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81.
82.
The geological processes responsible for outward growth of the Tibetan Plateau are debated.The Qilian Mountains on the northeastern margin of the plateau comprise one of the youngest structural components of the plateau whose understanding is key to deciphering the broader geological evolution of the region.Here,based on a reprocessed deep seismic profile which was originally collected during the 1990 s across the northeast margin of the western Qilian Mountains and previous geological and geophysical data,we find evidence for decoupled crustal deformation that was partitioned by a decollement,in which lowercrustal deformation featured by local duplexing preceded upper-crustal deformation featured by imbricate thrusts.Furthermore,we propose that the Asian lithospheric mantle is being underthrust beneath the western Qilian Mountains,as inferred from patterns of lower crustal deformation which is marked by the Moho geometry.Integrating these results yields a better understanding of lithospheric deformation of western Qilian Mountains,northeastern margin of the plateau during the Cenozoic. 相似文献
83.
84.
Stretching characteristics and its dynamic significance of the northern continental margin of South China Sea 总被引:5,自引:0,他引:5
Zhang YunFan Sun Zhen Zhou Di Guo XingWei Shi XiaoBin Wu XiangJie Pang Xiong 《中国科学D辑(英文版)》2008,51(3):422-430
To investigate the thinning of the whole crust, and the contribution of the upper versus lower crust to the stretching since Cenozoic, we calculated the stretching factor of the northern margin of South China Sea with data such as whole crustal thickness, depth of Cenozoic sedimentary basement and the horizontal displacement of faults. An isometric line drawing on whole crustal stretching factor is then obtained. Along the seismic Line 1530 in Baiyun sag, we also calculated the stretching factors of the upper and lower crust. The results suggest that the whole crustal thickness decreases seaward while the whole crustal stretching factor increases from shelf to slope. The Moho upwells highest beneath where the crust is thinned most. The value of the whole crustal stretching factor ranges from 1.5 to 6. Two areas were thinned intensely: the center of Yinggehai Basin, and the Baiyun sag in the Pearl River Mouth Basin. The calculation of the upper and lower crustal stretching factors from DSP1530 in Baiyun sag shows that the original crust of Baiyun sag should be thinned before deformation. Its pre-Cenozoic evolution as well as tectonic position during Cenozoic might be responsible for that. 相似文献
85.
Preliminary results of measuring the crustal deformation in Qinghai-Xizang area using GPS technique 总被引:5,自引:0,他引:5
GPS repetition measurement tbta in Qinghai-Xizatlg (Tibetan) area in 1992 and 1994 have been used to determine the change
rates of seven bascline vectors of Lhasa-Wenquan, etc. It is the first time to obtain the direct observation results of the
large-scale crustal horizontal motions in this area. Thesc preliminary results also for the first time provide the direct
observation evidence for some important geophysical and geological viewpoints, such as the northward gradual reduce of the
effect of the northward push-pressing to Eurasian continent by Indian Plate in the Qinghai-Xizang area, having a southward
strike slip movement of the Chuan-Dian diamond block, etc. 相似文献
86.
Chen Shun-yun Xu Zhao-yong Yang Run-hai Zhao Jin-ming Hao Jin-qi Wang Yun-yun Xiong Bing-heng Wang Zheng-rong 《地震学报(英文版)》2002,15(6):656-666
Based on the phenomena that the deformation gap was observed before the great Tangshang earthquake, this paper discusses the
strain gap according to test and theory. The (strain) patterns were recorded photographically by realtime holographic interferometry
and shadow optical method of caustics, as soon as the loading process started. In the meantime, the AE (acoustic emission)
signals were recorded by a micro crack information storage-analysis system. According to damage theory and location of micro
fracture, we have studied the stain gap and gained: a) It is necessary that strain gap appears under the condition of linear
elasticity theory, and its situation is relatively stable, corresponding to stress concentration. b) Micro fractures, which
appear initially at area of high stress, occur rarely at the strain gap, and their locations are finally in the zone between
the stress concentration area and the strain gap, which indicate the clusters or groups. However, the major macro fracture
(final rupture) started from the shadow areas, and then grew quickly towards the strain gaps, which resulted in failure of
sample.
Foundation item: The Dual Project of China Seismological Bureau (9691309020301), the Specialized Funds for National Key Basic Study (G1998040704),
the project for the MOST under contract (2001BA601B02) and Youth Funds for applied basic study of the Science and Technology
Bureau of Yunnan Province (98D019Q). 相似文献
87.
Introduction Greeting the coming of the 21st century, Professor HU Yu-xian and other Chinese scholars briefed the trend of earthquake engineering in China and aboard (HU, 1999; HU, ZHOU, 1999). The experiences and lessons learning from the destructive earthquakes in China and abroad in re-cent years, the damage action of the large velocity impulse in ground motion in near field in seis-mic design, numerous earthquake examples show that there are many weaknesses in aspects of earthquake p… 相似文献
88.
提出了融合多光谱影像、全色影像、DEM等多元遥感信息的断裂特征增强方法,建立了以地形和水体的空间特征变化为基础的断裂解译标志,解译并发现桂西北巴马-马山断裂带和右江断裂带之间存在一条北西向展布、长约40km的新的右江次级活动断裂,结合野外地震地质调查进行了验证。多元遥感信息融合处理中,将KL变换、HIS变换、乘积变换、比值变换、小波变换等融合方法进行了全面比较,对融合后影像进行主分量分析,确定了乘积变换融合的影像增强方法和解译底图,显著突出了活动断裂特征。 相似文献
89.
90.
基于线路设计模型的一体化中线测设方法研究 总被引:2,自引:0,他引:2
本文针对线路(包括铁路和公路)的中线测设计算量大、野外作业条件的不可预知性和劳动强度大等特点,介绍了一种基于线路设计模型的一体化中线测设的教学模型及方法,以此为基础开发了实用的中线放样程序并运用于我国第一条磁悬浮线───交大青城磁浮列车试验示范城的中经测设中,实践证明一体化的思想及方法具有高效、灵活和可靠性等特点。 相似文献