Results 191 to 200 of about 908 (240)

Application of Neural Network Automatic Event Detection for Reservoir-Triggered Seismicity Monitoring Networks. [PDF]

Sensors (Basel)
Wiszniowski J, Lizurek G, Tymińska A, Kucia P, Plesiewicz B.   +4 more
europepmc   +1 more source

Seismic imaging reveals a strain-partitioned sliver and nascent megathrust at an incipient subduction zone in the northeast Pacific. [PDF]

Sci Adv
Brandl CC, Worthington LL, Roland EC, Walton MAL, Nedimović MR, Gase AC, Adedeji O, Castellanos JC, Phrampus BJ, Bostock MG, Wang K, Oliva SJ.   +11 more
europepmc   +1 more source

Seismic source analysis of the destructive earthquake November 21, 2022, M_w 5.6 Cianjur (Indonesia) from relocated aftershock. [PDF]

Sci Rep
Zulfakriza Z, Nugraha AD, Heryandoko N, Ry RV, Muttaqy F, Andika A, Azhari MF, Putra AS, Palgunadi KH, Cummins PR, Supendi P, Lesmana A, Sahara DP, Puspito NT.   +13 more
europepmc   +1 more source

Variabilities of ground motion in 2023 M_w 7.8 Pazarcık earthquake in Turkey and 2008 M_w 7.9 Wenchuan earthquake in China. [PDF]

Sci Rep
Xu P, Liu X, Li L.
europepmc   +1 more source

Numerical simulation of crack propagation and AE precursor characteristics in coal failure under confining pressures. [PDF]

Sci Rep
Jing G, Wang S, Zhao L, Dong F, Fan Y.
europepmc   +1 more source

A New Catalogue and Insights into the 2022 Adriatic Offshore Seismic Sequence Using a Machine Learning-Based Procedure. [PDF]

Sensors (Basel)
Costanzo A.
europepmc   +1 more source

Direct evidence of active tectonics along the offshore sector of the Dinaric Fault System. [PDF]

Sci Rep
Korbar T, Hasan O, Brunović D, Markušić S, Alves T.   +4 more
europepmc   +1 more source

Coseismic deformation analysis of the 2017 Milin Ms 6.9 earthquake in the Namche Barwa Syntaxis: Implications for regional tectonics. [PDF]

Fundam Res
Wang J, Zhang S, Zhao Y, Cai F, Wang C, He J, Ding L.   +6 more
europepmc   +1 more source

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Seismic Source Radiation and Moment Tensor in the Time Domain

1997
Seismic waves in an elastic medium are produced by an inelastic deformation at the seismic source. Let us assume that the seismic source occupies the volume V, in which the body forces f are present, and in which the jump of displacement takes place on the surface Σ, composed of a positive side, Σ+, and a negative side, Σ−, with the unit vector, v ...
Mendecki A J
exaly   +2 more sources

Decomposition of seismic moment tensors for underground nuclear explosions

pure and applied geophysics, 1996
Generally the decomposition of a seismic moment tensor is not unique. However, to favorably view the characteristics of a certain seismic source, one must decompose a seismic moment tensor into parts according to assumptions about the properties of the seismic source.
Z. L. Wu, Y. T. Chen
openaire   +1 more source