Results 141 to 150 of about 6,766 (163)

Earthquake frequency-magnitude distribution at Mount Etna sheds light on magma ascent in the volcano's plumbing system. [PDF]

Sci Adv
Firetto Carlino M, Lo Bue R, Taroni M, Coltelli M, Cannavò F, Cocina O, Barberi G, Scarfì L.   +7 more
europepmc   +1 more source

Neurochagas: Experimental and human literature of an uncommon entity (Review). [PDF]

Med Int (Lond)
Rissardo JP, Ali HT, Byroju VV, Caprara ALF.   +3 more
europepmc   +1 more source

Multifunctional hydrogel sensors with dynamic covalent networks for machine learning-assisted Parkinson's disease diagnosis and encrypted human-computer interaction. [PDF]

Mater Today Bio
Ding S, Yu X, Wang Q, Luo P, Li H, Li Z, Wang R, Liu H, He Y, Nong J, Zhang C.   +10 more
europepmc   +1 more source

Basal Ganglia Intraparenchymal Cyst Revealed by a Movement Disorder. [PDF]

Cureus
Benyarou K, El Hasnaoui S, Yousfi S, Mebrouk Y.   +3 more
europepmc   +1 more source

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Complex Migration of Tremor Near Cholame, CA, Resolved by Seismic Array Analysis

Journal of Geophysical Research: Solid Earth, 2021
AbstractTectonic tremor observed along the Cholame and Parkfield sections of the San Andreas Fault has previously been associated with transient slip beneath the seismogenic zone. To study tremor and associated Low Frequency Earthquakes (LFEs), we deployed three dense near‐fault seismic arrays for a period of 3 months in 2018. In early August 2018, the
Amanda Thomas, Asaf Inbal, Tyler Newton   +2 more
exaly   +2 more sources

Striations, duration, migration and tidal response in deep tremor

Nature, 2010
Deep tremor in subduction zones is thought to be caused by small repeating shear slip events on the plate interface with significant slow components. It occurs at a depth of about 30 kilometres and provides valuable information on deep plate motion and shallow stress accumulation on the fault plane of megathrust earthquakes.
Satoshi Ide, Ide Satoshi
exaly   +3 more sources

Apparent migration of tremor source synchronized with the change in the tremor amplitude observed at Aso volcano, Japan

Journal of Volcanology and Geothermal Research, 2006
At Aso volcano, Kyushu, Japan, several different types of volcanic tremor have been observed for many years. One of them is the continuous tremor, the ground vibration which has dominant frequency between 3 and 10 Hz and has approximately constant amplitudes without any clear beginning and ending.
Hitoshi Kawakatsu, Takahiro Ohkura, Yasuaki Sudo   +2 more
exaly   +2 more sources

Fine Structure of Tremor Migrations Beneath the Kii Peninsula, Southwest Japan, Extracted With a Space‐Time Hough Transform

Journal of Geophysical Research: Solid Earth, 2022
Abstract Tectonic tremors occurring on subducting plate boundaries are known to migrate at various timescales and migration speeds. Spatiotemporal patterns of tremor migration are key to investigating the rupture growth of slow earthquakes.
Kodai Sagae, Hisashi Nakahara, Takeshi Nishimura, Kazutoshi Imanishi   +3 more
openaire   +1 more source