Regional geophysical data on the Carpathian-Pannonian Lithosphere
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F07%3APU66029" target="_blank" >RIV/00216305:26110/07:PU66029 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Regional geophysical data on the Carpathian-Pannonian Lithosphere
Popis výsledku v původním jazyce
Research of the lithosphere of theWestern Carpathians, based on the analysis and interpretation of the complex geological and geophysical data, has brought several remarkable results that enable us to understand more precisely the development of the sedimentary basins. First, a tight relationship between gravity anomalies and sources originated from Tertiary sedimentary basins that creates substantial parts of the gravity effect. Themain part of the gravity effects originating fromboth the Moho discontinuity and the boundary between lithosphere and asthenosphere is mutually compensated for in the region of the Carpathians, and therefore, it can be traced only with difficulties. In this chapter, basic information regarding the study of the gravity fieldof the Western Carpathians are presented, and these both describe the most significant anomalies and the features of the gravity field of basins and support the significance of gravity in the process of verification of interpretation of
Název v anglickém jazyce
Regional geophysical data on the Carpathian-Pannonian Lithosphere
Popis výsledku anglicky
Research of the lithosphere of theWestern Carpathians, based on the analysis and interpretation of the complex geological and geophysical data, has brought several remarkable results that enable us to understand more precisely the development of the sedimentary basins. First, a tight relationship between gravity anomalies and sources originated from Tertiary sedimentary basins that creates substantial parts of the gravity effect. Themain part of the gravity effects originating fromboth the Moho discontinuity and the boundary between lithosphere and asthenosphere is mutually compensated for in the region of the Carpathians, and therefore, it can be traced only with difficulties. In this chapter, basic information regarding the study of the gravity fieldof the Western Carpathians are presented, and these both describe the most significant anomalies and the features of the gravity field of basins and support the significance of gravity in the process of verification of interpretation of
Klasifikace
Druh
C - Kapitola v odborné knize
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA205%2F04%2F0820" target="_blank" >GA205/04/0820: Stabilita krasového území v okolí ponoru Bílé vody v Moravském krasu</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2007
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název knihy nebo sborníku
The Carpathians and their Foreland: Geology and Hydrocarbon Resources
ISBN
978-0-89181-365-1
Počet stran výsledku
47
Strana od-do
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Počet stran knihy
845
Název nakladatele
AAPG
Místo vydání
Neuveden
Kód UT WoS kapitoly
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