Crustal structure of northeastern Tibet inferred from receiver function analysis

Sponsored by National Science & Technology Committee, the cooperation between China Academy of Geoscience and Institute of Geophysics and Tectonics, University Joseph, France conducted a lithospherical experiment using 40 Minititan 3-component and 13 CEIS 1-component seismometers along the road from Gonghe to Yushu in Qinghai Province during 5 months after June, 1998. The interested area is on the north of Bangong- Nujiang fault, the east of Qaidam basin, the south of Center Qilian fault and the west of Longmenshan fault. And the profile across most tectonic parts of Eastern Tibet such as Southern Qilian, Eastern Kunlun fault, Bayan Har terrane, Jinshajiang suture (Figure 1), which is the first seismological profile across Eastern Tibet (Qinghai-Tibet) and will be beneficial on the comparison with the results of its center parts, especially on the understanding of the effect of the thousands-kilometer-faraway collision between Eurasia Plate and Indian Plate on the uplifting of south and north part of Eastern Kunlun fault, and on the thickening of crust and the feature of deep structure of Qilian mountain on the north of Tibet Plateau.     

多通道时间传递接收机NTSCGPS-1的研制与测试

近20年来，GPS共视(GPS CV)技术作为一种主要技术被用于TAI时间比对。GPS时间传递接收机是进行GPSCV时间比对的主要设备。介绍了中科院国家授时中心采用Motorola VP Oncore GPS OEM板、GT200计数器研发的高精度、多通道GIPS时间传递接收机NTscGPS-1的原理和特点。并通过实际观测数据分析，认为NTSCGPS-1的观测噪声水平与其它时间传递接收机相当，并有较好的兼客性。     

GPS信号多路径分析与处理技术

描述了GPS信号传输过程中的多路径问题，分析了多路径产生测量误差的机理，给出了多路径消除的处理技术，包括空间域和时间域的最新方法，指出了未来多路径问题需要重点关注，尤其是对高精度卫星导航应用领域。     

GPS共视接收机短期观测资料处理算法研究

提出了一种新的基于总体最小二乘数据拟合的短期观测资料处理算法 ,同时考虑测量时刻和时差测量值的不确定性 ,可提高共视接收机输出的单站数据精度。超短基线单通道共视测量数据表明 ,使用新算法后 ,可以提高原始共视数据短期稳定度     

一个用于GPS数据操作的实用软件

介绍了一个简单实用的GPS工具软件，描述了针对不同型号的接收机，可以完成数据的标准RINEX格式转换、数据质量检查和编辑工作，尤其数据质量检查的结果对了解接收机性能和数据环境等具有一定的指导作用。     

Dislocation structure of the crust-mantle boundary and low-velocity body within the crust beneath the Dabie Shan collision orogen

The Dabie Shan is located on the eastern side of the Qinling-Dabie orogenic belt, which marks a geological boundary between the Sino-Korean and Yangtze cra- ton. Since the 1980s, the discovery of coesite and mi- crodiamond in the Dabie Shan orogen motivates an extensive interest to the ultra-high pressure (UHP)metamorphism and its exhumation[1,2]. Many results about them were published, which deal with different disciplines, including tectonics, petrology and chro- nology[3?8]. Up to now,…     

The crustal structure of the eastern Marmara region, Turkey by teleseismic receiver functions

We study the crustal structure of eastern Marmara region by applying the receiver function method to the data obtained from the 11 broad-band stations that have been in operation since the 1999 İzmit earthquake. The stacked single-event receiver functions were modelled by an inversion algorithm based on a five-layered crustal velocity model to reveal the first-order shear-velocity discontinuities with a minimum degree of trade-off. We observe crustal thickening from west (29–32 km) to east (34–35 km) along the North Anatolian Fault Zone (NAFZ), but we observe no obvious crustal thickness variation from north to south while crossing the NAFZ. The crust is thinnest beneath station TER (29 km), located near the Black Sea coast in the west and thickest beneath station TAR (35 km), located inland in the southeast. The average crustal thickness and S -wave velocity for the whole regions are  31 ± 2  km and  3.64 ± 0.15 km s⁻¹  , respectively. The eastern Marmara region with its average crustal thickness, high heat flow value (101 ± 11 mW m⁻²) and with its remarkable extensional features seems to have a Basin and Range type characteristics, but the higher average shear velocities (∼3.64 km s⁻¹) and crustal thickening from 29 to 35 km towards the easternmost stations indicate that the crustal structure shows a transitional tectonic regime. Therefore, we conclude that the eastern Marmara region seems to be a transition zone between the Marmara Sea extensional domain and the continental Anatolian inland region.