Results 261 to 270 of about 120,186 (297)

Focal mechanism solutions and nature of plate movements in Pakistan

Journal of Geodynamics, 1986
Abstract From the seismic point of view, the territory of Pakistan which lies between latitude 23°–37° N and longitude 61°–75° E is one of the most active zones in the world. The importance of this area lies in terms of movements of the Indian plate with respect to Eurasia on the west.
R.K. Verma, Ch. Chandra Sekhar
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Focal mechanism solutions for earthquakes in Iran

Physics of the Earth and Planetary Interiors, 1984
Abstract Focal mechanism solutions, derived by using P-wave first motion directions read from seismograms of Worldwide Standardized Stations Network (WWSSN), are presented for 36 earthquakes in Iran. In many cases the first motion data admit more than one solution.
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FOCAL MECHANISM SOLUTION OF THE 15TH MARCH 2008, NYAMANDLOVU EARTHQUAKE

South African Journal of Geology, 2009
The focal mechanism solution of the 15th March 2008 earthquake (mb = 4.3) that occurred in the Nyamandlovu area, northwest of Bulawayo City, Zimbabwe, has been determined from P-wave first motion polarities. Results show normal oblique left lateral faulting. The earthquake mechanism bears a signature that is almost identical to those of events recorded
B. T. SHUMBA, D. J. HLATYWAYO, V. MIDZI
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A comparison of multiple solutions of focal mechanisms

Bulletin of the Seismological Society of America, 1964
Abstract The occurrence of focal mechanism solutions of the same earthquake by different authors is examined. Of 42 instances of such multiple solutions for earthquakes which occurred around the borders of the Pacific Ocean, it is found that of 84 possible pairs of multiple solutions agreement is excellent in 8 cases, good in 13, fair in
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Focal Mechanism Solutions of Intraplate Earthquakes and Stresses in the Lithosphere

1974
Focal mechanism solutions of 33 intraplate earthquakes are presented. These solutions, 47 additional mechanism solutions from the literature, and measurements of stress in situ indicate that the interiors of many lithospheric plates are characterized by large horizontal compressive stress. The predominance of com-pressive stress is particularly notable
Lynn R. Sykes, Marc L. Sbar
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Two focal-mechanism solutions for earthquakes from Iceland and Svalbard

Tectonophysics, 1977
Abstract Strike-slip solutions have been obtained and are presented here for the focal mechanisms of one earthquake from Iceland and one from Svalbard, on 13 and 18 January 1976, respectively. A fault plane is suggested for the Iceland earthquake.
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Focal mechanism solutions and dynamic parameters of earthquakes in the eastern Himalayas and northern Burma

Tectonophysics, 1983
Abstract Focal-mechanism solutions of four earthquakes in the eastern Himalayas and northern Burma are determined using the first motion of compressional waves. Two possible solutions thus obtained for each event reveal steeply dipping fault with predominantly strike-slip motion.
S.K. Upadhyay, V.K. Ahuja, V.Sri Ram
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Focal mechanism solution of the Himalayan earthquake of February 14, 1977

Tectonophysics, 1982
Abstract Through a closely spaced local network of seismic stations in Himachal Pradesh, India, supplemented by worldwide P-wave first-motion data, the source mechanism of the February 14, 1977 earthquake which occurred very close to the Rawalpindi area in Pakistan has been determined.
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Focal mechanism solutions for Albanian earthquakes for the years 1964–1988

Tectonophysics, 1994
Abstract Focal mechanism solutions for 175 Albanian earthquakes of Albania for the years 1964–1988 were obtained by using an interactive computer technique. The results obtained are elaborated upon by applying Fisherian statistical analysis to obtain parameters for the mean stress direction in five zones.
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Modern tectonic stress field in the Chinese mainland inverted from focal mechanism solutions

Acta Seismologica Sinica, 1999
The inversion of modern tectonic stress field in China is made by regions on the basis of focal mechanism data in the period of 1920–1996. Results of the inversion show that the maximum principal compressive stress σ1 axis strikes nearly north-south direction in the Tibet Plateau and western China, east-west direction in North China.
Xing-Xin Du, Hui-Cheng Shao
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