Comprehensive Seismicity, Seismic Sources and Seismic Hazard Assessment of Assam, North East India

2018 ◽  
Vol 24 (2) ◽  
pp. 254-297 ◽  
Author(s):  
Ashish Bahuguna ◽  
Arjun Sil
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Seismic Sources ◽  
North East India ◽  
North East

Seismic sources for southern Pakistan and seismic hazard assessment of Karachi

2019 ◽  
Vol 99 (1) ◽  
pp. 511-536 ◽  
Author(s):  
Muhammad Waseem ◽  
Muhammad Asif Khan ◽  
Sarfraz Khan
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Seismic Sources

Seismic Hazard Assessment at Esfaraen‒Bojnurd Railway, North‒East of Iran

Geotectonics ◽  
2018 ◽  
Vol 52 (1) ◽  
pp. 151-156 ◽  
Author(s):  
S. Haerifard ◽  
H. Jarahi ◽  
M. Pourkermani ◽  
M. Almasian
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
North East ◽  
East Of Iran

Seismic Hazard Assessment of the City of Khoy and Its Vicinity, NW of Iran

2015 ◽  
Vol 6 (1) ◽  
pp. 15-27
Author(s):  
Davood Fereidooni
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Seismic Sources ◽  
Occurrence Probability ◽  
Hazard Parameters ◽  
The City ◽  
Seismic Hazard Parameters ◽  
Earthquake Data

Analyses have been carried out considering the occurred earthquakes, geologic and seismotectonic conditions of the region covering a radius of 100 Km keeping Khoy as the center. The major seismic sources are small and large faults identified in the study area mostly directed in NW-SE. The MCE and PGA were measured based on both DSHA and PSHA approaches. The results of DSHA show that the MCE and PGA evaluated values are 6.8 Richter and 0.31g, which might be created by Chahar-Sotoon and Askar-Abad faults, respectively. The results of PSHA show that the MCE evaluated value is 6.1 Richter for a 0.64 probability in a 50- year period. Seismic hazard parameters have been evaluated considering the available earthquake data using Gutenberg-Richter relationship method. The ‘a' and ‘b' parameters were estimated 6.03 and 0.94, respectively. For earthquakes with magnitudes equal or greater than 6.1 Richter, the values of returning period (TR) and annual occurrence probability (PT) were obtained 112 and 0.009, respectively. The results obtained from two mentioned methods are matched to each other.

Probabilistic seismic hazard assessment for the main cities along the continental section of the Cameroon volcanic line

2021 ◽  
Vol 14 (9) ◽  
Author(s):  
Etoundi Delair Dieudonné Ndibi ◽  
Eddy Ferdinand Mbossi ◽  
Nguet Pauline Wokwenmendam ◽  
Bekoa Ateba ◽  
Théophile Ndougsa-Mbarga
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Probabilistic Seismic Hazard Assessment ◽  
Probabilistic Seismic Hazard ◽  
Cameroon Volcanic Line

Probabilistic Seismic-Hazard Assessment in Quito, Estimates and Uncertainties

2014 ◽  
Vol 85 (6) ◽  
pp. 1316-1327 ◽  
Author(s):  
C. Beauval ◽  
H. Yepes ◽  
L. Audin ◽  
A. Alvarado ◽  
J.-M. Nocquet ◽  
...  
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Probabilistic Seismic Hazard Assessment ◽  
Probabilistic Seismic Hazard

Seismic hazard assessment using intensity point data

1994 ◽  
Vol 13 (3) ◽  
pp. 219-226 ◽  
Author(s):  
G. Monachesi ◽  
L. Peruzza ◽  
D. Slejko ◽  
M. Stucchi
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Point Data

scholarly journals Preliminary Seismic Hazard Assessment of the Oral and Dental Hospital of Jenderal Soedirman University Indonesia

2017 ◽  
Vol 171 ◽  
pp. 1025-1034 ◽  
Author(s):  
Yanuar Haryanto ◽  
Gathot Heri Sudibyo ◽  
Fransisca Cynthia Angelina Effendi
Keyword(s):  
Seismic Hazard ◽  
Hazard Assessment ◽  
Seismic Hazard Assessment ◽  
Dental Hospital
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