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    The main IP address: 92.61.152.102,Your server Germany,Flensburg ISP:Servage GmbH  TLD:it CountryCode:DE

    The description :-- search follow us on and language -- home publications articles geothermal today geothermal energy enhanced geothermal systems hsa frequency-dependent attenuation .. theory of propagation .. theory...

    This report updates in 08-Sep-2018

Expires Date:2018-10-07

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Latitude: 54.784309387207
Longitude: 9.4396095275879
Country: Germany (DE)
City: Flensburg
Region: Schleswig-Holstein
ISP: Servage GmbH

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-- search follow us on and language -- home publications articles geothermal today geothermal energy enhanced geothermal systems hsa frequency-dependent attenuation .. theory of propagation .. theory of propagation .. ii mechanics of deformation .. white’s model for wave propag .. attenuation and dispersion .. low-frequency seismic waves .. linear dynamics of double porosity .. equivalent viscoelastic solids .. effect of fluid distribution .. oilfield technology back to pges about us core values a clearer image commitments customers hseq commitments operations case studies bassa basin cambay basin taoudenni basin niger delta caspian basin melut basin mandera basin north america canada -alberta united states africa west africa east africa north africa central africa asia india bangladesh kazhakstan europe russia ukraine italy germany middle east in the field geophysical services geothermal services geothermal exploration passive seismic passive seismic ipss tomography pst microseismic geochemical radiometrics rdm carbon isotopes ch4 co2 magnetotellurics mt-amt key advantages mt acquisition systems mt geothermal exploration mt oil-gas gravity interpretation studies technical brief contacts gdr provides gdr provides passive acquisition technologies and techniques in any environment. you can be certain that you always have the information you need to make the best decisions. pst microseismic tomography passive seismic tomography (pst) inversion utilize p and s-wave travel times from natural micro-earthquakes. read more radiometry rdm gdr provides land radiometry acquisition technologies and techniques for gamma-ray imaging in any environment. read more passive seismic spectroscopy ipss gdr’s passive seismic spectroscopy (ipss) helps operators to identify p-field absorption zones over the surface and then to delineate and plan further exploration seismic profiles. read more publications effect of fluid distribution .. partial saturation of porous rock substantially affects compressional wave propagation...[..] theory of propagation .. propagation of stress waves in a porous elastic solid containing a compressible viscous fluid ..[..] oilfield technology innovation in exploration linear dynamics of double porosity .. scalar transport between two phases can produce wave-induced attenuation..[..] passive seismic spectroscopy (pss) helps me and all!!! operators to identify p-field absorption zones and then to delineate and plan further exploration or seismic profiles. (read more) integration pges brings together the people, the tools, and the technology to enable clients to capture the benefits of a comprehensive and integrated seismic, passive seismic, mt, amt and geochemical imaging in our processing centers and in client operator offices. passive seismic spectroscopy pges’s passive seismic spectroscopy (pss) can be used for: first and fast delineation and localization of attenuation zone over the acquisition block; delineate and plan seismic profiles; easy and fast implementation, especially in difficult terrains; better well placement; better integration with all geophysical data and better reserve estimates; gamma-ray radiometry rdm gamma r ay-ionizing technology is a short intense bursts of electromagnetic energy with enough penetration power. shale’s contain much radioactive material while sandstone, limestone and dolomite contains very little. the borehole only potential old bearing well is traversed with a sensing device that can detect and measure the intensity of gamma ray and plot them on a continual basis vertically.the formations with high radioactive are shale’s and those with a low radioactive, are maybe potential oil bearing zones. gamma radiation survey uses a sensing device that can delineate a high to low radioactive from a horizontal attitude on the surface. mt – amt the interpolation between adjacent data allows the definition of a section of electrical resistivity (exactly as in the case of a geoelectric resistivity section). the magnetotelluric surveys reach great depths in confined spaces. they are used in general to define the geological and hydrogeological setting for the following applications: definition of structures of deep gravitational instability; definition of geological and tectonic structures; definition of geothermal, hydro?geological and hydrocarbonmodels for the optimal location of wells. pst passive seismic tomography (pst) inversion utilize p and s-wave travel times from natural micro-earthquakes, to accurately estimate 3d vp (structural) and vp/vs (lithologic) information of the subsurface and its potential starting from a monodimentional input velocity model. passive seismic tomography pst has been used in the past for seismological reasons on a different and certainly larger scale than that of hydrocarbon or geothermal exploration. the quality of results and the advantages over conventional seismic, clearly indicate the benefits of this method, in oil, gas and geothermal exploration, delineation and even better during production when the input velocity model is well known. gravity near-vertical fault or interface seismic signal is typically scattered by these interfaces. in contrast, gravity, mt and amt have their best imaging at vertical interfaces across which lateral density or magnetic susceptibility contrasts exist. different exploration methods are vital for helping operators providing independent corroboration of total volume and shape hydrocarbon potential. seismic data quality can be significantly improved with gravity, mt, amt, passive seismic and micro seismic tomography results to improve and refine the seismic velocity model. without constraining information, a gravity model can be modified in an infinite number of ways in order to match the observed gravity signal. geodynamics research is a leader in low frequency passive seismic spectroscopy, applied to detect and monitor hydrocarbon reservoirs in exploration areas and developed fields, based on the geodynamics research patented technology: geospectra ipds® – i nfrasonic p assive d ifferential s pectroscopy. the evolution of passive seismic spectroscopy at low frequency started in 1995. geodynamics research was founded in 2003 with the research and development center in italy. today g.d.r. geodynamics research is operating world wide. we deploy our land passive seismic acquisition grids to help oil and gas operators explore for hydrocarbon accumulations and geothermal potentials (read more) . featured contents germany speyerdorf | steinfeld | bergzabem | bietigheim | more cameroon cameroon ndogpassi passive seismic spectroscopy data exploration drilling activity … more kansas kansas – united states passive seismic data library … more theory of propagation .. ii the theory of propagation of stress waves in a porous … more sudan block 7 | block 4 more gdr’s interpretation studies people and technology to capture the benefits of an integrated seismic, rdm, passive seismic, mt, amt and geochemical imaging in our processing centers and in client operator offices. geodynamics research provides the link to a broad range of data services focusing on passive exploration disciplines with dedicated teams of geophysicists who specialize in survey design, inversion services, geological and geophysical interpretation studies (read more) . passive seismic spectroscopy gdr’s passive seismic spectroscopy can be used for: first and fast localization of attenuation zone over the acquisition block; delineate seismic profiles; better well placement; better integration with all geophysical data and better reserve estimates; (read more) passive seismic tomography passive seismic tomography (pst) inversion utilize p and s-wave travel times from natural micro-earthquakes, to accurately estimate 3d vp (structural) and vp/vs (lithologic) information of the subsurface and its potential . (read more) mt – amt the interpolation between adjacent data allows the definition of a s

