RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE
Recent deformation processes taking place in real time are analyzed on the basis of data on fault zones which were collected by long-term detailed geodetic survey studies with application of field methods and satellite monitoring.A new category of recent crustal movements is described and termed as...
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2015
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ftdoajarticles:oai:doaj.org/article:b2872f5c60bc4f25985cac1d2991b8c5 2023-05-15T16:58:57+02:00 RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE Yu. O. Kuzmin 2015-09-01T00:00:00Z https://doi.org/10.5800/GT-2014-5-2-0135 https://doaj.org/article/b2872f5c60bc4f25985cac1d2991b8c5 EN RU eng rus Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust https://www.gt-crust.ru/jour/article/view/47 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2014-5-2-0135 https://doaj.org/article/b2872f5c60bc4f25985cac1d2991b8c5 Геодинамика и тектонофизика, Vol 5, Iss 2 (2015) faulting deformation seismically active zones geodynamic processes quazi-meridional faults pripyat basin kopetdag kamchatka california strain velocities anomalous deformation displacement pseudo-waves deformation auto-waves geostrain monitor Science Q article 2015 ftdoajarticles https://doi.org/10.5800/GT-2014-5-2-0135 2022-12-30T20:48:42Z Recent deformation processes taking place in real time are analyzed on the basis of data on fault zones which were collected by long-term detailed geodetic survey studies with application of field methods and satellite monitoring.A new category of recent crustal movements is described and termed as parametrically induced tectonic strain in fault zones. It is shown that in the fault zones located in seismically active and aseismic regions, super intensive displacements of the crust (5 to 7 cm per year, i.e. (5 to 7)·10–5 per year) occur due to very small external impacts of natural or technogenic / industrial origin.The spatial discreteness of anomalous deformation processes is established along the strike of the regional Rechitsky fault in the Pripyat basin. It is concluded that recent anomalous activity of the fault zones needs to be taken into account in defining regional regularities of geodynamic processes on the basis of real-time measurements.The paper presents results of analyses of data collected by long-term (20 to 50 years) geodetic surveys in highly seismically active regions of Kopetdag, Kamchatka and California. It is evidenced by instrumental geodetic measurements of recent vertical and horizontal displacements in fault zones that deformations are ‘paradoxically’ deviating from the inherited movements of the past geological periods.In terms of the recent geodynamics, the ‘paradoxes’ of high and low strain velocities are related to a reliable empirical fact of the presence of extremely high local velocities of deformations in the fault zones (about 10–5 per year and above), which take place at the background of slow regional deformations which velocities are lower by the order of 2 to 3. Very low average annual velocities of horizontal deformation are recorded in the seismic regions of Kopetdag and Kamchatka and in the San Andreas fault zone; they amount to only 3 to 5 amplitudes of the earth tidal deformations per year.A ‘fault-block’ dilemma is stated for the recent geodynamics of faults in view ... Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Geodynamics & Tectonophysics 5 2 401 443 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
faulting deformation seismically active zones geodynamic processes quazi-meridional faults pripyat basin kopetdag kamchatka california strain velocities anomalous deformation displacement pseudo-waves deformation auto-waves geostrain monitor Science Q |
spellingShingle |
faulting deformation seismically active zones geodynamic processes quazi-meridional faults pripyat basin kopetdag kamchatka california strain velocities anomalous deformation displacement pseudo-waves deformation auto-waves geostrain monitor Science Q Yu. O. Kuzmin RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
topic_facet |
faulting deformation seismically active zones geodynamic processes quazi-meridional faults pripyat basin kopetdag kamchatka california strain velocities anomalous deformation displacement pseudo-waves deformation auto-waves geostrain monitor Science Q |
description |
Recent deformation processes taking place in real time are analyzed on the basis of data on fault zones which were collected by long-term detailed geodetic survey studies with application of field methods and satellite monitoring.A new category of recent crustal movements is described and termed as parametrically induced tectonic strain in fault zones. It is shown that in the fault zones located in seismically active and aseismic regions, super intensive displacements of the crust (5 to 7 cm per year, i.e. (5 to 7)·10–5 per year) occur due to very small external impacts of natural or technogenic / industrial origin.The spatial discreteness of anomalous deformation processes is established along the strike of the regional Rechitsky fault in the Pripyat basin. It is concluded that recent anomalous activity of the fault zones needs to be taken into account in defining regional regularities of geodynamic processes on the basis of real-time measurements.The paper presents results of analyses of data collected by long-term (20 to 50 years) geodetic surveys in highly seismically active regions of Kopetdag, Kamchatka and California. It is evidenced by instrumental geodetic measurements of recent vertical and horizontal displacements in fault zones that deformations are ‘paradoxically’ deviating from the inherited movements of the past geological periods.In terms of the recent geodynamics, the ‘paradoxes’ of high and low strain velocities are related to a reliable empirical fact of the presence of extremely high local velocities of deformations in the fault zones (about 10–5 per year and above), which take place at the background of slow regional deformations which velocities are lower by the order of 2 to 3. Very low average annual velocities of horizontal deformation are recorded in the seismic regions of Kopetdag and Kamchatka and in the San Andreas fault zone; they amount to only 3 to 5 amplitudes of the earth tidal deformations per year.A ‘fault-block’ dilemma is stated for the recent geodynamics of faults in view ... |
format |
Article in Journal/Newspaper |
author |
Yu. O. Kuzmin |
author_facet |
Yu. O. Kuzmin |
author_sort |
Yu. O. Kuzmin |
title |
RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
title_short |
RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
title_full |
RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
title_fullStr |
RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
title_full_unstemmed |
RECENT GEODYNAMICS OF FAULT ZONES: FAULTING IN REAL TIME SCALE |
title_sort |
recent geodynamics of fault zones: faulting in real time scale |
publisher |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
publishDate |
2015 |
url |
https://doi.org/10.5800/GT-2014-5-2-0135 https://doaj.org/article/b2872f5c60bc4f25985cac1d2991b8c5 |
long_lat |
ENVELOPE(-60.729,-60.729,-64.008,-64.008) |
geographic |
Andreas |
geographic_facet |
Andreas |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Геодинамика и тектонофизика, Vol 5, Iss 2 (2015) |
op_relation |
https://www.gt-crust.ru/jour/article/view/47 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2014-5-2-0135 https://doaj.org/article/b2872f5c60bc4f25985cac1d2991b8c5 |
op_doi |
https://doi.org/10.5800/GT-2014-5-2-0135 |
container_title |
Geodynamics & Tectonophysics |
container_volume |
5 |
container_issue |
2 |
container_start_page |
401 |
op_container_end_page |
443 |
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1766051086125236224 |