understanding of these thrust systems are very important for the evaluation of the petroleum resources of the region.
文摘The Jiarong Tibetan traditional residence is a characteristic regional architecture, located in a high-intensity, high-altitude and cold area, with geographic identification, and is a typical representative of this ethnic group. It has also become an important tourist destination and has important research value. The research used the methods of field survey surveying and mapping to conduct field survey and surveying on 20 buildings in Xisuo Village, a traditional village in the Jiarong Tibetan area. Measure building plans, elevations, and building sections, and collect measurement data for statistical analysis. The results show that the average total height of the building is 10.08 m, the average total building span is 12.44 m, the average total depth is 10.87 m, and the squareness is 0.87. The square shape of the building is more in line with the seismic requirements of high-intensity areas and the local terrain environment<span style="font-family:Verdana;">.<span style="font-family:Verdana;"> The maximum window-wall ratio in the building is 0.18 south for the second floor, and 0.025 west for the first floor. Smaller window-to-<span style="font-family:Verdana;"> <span style="font-family:Verdana;">wall ratios have better adaptability to high-altitude cold areas<span style="font-family:Verdana;">.<span style="font-family:Verdana;"> The height of the building beam section is generally from 0.17 m to 0.32 m, and the average Beam span-depth ratio is 0.10. The building space construction has a good match with the properties of wood materials. These conclusions quantitatively analyze the characteristics of stone-built houses in high-intensity, high-altitude and cold areas, supplement the research on ethnic regional architecture, and provide materials and references for the design, repair and update of related buildings.
文摘不同语体阅读知觉广度的研究由来已久,研究重心多集中于拼音文字和表意文字,已有研究表明阅读知觉广度存在语言加工的特异性。藏语作为拼音文字,同时具有表意文字的特征,是阅读知觉广度研究尚未涉及的语言材料。因此,藏语阅读知觉广度的范围尚不清楚,藏语阅读知觉广度是否也表现出语言加工的特异性也有待证实。为了探测藏语阅读知觉广度的大小,使用Eye Link 1000 Plus型眼动记录仪,以35名在校藏族大学生为被试,采用经典的移动窗口范式,设计了7种窗口(5、9、13、17、21、25和整行)。结果发现,L2R2-L12R12在所有指标的观测值上均存在显著差异,L4R4-L12R12在总注视次数、总注视时间和向右眼跳幅度三个指标的观测值上存在显著差异,L6R6-L12R12在向右眼跳幅度指标的观测值上存在显著差异,L8R8-L12R12在所有指标的观测值上均不存在显著差异,达到了基准水平。结果支持藏族大学生藏语阅读知觉广度的右侧范围大约是注视点右侧4~8个字符的空间。阅读知觉广度存在语言加工的特异性。
