Study of active faults: Theoretical and applied implications
Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The disp...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Trifonov, V. G. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2010 |
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| Übergeordnetes Werk: |
Enthalten in: Geotectonics - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 44(2010), 6 vom: Nov., Seite 510-528 |
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| Übergeordnetes Werk: |
volume:44 ; year:2010 ; number:6 ; month:11 ; pages:510-528 |
| Links: |
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| DOI / URN: |
10.1134/S0016852110060051 |
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| Katalog-ID: |
SPR020008252 |
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| 520 | |a Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. | ||
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| 700 | 1 | |a Kozhurin, A. I. |4 aut | |
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10.1134/S0016852110060051 doi (DE-627)SPR020008252 (SPR)S0016852110060051-e DE-627 ger DE-627 rakwb eng Trifonov, V. G. verfasserin aut Study of active faults: Theoretical and applied implications 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 Kozhurin, A. I. aut Enthalten in Geotectonics Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2010), 6 vom: Nov., Seite 510-528 (DE-627)342320939 (DE-600)2071668-0 1556-1976 nnns volume:44 year:2010 number:6 month:11 pages:510-528 https://dx.doi.org/10.1134/S0016852110060051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2010 6 11 510-528 |
| spelling |
10.1134/S0016852110060051 doi (DE-627)SPR020008252 (SPR)S0016852110060051-e DE-627 ger DE-627 rakwb eng Trifonov, V. G. verfasserin aut Study of active faults: Theoretical and applied implications 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 Kozhurin, A. I. aut Enthalten in Geotectonics Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2010), 6 vom: Nov., Seite 510-528 (DE-627)342320939 (DE-600)2071668-0 1556-1976 nnns volume:44 year:2010 number:6 month:11 pages:510-528 https://dx.doi.org/10.1134/S0016852110060051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2010 6 11 510-528 |
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10.1134/S0016852110060051 doi (DE-627)SPR020008252 (SPR)S0016852110060051-e DE-627 ger DE-627 rakwb eng Trifonov, V. G. verfasserin aut Study of active faults: Theoretical and applied implications 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 Kozhurin, A. I. aut Enthalten in Geotectonics Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2010), 6 vom: Nov., Seite 510-528 (DE-627)342320939 (DE-600)2071668-0 1556-1976 nnns volume:44 year:2010 number:6 month:11 pages:510-528 https://dx.doi.org/10.1134/S0016852110060051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2010 6 11 510-528 |
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10.1134/S0016852110060051 doi (DE-627)SPR020008252 (SPR)S0016852110060051-e DE-627 ger DE-627 rakwb eng Trifonov, V. G. verfasserin aut Study of active faults: Theoretical and applied implications 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 Kozhurin, A. I. aut Enthalten in Geotectonics Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2010), 6 vom: Nov., Seite 510-528 (DE-627)342320939 (DE-600)2071668-0 1556-1976 nnns volume:44 year:2010 number:6 month:11 pages:510-528 https://dx.doi.org/10.1134/S0016852110060051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2010 6 11 510-528 |
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10.1134/S0016852110060051 doi (DE-627)SPR020008252 (SPR)S0016852110060051-e DE-627 ger DE-627 rakwb eng Trifonov, V. G. verfasserin aut Study of active faults: Theoretical and applied implications 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 Kozhurin, A. I. aut Enthalten in Geotectonics Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2010), 6 vom: Nov., Seite 510-528 (DE-627)342320939 (DE-600)2071668-0 1556-1976 nnns volume:44 year:2010 number:6 month:11 pages:510-528 https://dx.doi.org/10.1134/S0016852110060051 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2010 6 11 510-528 |
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Trifonov, V. G. |
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Trifonov, V. G. misc Fault Zone misc Tephra misc Active Fault misc Strike Slip Fault misc Strike Slip Study of active faults: Theoretical and applied implications |
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Study of active faults: Theoretical and applied implications Fault Zone (dpeaa)DE-He213 Tephra (dpeaa)DE-He213 Active Fault (dpeaa)DE-He213 Strike Slip Fault (dpeaa)DE-He213 Strike Slip (dpeaa)DE-He213 |
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Study of active faults: Theoretical and applied implications |
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study of active faults: theoretical and applied implications |
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Study of active faults: Theoretical and applied implications |
| abstract |
Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. © Pleiades Publishing, Ltd. 2010 |
| abstractGer |
Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. © Pleiades Publishing, Ltd. 2010 |
| abstract_unstemmed |
Abstract Theoretical and applied implications of the study of active faults and their identification and parametrization are discussed. The term active fault is defined as a fault with displacements that occurred in the late Pleistocene and Holocene and are expected to resume in the future. The displaced young landforms, late Quaternary sediments, and man-made constructions are the main reference marks to recognize active faults and estimate their kinematics and intensity. Since the structural pattern and parameters of all active faults are referred to the same, geologically short time interval, they are important for the study of recent geodynamics and young tectogenesis on the global, regional, and local scales. The opportunities that are opened for such investigations are illustrated by verification of the real existence of the Okhotsk and Bering minor plates. With allowance for active faults, it is possible to make tectonic and geodynamic reconstructions of the past events more plausible. Natural hazards, primarily, earthquakes, are related to active faults. The geological and geomorphic assessment of the seismic potential of active fault zones is discussed with emphasis on the maximum possible magnitude of earthquakes (Mmax) estimated from the segmentation of the active zones, the length of particular segments (L), the empirical relationships Mmax/L for strong recent earthquakes, as well as the resumption periods of strong earthquakes and measurement of particular seismogenic offsets by trenching and other techniques, including archeoseismological methods. A question is posed about possible perennial variations in the stress-and-strain state of active zones, which are expressed on the scale of large seismoactive regions in oscillations of released seismic energy and should be taken into account by assessment of the seismic hazard. © Pleiades Publishing, Ltd. 2010 |
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Study of active faults: Theoretical and applied implications |
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| score |
7.4007635 |