GOCE GeoExplore Final Report

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F49777513%3A23520%2F15%3A43925922" target="_blank" >RIV/49777513:23520/15:43925922 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

GOCE GeoExplore Final Report

Popis výsledku v původním jazyce

The main goal of the GOCE mission is to determine the Earth's stationary gravity field with unprecedented accuracy and resolution. GOCE data may improve the understanding and modelling of the Earth's interior and its dynamic processes, contributing to gain new insights into the geodynamics associated with the lithosphere, mantle composition and rheology, uplift and subduction processes. The overall objective of the study was to combine GOCE gravity gradients with heterogeneous other satellite gravity information to arrive at a combined set of gravity gradients complementing (near)-surface data sets spanning all together scales from global down to 5 km useful for various geophysical applications and demonstrate their utility to complement additional data sources (e.g., magnetic, seismic) to enhance geophysical modelling and exploration. We conclude that in areas where good information about the crustal structure exists, satellite gravity gradients hold the potential to unravel lateral a

Název v anglickém jazyce

GOCE GeoExplore Final Report

Popis výsledku anglicky

The main goal of the GOCE mission is to determine the Earth's stationary gravity field with unprecedented accuracy and resolution. GOCE data may improve the understanding and modelling of the Earth's interior and its dynamic processes, contributing to gain new insights into the geodynamics associated with the lithosphere, mantle composition and rheology, uplift and subduction processes. The overall objective of the study was to combine GOCE gravity gradients with heterogeneous other satellite gravity information to arrive at a combined set of gravity gradients complementing (near)-surface data sets spanning all together scales from global down to 5 km useful for various geophysical applications and demonstrate their utility to complement additional data sources (e.g., magnetic, seismic) to enhance geophysical modelling and exploration. We conclude that in areas where good information about the crustal structure exists, satellite gravity gradients hold the potential to unravel lateral a

Druh

V_souhrn - Souhrnná výzkumná zpráva

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

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Návaznosti

R - Projekt Ramcoveho programu EK

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Počet stran výsledku

443

Místo vydání

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Název nakladatele resp. objednatele

European Space Agency

Verze

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