Results 201 to 210 of about 26,882 (267)

Seismic rehabilitation of steel buildings with semi-rigid connections under fifth generation of ETEF. [PDF]

Sci Rep
Majdi A, Sadeghi-Movahhed A, Alasiri MR, Islam S, Movahedi Rad M.   +4 more
europepmc   +1 more source

Introducing the inverted pendulum as a negative stiffness mechanism and a novel structural system to improve seismic performance using a quasi-zero stiffness approach. [PDF]

Sci Rep
Azizi A, Barghian M.
europepmc   +1 more source

Seismic Risk Analysis

Zisin (Journal of the Seismological Society of Japan. 2nd ser.), 1988
openaire   +2 more sources

Source-to-sink coupling and spatiotemporal evolution during multiphase rifting: The Jurassic-Cretaceous Lishu fault depression, Southeastern Songliao Basin. [PDF]

PLoS One
Wang K, Zhou Y, Yan J, Zhang Y.
europepmc   +1 more source

Mineralogical imprints of earthquake activity in sedimentary structures. [PDF]

Sci Rep
Świątek S, Lewińska K, Pisarska-Jamroży M, Günter C.   +3 more
europepmc   +1 more source

Fault-mediated magma propagation and triggered seismicity revealed by the 2022 São Jorge Azores unrest. [PDF]

Nat Commun
Hicks SP, Gonzalez PJ, Lomax A, Ferreira AMG, Ramalho RS, Mitchell NC, Silveira G, Dias NA, Fontiela J, Fernandes R, Custódio S, Tsekhmistrenko M, Mendes V, Pimentel A, Silva R, Prates G, Sturgeon W, Marignier A, Carrilho F, Marques R, Miranda M, Garcia AM.   +21 more
europepmc   +1 more source

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Probabilistic Seismic Hazard Analysis for Induced Seismicity

2014
Probabilistic Seismic Hazard Analysis is currently the most common approach to seismic hazard analysis. For application to induced seismicity, a major challenge is the fact that the hazard is inherently nonstationary. In this paper we describe the theoretical extension of PSHA to a non-stationary context.
Kraaijpoel D A, Caccavale M, Van Eck T, Dost B   +3 more
openaire   +2 more sources

Seismic Analysis

2021
An earthquake is caused by sudden motion of the earth's crust. Every year, tens of thousands of earthquakes of all sizes occur all over the world. Some cause tiny or major tremors, others occur in remote areas where no one lives. This chapter allow readers to find out more about the earth structure as well as earthquake nature. Therefore, to detail the
openaire   +1 more source

Seismic graph analysis to aid seismic interpretation

Interpretation, 2019
During the seismic interpretation process, geoscientists rely on their experience and visual analysis to assess the similarity between seismic sections. However, evaluating all of the seismic sections in a 3D survey can be a time-consuming task. When interpreters are working on a data set, a common procedure is to divide the cube in increasingly finer ...
Rodrigo S. Ferreira, Emilio Vital Brazil, Reinaldo Silva, Renato Cerqueira   +3 more
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Analysis of a Polarized Seismic Wave Model

IEEE Seventh SP Workshop on Statistical Signal and Array Processing, 1996
We present a model for polarized seismic waves where the data are collected by three-component geophone receivers. The model is based on two parameters describing the polarization properties of the waveforms. These parameters are the ellipticity and the orientation angle of the polarization ellipse.
Sören Anderson, Arye Nehorai
openaire   +1 more source