Javascript must be enabled to continue!
Earthquake Risk Probability Evaluation for Najin Lhasa in Southern Tibet
View through CrossRef
The probabilistic seismic hazard analysis (PSHA) method is effectively used in an earthquake risk probability evaluation in seismogenic regions with active faults. In this study, by focusing on the potential seismic source area in Najin Lhasa, southern Tibet, and by incorporating the PSHA method, we determined the seismic activity parameters and discussed the relationship of ground motion attenuation, the seismic hazard probability, and the horizontal bedrock ground motion acceleration peak value under different transcendence probabilities in this area. The calculation results show that the PSHA method divides the potential source area via specific tectonic scales and detailed tectonic markers, which reduces the scale of the potential source area and better reflects the uneven spatial distribution of seismic activity in the vicinity of Najin. The corrected attenuation relationship is also in line with the actual work requirements and is suitable for earthquake risk analysis. In addition, the major influences on the peak acceleration of ground motion in the study area are mainly in the potential source areas of Qushui (M7.5), Dangxiong (M8.5), and Kangma (M7.5). The peak horizontal ground motion acceleration (PGA) with a transcendence probability of 10% in 50 years is 185.9 cm/s2, and that with a transcendence probability of 2% in 50 years is 265.9 cm/s2.
Title: Earthquake Risk Probability Evaluation for Najin Lhasa in Southern Tibet
Description:
The probabilistic seismic hazard analysis (PSHA) method is effectively used in an earthquake risk probability evaluation in seismogenic regions with active faults.
In this study, by focusing on the potential seismic source area in Najin Lhasa, southern Tibet, and by incorporating the PSHA method, we determined the seismic activity parameters and discussed the relationship of ground motion attenuation, the seismic hazard probability, and the horizontal bedrock ground motion acceleration peak value under different transcendence probabilities in this area.
The calculation results show that the PSHA method divides the potential source area via specific tectonic scales and detailed tectonic markers, which reduces the scale of the potential source area and better reflects the uneven spatial distribution of seismic activity in the vicinity of Najin.
The corrected attenuation relationship is also in line with the actual work requirements and is suitable for earthquake risk analysis.
In addition, the major influences on the peak acceleration of ground motion in the study area are mainly in the potential source areas of Qushui (M7.
5), Dangxiong (M8.
5), and Kangma (M7.
5).
The peak horizontal ground motion acceleration (PGA) with a transcendence probability of 10% in 50 years is 185.
9 cm/s2, and that with a transcendence probability of 2% in 50 years is 265.
9 cm/s2.
Related Results
Volcanic rocks of the 1985 Tibet Geotraverse: Lhasa to Golmud
Volcanic rocks of the 1985 Tibet Geotraverse: Lhasa to Golmud
Abstract
Volcanic rocks encountered during the Tibet Geotraverse have been studied in the field, in thin section and by major and trace element geochemistry in or...
Using satellite soil moisture and rainfall in the Landslide Hazard Assessment for Situational Awareness system
Using satellite soil moisture and rainfall in the Landslide Hazard Assessment for Situational Awareness system
<p>The Landslide Hazard Assessment for Situational Awareness system (LHASA) gives a global view of landslide hazard in nearly real time. Currently, it is being upgrad...
Unexpectedly high concentrations of atmospheric mercury species in Lhasa, the largest city on the Tibetan Plateau
Unexpectedly high concentrations of atmospheric mercury species in Lhasa, the largest city on the Tibetan Plateau
Abstract. Lhasa City is located in the central Tibetan Plateau and is the most densely populated area. As the first continuous monitoring of atmospheric mercury (Hg) species in a c...
Zircon U–Pb dating, geochemistry, and Sr–Nd–Pb–Hf isotopes of the subvolcanic intrusion from Beina Pb–Zn–(Ag) deposit in the southern Lhasa terrane, Tibet: Implications for petrogenesis and mineralization
Zircon U–Pb dating, geochemistry, and Sr–Nd–Pb–Hf isotopes of the subvolcanic intrusion from Beina Pb–Zn–(Ag) deposit in the southern Lhasa terrane, Tibet: Implications for petrogenesis and mineralization
The Beina Pb–Zn–(Ag) deposit is a newly discovered deposit situated in the southern Lhasa terrane, Tibet. LA‐ICP‐MS U–Pb dating for the ore‐bearing rhyolite porphyry indicates that...
Compositional and tectonomagmatic evolution of Early Cretaceous magmatism in the central Lhasa suberrane, Tibet: Implications from the Zenong Group volcanic rocks
Compositional and tectonomagmatic evolution of Early Cretaceous magmatism in the central Lhasa suberrane, Tibet: Implications from the Zenong Group volcanic rocks
The Lhasa Terrane in southern Tibet is widely recognized as having separated from the northern margin of Gondwana with a Precambrian basement and undergoing a pro...
Simulating Reservoir Induced Lhasa Streamflow Variability Using ArcSWAT
Simulating Reservoir Induced Lhasa Streamflow Variability Using ArcSWAT
Lhasa River Basin being the socio-economic hotspot of Qinghai-Tibetan Plateau is experiencing an increased hydropower capacity in the form of damming and reservoir construction. Th...
Towards A Global Landslide Forecast
Towards A Global Landslide Forecast
<p>Numerical weather models are used in a variety of applications, including a growing body of landslide hazard assessment models. Heretofore, these applications have...
Indosinian Orogenesis in the Lhasa Terrane, Tibet: New Muscovite 40Ar‐39Ar Geochronology and Evolutionary Process
Indosinian Orogenesis in the Lhasa Terrane, Tibet: New Muscovite 40Ar‐39Ar Geochronology and Evolutionary Process
AbstractMuscovite 40Ar‐39Ar dating of muscovite‐quartz schist, eclogite and retrograde eclogite indicates an Indosinian orogenesis occurred at 220–240 Ma in the Lhasa terrane, whic...

