Results 141 to 150 of about 425 (169)
Tidal sensitivity of tectonic tremors and frictionally heterogeneous fault model
, 2017 openaire +1 more source
Variety and spatial heterogeneity of tectonic tremor worldwide [PDF]
Journal of Geophysical Research: Solid Earth, 2012 Deep tectonic tremor occurs at various sites worldwide, and the source characteristics are heterogeneous, even at small scales. In this study, tremor sources were determined using data sets of seismic waveforms from various locations, some of which are not well recognized as being a site of tremor activity.
Satoshi Ide
exaly +2 more sources
Crustal anisotropy from tectonic tremor in Guerrero, Mexico
Geochemistry, Geophysics, Geosystems, 2016 AbstractWe present new shear wave anisotropy measurements in the continental crust in northern Guerrero obtained from tectonic tremor. Measurements of crustal anisotropy had not been performed in this area due to the lack of seismicity. However, tectonic tremor activity is abundant and offers an opportunity to determine anisotropy parameters ...
Raul Valenzuela +2 more
exaly +2 more sources
Tectonic tremor and deep slow slip on the Alpine Fault [PDF]
Geophysical Research Letters, 2012 Tectonic tremor is characterized by persistent, low-frequency seismic energy seen at major plate boundaries. Although predominantly associated with subduction zones, tremor also occurs along the deep extension of the strike-slip San Andreas Fault.
John Townend, Aaron G. Wech
exaly +7 more sources
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Experimental constraints on the controlling mechanisms of tectonic tremors
2023Tectonic (or non-volcanic) tremors have been extensively documented at subduction zones and are considered as the signature of transport processes of dehydration-related fluids in subduction zones, often recorded in close association with geodetically observed shear induced slow-slip events. However, to the best of our knowledge, they have not yet been
Timm John +6 more
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Cataloging Tectonic Tremor Energy Radiation in the Cascadia Subduction Zone
Journal of Geophysical Research: Solid Earth, 2021AbstractFor the past ∼12 years the Pacific Northwest Seismic Network has been automatically detecting and locating tectonic tremor across the Cascadia subduction zone, resulting in a catalog of more than 500,000 tremor epicenters to date, which has served as a valuable resource for tremor and slip research.
Aaron G. Wech
exaly +2 more sources
Tectonic Tremor Recorded by Ocean Bottom Seismometers
Seismological Research Letters, 2013Widespread observations of tremor and slow slip in different tectonic environments (Rubinstein et al. , 2009; Schwartz and Rokosky, 2007) reveal that these newly recognized processes play fundamental roles in accommodating and marking fault motion. Understanding the relationship between fault dynamics, stable (slow) slip, and more rapid earthquake ...
Wech, A. +5 more
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Continental crust anisotropy measurements from tectonic tremor in Cascadia
Journal of Geophysical Research: Solid Earth, 2017AbstractWe present new observations of crustal anisotropy in the southern Cascadia fore arc from tectonic tremor. The abundance of tremor activity in Oregon and northern California during slow‐slip events offers an enormous amount of information with which to measure and analyze anisotropy in the upper brittle continental crust.
Raul Valenzuela +2 more
exaly +2 more sources
Investigation of Single-Station Classification for Short Tectonic Tremor in Taiwan
Journal of Geophysical Research: Solid Earth, 2019AbstractTectonic tremor in Taiwan is known for its short duration and weak amplitude. Recent observations from the mountain area (Central Range) allows us to document such type of tectonic tremor recorded at a close distance and to investigate a single station technique for a minute‐long tremor.
Yaochieh Chen +2 more
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Detecting Deep Tectonic Tremor in Taiwan with a Dense Array
Bulletin of the Seismological Society of America, 2015Abstract We perform a systematic detection of deep tectonic tremor beneath the southern Central Range in Taiwan using a dense, small‐aperture seismic array. Deployed in February 2011, the array has been recording tectonic tremor nearly continuously for 134 days, including tremor triggered by the 2011 M w 9.0 Tohoku‐Oki earthquake.
Wei‐Fang Sun +3 more
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