Results 71 to 80 of about 793 (206)
Evidence for fluid-assisted shear failure in a ductile shear zone: tectonic tremor in the geologic record? [PDF]
Includes bibliographical references.2015 Summer.Recent direct observations of tectonic tremor below the seismogenic zone of large fault zones have emphasized the significance of coeval ductile and brittle processes at high temperatures.
Compton, Katharine, author +3 more
core
Tectonic Tremor Explained by Successive Ruptures of Clustered Quartz‐Filled Shear Veins
A tectonic tremor is a successive seismic signal observed along plate boundaries in subduction zones. However, the source processes and mechanisms responsible for the tremor remain unclear. Quartz‐filled shear and extension veins are clustered in tens to
S. Yabe, K. Ujiie
doaj +1 more source
Aeromagnetic mapping of fault architecture along Lagos–Ore axis, southwestern Nigeria
A seismic wave is released when there is sudden displacement on a fault plane. The passage of this wave along the fault plane or within the lithosphere could result in ground shaking or vibration at the surface of the Earth.
Oladejo Olagoke Peter +5 more
doaj +1 more source
Abstract The seismic behavior of subduction megathrusts varies spatially and is influenced by the properties of subducting plates, including their sedimentary cover. Characterizing these subduction inputs is essential for understanding the mechanisms behind fault slip variability.
Philip M. Barnes +12 more
wiley +1 more source
Tectonic tremors are key indicators of slow-slip phenomena, and detecting them accurately is a challenging task. Conventional techniques often fail to detect tremors during periods of intense tremor activity.
Yuya Jinde +2 more
doaj +1 more source
Off Cape Muroto area, along the Nankai Trough in southwest Japan, is a typical area with adjacent occurrences of slow and megathrust earthquakes. High‐resolution monitoring of slow earthquakes is necessary to understand tectonic conditions.
Satoru Baba +7 more
doaj +1 more source
Abstract Deformation along oceanic transform faults is partitioned between seismic and aseismic slip, controlled by lithology, thermal structure, and fluid circulation. We analyze one year of data from a 54‐station ocean bottom seismometer network deployed across the Blanco Transform Fault (BTF), Northeast Pacific.
Cyril Journeau +5 more
wiley +1 more source
Does deep tectonic tremor occur in the central-eastern Mediterranean basin?
Tectonic tremor has been observed at the roots of many fault systems around the Pacific rim, including convergent and transform plate boundaries.
Harrington, Rebecca M. (Prof. Dr.) +3 more
core
Defining the Relationship between Seismicity and Deformation at Regional and Local Scales [PDF]
In this thesis, I use source inversion methods to improve understanding of crustal deformation along the Nyainquentanglha (NQTL) Detachment in Southern Tibet and the Piceance Basin in northwestern Colorado.
Williams, Nneka Njeri Akosua
core +1 more source
Additional file 1 of Harmonic tremor from the deep part of Hakone volcano
Additional file 1: Figure S1. Particle motions on the horizontal plane during the main volcanic tremor (03:25–03:45). (a) The vertical waveform at the N.ASGH stations.
Yohei Yukutake (13842168) +3 more
core +1 more source