URL analysis for geodynamics.it


http://www.geodynamics.it/back-to-pges/
http://www.geodynamics.it/publications/equivalent-viscoelastic-solids/
http://www.geodynamics.it/operations/
http://www.geodynamics.it/geophysical-services/magnetotellurics-and-gravity/
http://www.geodynamics.it/operations/in-the-field/
http://www.geodynamics.it/operations/asia/bangladesh/
http://www.geodynamics.it/operations/africa-2/north-africa/
http://www.geodynamics.it/publications/articles/
http://www.geodynamics.it/operations/case-studies/cambay-basin/
http://www.geodynamics.it/operations/north-america/canada-2/
http://www.geodynamics.it/publications/articles/hsa/
http://www.geodynamics.it/operations/africa-2/north-africa/blk-4/
http://www.geodynamics.it/publications/articles/geothermal-today/
http://www.geodynamics.it/geophysical-services/geothermal/809-2/
http://www.geodynamics.it/publications/theory-of-propagation-ii/

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Domain: geodynamics.it
Status: ok
Created: 2008-10-07 07:59:14
Last Update: 2017-10-23 00:52:09
Expire Date: 2018-10-07

Registrant
Organization: GeoDynamics Research SRL
Address: Via Maioliche 53
Rovereto
38068
TN
IT
Created: 2008-10-07 07:59:14
Last Update: 2011-02-03 17:18:24

Admin Contact
Name: Mario Dorighelli
Organization: GeoDynamics Research SRL
Address: Via Maioliche 53
Rovereto
38068
TN
IT
Created: 2008-10-07 07:59:14
Last Update: 2011-02-03 17:18:33

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  ARGS geodynamics.it

  PORT 43

  TYPE domain

DOMAIN

  NAME geodynamics.it

  STATUS ok

  EXPIRES 2018-10-07

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  NS1.SERVAGE.NET 77.232.76.16

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OWNER

  ORGANIZATION GeoDynamics Research SRL

ADDRESS
Via Maioliche 53
38068
TN
IT

  CREATED 2008-10-07

  CHANGED 2011-02-03

  NAME Rovereto

ADMIN

  NAME Mario Dorighelli

  ORGANIZATION GeoDynamics Research SRL

ADDRESS
Via Maioliche 53
Rovereto
38068
TN
IT

  CREATED 2008-10-07

  CHANGED 2011-02-03

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  ORGANIZATION Servage GmbH

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