Abstract
An analysis was performed to compare results of deformometric measurements from the Caucasus orogen and data of fluid dynamic (emanation) monitoring geodeformation processes from the conjugated East European Platform. It allowed us to identify spectral components, first of all, in a range of lunar-solar tides that demonstrates a relationship between the analyzed fields and global geodeformation processes. Moreover, the analysis made it possible to reveal some prominent features of changes in the measured parameters during global changes in tense-deformed state in the Earth's crust, in particular, during preparation and realization of catastrophic earthquakes in the Indian Ocean on 26 December, 2004 and 28 March, 2005.
Highlights
Ïîð3âíÿëüíèé àíàë3ç äàíèõ äåôîðìîìåòðè÷íèõ ñïîñòåðåæåíü, îòðèìàíèõ â óìîâàõ Êàâêàçüêîãî îðîãåíà, 3 äàíèõ ôëþ¿äîäèíàì3÷íîãî ìîí3òîðèíãó ãåîäåôîðìàö3éíèõ ïðîöåñ3â â óìîâàõ ñïðÿæåíî¿ ç íèì Ñõ3äíîoâðîïåéñüêî¿ ïëàòôîðìè äàâ çìîãó 3äåíòèô3êóâàòè ñïåêòðàëüí3 ñêëàäîâ3 âèì3ðþâàíèõ ïàðàìåòð3â, ïåðåäóñ3ì ñêëàäîâèõ ì3ñÿ÷íî-ñîíÿ÷íèõ ïðèïëèâ3â, ùî çàñâ3ä÷óo çâÿçîê àíàë3çîâàíèõ ïîë3â ç ãëîáàëüíèìè ãåîäåôîðìàö3éíèìè ïðîöåñàìè
It allowed us to identify spectral components, first of all, in a range of lunar-solar tides that demonstrates a relationship between the analyzed fields and global geodeformation processes
The analysis made it possible to reveal some prominent features of changes in the measured parameters during global changes in tensedeformed state in the Earths crust, in particular, during preparation and realization of catastrophic earthquakes in the Indian Ocean on 26 December, 2004 and 28 March, 2005
Summary
Ïîð3âíÿëüíèé àíàë3ç äàíèõ äåôîðìîìåòðè÷íèõ ñïîñòåðåæåíü, îòðèìàíèõ â óìîâàõ Êàâêàçüêîãî îðîãåíà, 3 äàíèõ ôëþ¿äîäèíàì3÷íîãî (åìàíàö3éíîãî) ìîí3òîðèíãó ãåîäåôîðìàö3éíèõ ïðîöåñ3â â óìîâàõ ñïðÿæåíî¿ ç íèì Ñõ3äíîoâðîïåéñüêî¿ ïëàòôîðìè äàâ çìîãó 3äåíòèô3êóâàòè ñïåêòðàëüí3 ñêëàäîâ3 âèì3ðþâàíèõ ïàðàìåòð3â, ïåðåäóñ3ì ñêëàäîâèõ ì3ñÿ÷íî-ñîíÿ÷íèõ ïðèïëèâ3â, ùî çàñâ3ä÷óo çâÿçîê àíàë3çîâàíèõ ïîë3â ç ãëîáàëüíèìè ãåîäåôîðìàö3éíèìè ïðîöåñàìè. An analysis was performed to compare results of deformometric measurements from the Caucasus orogen and data of fluid dynamic (emanation) monitoring geodeformation processes from the conjugated East European Platform. Ðàíåå áûëî ïîêàçàíî [Ðóäàêîâ, 1993, 2004, 2008], ÷òî êîëåáàòåëüíûå äâèæåíèÿ Âîñòî÷íîÅâðîïåéñêîé ïëàòôîðìû (ÂÅÏ) îêàçûâàþò îùóòèìîå âëèÿíèå íà èçìåíåíèå íàïðÿæåííî-äåôîðìèðîâàííîãî ñîñòîÿíèÿ ìàññèâà ãîðíûõ ïîðîä íà Êàâêàçå è , ïðåæäå âñåãî , â ïåðèîäû ïîäãîòîâêè è ðåàëèçàöèè êàòàñòðîôè÷åñêèõ çåìëåòðÿñåíèé.
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