Zobrazeno 1 - 10
of 58
pro vyhledávání: '"Xuzhang, Shen"'
Publikováno v:
地震科学进展, Vol 54, Iss 1, Pp 65-74 (2024)
The 1∶500000 seismotectonic map of the Ordos active block and boundary zone is a special achievement of the national key research and development project “Research on dynamic model and strong earthquake risk of Ordos active block boundary zone”
Externí odkaz:
https://doaj.org/article/31fd31d6daf64de0b092588148bd653f
Publikováno v:
Geoscience Frontiers, Vol 14, Iss 1, Pp 101482- (2023)
The Cathaysia block located at the southeast South China block (SCB) is considered formed by the amalgamation of the east and west Cathaysia blocks along the Gaoyao–Huilai and Zhenghe–Dapu deep faults (here referred as GHF and ZDF, respectively).
Externí odkaz:
https://doaj.org/article/df4e7d8b1962431d960973fe34853733
Publikováno v:
Earth, Planets and Space, Vol 73, Iss 1, Pp 1-14 (2021)
Abstract The Shanxi Rift located in the central part of the North China Craton (NCC) as a boundary between the Ordos block and the Huabei basin. The Shanxi graben system is a Cenozoic rift and originated from back-arc spreading related to westward su
Externí odkaz:
https://doaj.org/article/8d3b4d11c7c34392b23ef402bac060b2
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The North China Craton (NCC) is one of the oldest cratons in the world, and its internal tectonic belt is often used to investigate the earth’s tectonic evolution events. During the late Mesozoic and Cenozoic, the western Pacific subduction zone ca
Externí odkaz:
https://doaj.org/article/86a89d13c8044e80bda3dde6e6d698b7
Publikováno v:
地震科学进展, Vol 50, Iss 4, Pp 1-21 (2020)
The Ordos active block and its surrounding areas are ideal to examine and develop the active block theory on geodynamics and seismic hazards. In recent years, research on geodynamics of the Tibetan Plateau has become a new hotspot in geoscience both
Externí odkaz:
https://doaj.org/article/7dc4cc92983849eaad90c9116424180c
Autor:
Jinyu Lv, Xuzhang Shen, Liuting Huang, Xiaohui He, He Huang, Wenjun Zheng, Dongli Zhang, Jian Zhang
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 7, Pp n/a-n/a (2021)
Abstract Based on the teleseismic records of the dense broadband seismic array, the crustal anisotropy parameters of the west Ordos block and its adjacent regions were determined with P wave receiver functions. The results indicate that the dominant
Externí odkaz:
https://doaj.org/article/093adee9799f480194b0b0f64aa1f06d
Publikováno v:
Remote Sensing, Vol 14, Iss 12, p 2760 (2022)
As a traditional method, passive seismic exploration is used to construct the body-wave velocity structure of the upper crust, but it is cost-ineffective and depth-limited when applied to large areas. In this study, we use another more economical met
Externí odkaz:
https://doaj.org/article/cff54b47fb0441e8b92f9b4995599e0b
Publikováno v:
Remote Sensing, Vol 13, Iss 15, p 2957 (2021)
A directional borehole radar consists of one transmitting antenna in the borehole and four receiving antennas distributed at equal angles in a ring. The receiving antennas can determine the depth and orientation of targets beside the borehole. Howeve
Externí odkaz:
https://doaj.org/article/b90b740576354f66aac0b5b649281296
Publikováno v:
Gondwana Research. 106:224-236
Publikováno v:
Sensors, Vol 20, Iss 20, p 5812 (2020)
The directional borehole radar can accurately locate and image the geological target around the borehole, which overcomes the shortcomings that the conventional borehole radar can only detect the depth of the target and the distance from the borehole
Externí odkaz:
https://doaj.org/article/de45b9ccc5a64e6298a61e862fddd5e5