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IODP Expedition 340T: Borehole Logging at Atlantis Massif Oceanic
IODP Expedition 340T: Borehole Logging at Atlantis Massif Oceanic

Topic The IASPEI standard nomenclature of seismic
Topic The IASPEI standard nomenclature of seismic

Seismic evidence for a chemical heterogeneity in the midmantle: A
Seismic evidence for a chemical heterogeneity in the midmantle: A

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... Vegas, we chose different filter parameters for the two segments of the southern CD-ROM profile. However the processing parameters of the two seismic segments are very similar, permitting the combination of the final migrated sections into a composite display. The seismic data generally exhibit good ...
Porosity prediction using attributes from 3C–3D seismic data
Porosity prediction using attributes from 3C–3D seismic data

Adams2010-MechanicalVibrations.pdf
Adams2010-MechanicalVibrations.pdf

... when it is forced to do so externally, the term “vibration” in mechanical engineering is often reserved for systems that can oscillate freely without applied forces. Sometimes these vibrations cause minor or serious performance or safety problems in engineered systems. For instance, when an aircraft ...
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Research and Development of Seismic Base Isolation Technique

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Nature of Earthquakes

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Lecture 14. Chiroptera II

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Slow strain waves in blocky geological media from GPS and
Slow strain waves in blocky geological media from GPS and

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Magma-compensated crustal thinning in continental rift zones

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The state of the upper mantle beneath southern Africa

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Vp Japan, derived from a dense array observation

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psha using different attenuation relationships for different

... In most of the PSHA applications, a single attenuation relationship is used for all the seismic sources. This may not lead to realistic estimate of the hazard, because there may be a combination of seismic sources with fundamentally different characteristics, warranting the use of different attenuat ...
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2. Data processing and group velocity measurements

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Introduction to Seismology: The wave equation and body waves

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Probabilistic Seismic Hazard Analysis of East Java Region
Probabilistic Seismic Hazard Analysis of East Java Region

SEISMIC RISK ASSESSMENT FOR LARGE DAMS
SEISMIC RISK ASSESSMENT FOR LARGE DAMS

Consulta: subjectFacets:"Crustal structure" Registros recuperados
Consulta: subjectFacets:"Crustal structure" Registros recuperados

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Seismic communication



Seismic communication, sometimes called vibrational communication, describes the conveying of information through seismic vibrations of the substrate. The substrate may be the earth, a plant stem or leaf, the surface of a body of water, a spider’s web, a honeycomb, or any of the myriad types of soil substrates. Seismic cues are generally conveyed by Rayleigh waves generated through vibrations on the substrate, or acoustical waves that couple with the substrate. Vibrational communication is an ancient sensory modality and it is widespread in the animal kingdom where it has evolved several times independently. It has been reported in mammals, birds, reptiles, amphibians, insects, arachnids, crustaceans and nematode worms. Vibrations and other communication channels are not necessarily mutually exclusive, but can be used in multi-modal communication.
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