Gravity-induced seismicity modulation on planetary bodies and their natural satellites. [PDF]
Senapati B, Kundu B, Jha B, Jin S.
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Subduction intraslab-interface fault interactions in the 2022 Mw 6.4 Ferndale, California, earthquake sequence. [PDF]
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Global subduction slow slip events and associated earthquakes. [PDF]
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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.
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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.
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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
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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 ...
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