Developing the Methods for Multidisciplinary Morphometric Analysis of Relief for Assessing the Tectonic Fragmentation of the Interior
The estimation of the degree of tectonic fragmentation for upper lithosphere following the method of Yu.V. Nechaev (2010) is based on calculations of specific lineament lengths. We used data for three regions—Northwest Caucasus, the Voronezh Anteclise, and the Malko–Petropavlovsk zone in Kamchatka—t...
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| Veröffentlicht in: | Journal of volcanology and seismology 2024-06, Vol.18 (3), p.251-260 |
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| creator | Sobisevich, A. L. Agibalov, A. O. Bergal-Kuvikas, O. V. Zaitsev, V. A. Zykov, D. S. Makeev, V. M. Poleshchuk, A. V. Sentsov, A. A. Shevchenko, A. V. |
| description | The estimation of the degree of tectonic fragmentation for upper lithosphere following the method of Yu.V. Nechaev (2010) is based on calculations of specific lineament lengths. We used data for three regions—Northwest Caucasus, the Voronezh Anteclise, and the Malko–Petropavlovsk zone in Kamchatka—to test whether other morphometric parameters could be used: specific lengths of “weak” zones, elongation lines and water streams, as well as relief curvature. Their anomalies are confined to seismic areas and to areas of hydrothermal and magmatic activity. We show that the most information is provided by 3D models of tectonic fragmentation that incorporate specific lengths of “weak” zones and water stream lengths. |
| doi_str_mv | 10.1134/S074204632470057X |
| format | Article |
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L. ; Agibalov, A. O. ; Bergal-Kuvikas, O. V. ; Zaitsev, V. A. ; Zykov, D. S. ; Makeev, V. M. ; Poleshchuk, A. V. ; Sentsov, A. A. ; Shevchenko, A. V.</creator><creatorcontrib>Sobisevich, A. L. ; Agibalov, A. O. ; Bergal-Kuvikas, O. V. ; Zaitsev, V. A. ; Zykov, D. S. ; Makeev, V. M. ; Poleshchuk, A. V. ; Sentsov, A. A. ; Shevchenko, A. V.</creatorcontrib><description>The estimation of the degree of tectonic fragmentation for upper lithosphere following the method of Yu.V. Nechaev (2010) is based on calculations of specific lineament lengths. We used data for three regions—Northwest Caucasus, the Voronezh Anteclise, and the Malko–Petropavlovsk zone in Kamchatka—to test whether other morphometric parameters could be used: specific lengths of “weak” zones, elongation lines and water streams, as well as relief curvature. Their anomalies are confined to seismic areas and to areas of hydrothermal and magmatic activity. 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Their anomalies are confined to seismic areas and to areas of hydrothermal and magmatic activity. We show that the most information is provided by 3D models of tectonic fragmentation that incorporate specific lengths of “weak” zones and water stream lengths.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fragmentation</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Lithosphere</subject><subject>Morphometry</subject><subject>Tectonics</subject><subject>Three dimensional models</subject><issn>0742-0463</issn><issn>1819-7108</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp1kM1KAzEUhYMoWGofwF3A9WiS-UuWpVottAhawd2QZm7alOlkTFKhD-B7m7GKC3F1F-d853IOQpeUXFOaZjfPpMwYyYqUZSUhefl6ggaUU5GUlPBTNOjlpNfP0cj7LSGE8pylLB-gj1t4h8Z2pl3jsAG8gLCxtcfaOrzYN8HUxivTNaaV7oAX1nUbu4PgjMLjVjYHbzy2Gj9BY0B_UWPvwfufvCWoYNvonjq53kEbZDC27ZFenbUBnLHuAp1p2XgYfd8hepneLScPyfzxfjYZzxNFBQ8JpyvOcqAStBS6hjyVhdI1V1qXVAsmWBZbFnUtZA5cr2TNUsmUUJJJkUuSDtHVMbdz9m0PPlRbu3exh69SUsYfhch4dNGjSznrvQNddc7sYv-KkqofvPozeGTYkfHR267B_Sb_D30CeEeFtw</recordid><startdate>20240601</startdate><enddate>20240601</enddate><creator>Sobisevich, A. 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| subjects | Earth and Environmental Science Earth Sciences Fragmentation Geochemistry Geology Geophysics/Geodesy Lithosphere Morphometry Tectonics Three dimensional models |
| title | Developing the Methods for Multidisciplinary Morphometric Analysis of Relief for Assessing the Tectonic Fragmentation of the Interior |
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