2023
DOI: 10.1007/s11440-023-01881-w
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Seismic response and deformation mechanism of near-fault deep tunnels in a strong earthquake area

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Cited by 11 publications
(6 citation statements)
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“…The results of the best-fit model indicate that the LHSF is controlled by a left-lateral strike-slip at a rate of ~3.5 mm/yr, which is consistent with geology [11] and geodesy [12,15,17,18,24], approaching the result of 4.1 ± 0.4 mm/yr [21]. The HYF is controlled by a left-lateral strike-slip at a rate of 2.8-3.3 mm/yr, and the average rate is about 3 mm/yr, which is close to the results of 3.3-9.2 mm/yr obtained by geology [7] and 4.5 ± 1.1 mm/yr [11], is close to the GPS, InSAR, and other geodetic methods [12,15,17,18,23,24], and is also consistent with the rates of 3.9 ± 0.4 mm/yr, 3.7 ± 0.4 mm/yr, and 3.6 ± 0.4 mm/yr for the western, middle, and eastern sections of the HYF [21]. The average contraction rate is 0.6 mm/yr, and the maximum rate is 1.4 mm/yr in the middle of the fault.…”
Section: Fault Slip Ratesupporting
confidence: 70%
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“…The results of the best-fit model indicate that the LHSF is controlled by a left-lateral strike-slip at a rate of ~3.5 mm/yr, which is consistent with geology [11] and geodesy [12,15,17,18,24], approaching the result of 4.1 ± 0.4 mm/yr [21]. The HYF is controlled by a left-lateral strike-slip at a rate of 2.8-3.3 mm/yr, and the average rate is about 3 mm/yr, which is close to the results of 3.3-9.2 mm/yr obtained by geology [7] and 4.5 ± 1.1 mm/yr [11], is close to the GPS, InSAR, and other geodetic methods [12,15,17,18,23,24], and is also consistent with the rates of 3.9 ± 0.4 mm/yr, 3.7 ± 0.4 mm/yr, and 3.6 ± 0.4 mm/yr for the western, middle, and eastern sections of the HYF [21]. The average contraction rate is 0.6 mm/yr, and the maximum rate is 1.4 mm/yr in the middle of the fault.…”
Section: Fault Slip Ratesupporting
confidence: 70%
“…In order to obtain a more accurate crustal deformation pattern of the faults on the northeastern corner of the Tibetan Plateau, this paper integrated the observations from encrypted GPS stations around the Haiyuan-Liupanshan fault zone, with the GPS observations on the northeastern margin of the Tibetan Plateau from 2010 to 2020, based on the block-fault back-slip dislocation model to obtain the locking depth, slip rate deficit distribution, and motion characteristics of the faults. 5.8 [11] 4.5 ± 1.1 [12] 3.4 ± 0.2 [13] 8.25 5.49 5.97 [14] 6.5 4.5 5.6 5.5 [15] 2-4.5 [16] 4.6-4.7 [17] 2-5.5 1.0 Terrestrial [18] 2.9-5.9 measurement [19] 5.4 ± 0.1 5.0 ± 0.…”
Section: Introductionmentioning
confidence: 99%
“…The original gauge length, L 0 , can be calculated using Equation (1), where k is the proportion coefficient.…”
Section: Design Of Test Specimensmentioning
confidence: 99%
“…In addition to various advantages, large-span spatial structures also have characteristics such as a frequency density, complex vibration modes, and significant spatial effects in terms of earthquake action [1]. The seismic response of large-span spatial structures is complex, and seismic damage events are often reported [2].…”
Section: Introductionmentioning
confidence: 99%
“…As urban construction continues to develop, the utilization of underground space has attracted widespread attention. In urban engineering construction, the existence of special geological environments, such as active fault zones and fault slippage, has caused serious damage and threats to engineering [1][2][3][4] . The existence of fault slippage not only causes damage to engineering structures such as cross-fault buildings and underground engineering structures, but also poses a serious threat to the structural engineering in its affected area [5][6][7][8][9] .…”
mentioning
confidence: 99%