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seismic recorder

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  • Geophysical MASINT — is a branch of Measurement and Signature Intelligence (MASINT) that involves phenomena transmitted through the earth (ground, water, atmosphere) and manmade structures including emitted or reflected sounds, pressure waves, vibrations, and… …   Wikipedia

  • Халилов, Эльчин Нусрат оглы — Автобиография Эта статья представляет собой автобиографию или же её в значительном объёме редактирует герой статьи, либо связанная с ним организация, или другие заинтересованные лица. Возможно, статья не соответствует правилу о нейтральной точке… …   Википедия

  • earthquake — /errth kwayk /, n. 1. a series of vibrations induced in the earth s crust by the abrupt rupture and rebound of rocks in which elastic strain has been slowly accumulating. 2. something that is severely disruptive; upheaval. [1300 50; ME erthequake …   Universalium

  • Earth Sciences — ▪ 2009 Introduction Geology and Geochemistry       The theme of the 33rd International Geological Congress, which was held in Norway in August 2008, was “Earth System Science: Foundation for Sustainable Development.” It was attended by nearly… …   Universalium

  • Reflection seismology — (or seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth s subsurface from reflected seismic waves. The method requires a controlled seismic source of energy,… …   Wikipedia

  • Nigel Anstey — Nigel Allister Anstey, British geophysicist, has made major contributions to seismic exploration, which are the foundations for many of the techniques used in today’s oil and gas exploration. Anstey’s contributions impact every major area of… …   Wikipedia

  • Seismometer — Seismometers (from Greek Seism the shakes and Metro I measure ) are instruments that measure and record motions of the ground, including those of seismic waves generated by earthquakes, nuclear explosions, and other seismic sources. Records of… …   Wikipedia

  • Geophysical migration — of seismic data is the correction of the flat geological layer assumption by a numerical, grid based spatial convolution of the seismic data to account for dipping events (where geological layers are not flat). There are many approaches, such as… …   Wikipedia

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