Results 241 to 250 of about 152,674 (295)

On monitoring of seismic activity

The Journal of Zhytomyr State Technological University. Series: Engineering, 2018
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Enhancing the resolution of microseismicity through dense array monitoring in complex extensional settings. [PDF]

Sci Rep
Scotto di Uccio F, Muzellec T, Scala A, De Landro G, Camanni G, Carotenuto F, Elia L, Picozzi M, Zollo A, Strumia C, Beroza GC, Festa G.   +11 more
europepmc   +1 more source

Long period quakes linked to Mefite D'Ansanto (Italy) mantellic CO₂ emissions. [PDF]

Sci Rep
Cusano P, Morabito S, Petrosino S, Nardone L.   +3 more
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Mechanisms of seismic improvement in pile-sheet wall supported slopes using ECC and anchor cables. [PDF]

Sci Rep
Wang R, Shen J, Ding X, Wang C, Ma D, Li Y.   +5 more
europepmc   +1 more source

Seizing opportunities and navigating the challenges of spaceflight research as an early career researcher

Experimental Physiology, EarlyView.
Colleen S. Deane
wiley   +1 more source

Life on Mars? The physiological perspective

Experimental Physiology, EarlyView.
Ronan M. G. Berg, Damian M. Bailey
wiley   +1 more source

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On seismic activity

pure and applied geophysics, 1966
Seismic activity at a point of the surface of the earth up to a given time has to be computed by the total energy per unit area at the point considered in consequence of the earthquakes up to that time. The definition of seismic activity of a region can be developed from that. Seismic activity in a given time-interval results from earthquakes up to the
Wolfgang Ullmann, Richard Maaz
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Apollo 14 Active Seismic Experiment

Science, 1972
Explosion seismic refraction data indicate that the lunar near-surface rocks at the Apollo 14 site consist of a regolith 8.5 meters thick and characterized by a compressional wave velocity of 104 meters per second. The regolith is underlain by a layer with a compressional wave velocity of 299 meters per second.
J S, Watkins, R L, Kovach
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Investigation of Seismic Activity

2012
The Caucasus is one of the most active segments of the Alpine-Himalayan seismic belt (Khain 2000). The Caucasian region is characterized by intensive deformation and seismicity that accommodates the continental shortening between the Eurasian and Arabian plates, which are converging at a rate of about 30 mm/year (De Mets et al. 1990; Jackson 1992). The
Lev Eppelbaum, Boris Khesin
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Active seismic imaging using microseismic events

SEG Technical Program Expanded Abstracts 2009, 2009
Summary The analysis and interpretation of microseismic data sets are receiving increased attention, both in the exploration industry for the characterization of hydrocarbon and geothermal reservoirs as well as in academia for the general understanding of seismogenic processes at plate boundaries.
A. Reshetnikov, S. Buske, S. Shapiro
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