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Insights from scaled analogue modelling into the seismotectonics of the Iranian region
We show how analogue modelling provides insights into complex crustal block kinematics and the seismotectonics of active areas undergoing contraction, such as the Iranian region. The seismotectonic model deriving from this analysis is consistent with
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Tectonophysics, 1998
Abstract Instrumental seismic activity in Madagascar over a 16-years period, as well as the largest earthquakes experienced over the last century, are studied using seismic signal recordings and the archives of the Antananarivo Geophysical Observatory (Institut et Observatoire de Geophysique d'Antananarivo).
Didier Bertil, Jean Marc Regnoult
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Abstract Instrumental seismic activity in Madagascar over a 16-years period, as well as the largest earthquakes experienced over the last century, are studied using seismic signal recordings and the archives of the Antananarivo Geophysical Observatory (Institut et Observatoire de Geophysique d'Antananarivo).
Didier Bertil, Jean Marc Regnoult
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Tectonophysics, 1986
Abstract High-quality seismicity data and focal mechanism solutions obtained during 1973–1983 by the permanent Taiwan Telemetered Seismographic Network and several temporary local seismographic networks are used for a detailed study of the seismotectonics of the Taiwan area.
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Abstract High-quality seismicity data and focal mechanism solutions obtained during 1973–1983 by the permanent Taiwan Telemetered Seismographic Network and several temporary local seismographic networks are used for a detailed study of the seismotectonics of the Taiwan area.
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Seismotectonics of Sulawesi, Indonesia
Tectonophysics, 2023In eastern Indonesia, Sulawesi Island lies at the triple junction of the Australian, Sunda, and Phillippine Sea plates. The distinctive K-shape of Sulawesi, consisting of four arms (North, South, East, and Southeast), resulted from continuous geological evolution at different stages. Consequently, each arm has a different deformation style and tectonic
Yopi Serhalawan, Po-Fei Chen
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pure and applied geophysics, 1970
Elastic strain rebound increments for the Hindukush region has been studiedwhich revealed a cyclic pattern of strain release in this area where the rate of strain release decreases with time. The spatial distribution of earthquakes clearly defines the Pamir knot where most of the shocks are concentrated.
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Elastic strain rebound increments for the Hindukush region has been studiedwhich revealed a cyclic pattern of strain release in this area where the rate of strain release decreases with time. The spatial distribution of earthquakes clearly defines the Pamir knot where most of the shocks are concentrated.
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Seismotectonics and Earth tides
Russian Journal of Pacific Geology, 2012The results of the processing and analysis of the global earthquake distribution (more than 250000 events based on the ISC catalog) and the study of moonquakes distribution (about 900 events based on the published materials) are presented. It was found that the number of events and the energy for both cases show a bimodal distribution with maximums in ...
B. W. Levin, E. V. Sasorova
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