Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka
Detailed data are discussed on the rate of Holocene horizontal and vertical movements along a fault in the southeastern Kamchatsky Peninsula, which is situated between the converging Aleutian and Kamchatka island arcs. The fault is the northern boundary of the block invading into the peninsula under...
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MAIK Nauka/Interperiodica
2014
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ftoceanrep:oai:oceanrep.geomar.de:28469 2024-01-28T10:06:55+01:00 Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka Kozhurin, A. I. Pinegina, T. K. Ponomareva, Vera V. Zelenin, E. A. Mikhailyukova, P. G. 2014 text https://oceanrep.geomar.de/id/eprint/28469/ https://oceanrep.geomar.de/id/eprint/28469/1/Kozhurin_et_%20al_%202014_en%20.pdf https://doi.org/10.1134/S001685211402006X en eng MAIK Nauka/Interperiodica Springer https://oceanrep.geomar.de/id/eprint/28469/1/Kozhurin_et_%20al_%202014_en%20.pdf Kozhurin, A. I., Pinegina, T. K., Ponomareva, V. V., Zelenin, E. A. and Mikhailyukova, P. G. (2014) Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka. Open Access Geotectonics, 48 (2). pp. 122-138. DOI 10.1134/S001685211402006X <https://doi.org/10.1134/S001685211402006X>. doi:10.1134/S001685211402006X cc_by_nc_3.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2014 ftoceanrep https://doi.org/10.1134/S001685211402006X 2024-01-01T00:22:33Z Detailed data are discussed on the rate of Holocene horizontal and vertical movements along a fault in the southeastern Kamchatsky Peninsula, which is situated between the converging Aleutian and Kamchatka island arcs. The fault is the northern boundary of the block invading into the peninsula under pressure of the Komandorsky Block of the Aleutian arc. The rate of right-lateral slip along the fault was increasing in the Holocene and reached 18–19 mm/yr over the last 2000 years and 20 mm/yr by contemporary time. Comparison of these estimates with those that follow from offsets of older rocks also indicates acceleration of horizontal movements along the fault from the early Quaternary to the present. The results obtained from rates of GPS station migration show that about half the rate of the northwestern drift of the Komandorsky Block is consumed for movement of the block of the southern side of the fault. The remainder of movement of the Komandorsky Block is consumed for movements (probably, underthrusting) at the eastern continental slope of the Kamchatsky Peninsula. Article in Journal/Newspaper Kamchatka OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Geotectonics 48 2 122 138 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Detailed data are discussed on the rate of Holocene horizontal and vertical movements along a fault in the southeastern Kamchatsky Peninsula, which is situated between the converging Aleutian and Kamchatka island arcs. The fault is the northern boundary of the block invading into the peninsula under pressure of the Komandorsky Block of the Aleutian arc. The rate of right-lateral slip along the fault was increasing in the Holocene and reached 18–19 mm/yr over the last 2000 years and 20 mm/yr by contemporary time. Comparison of these estimates with those that follow from offsets of older rocks also indicates acceleration of horizontal movements along the fault from the early Quaternary to the present. The results obtained from rates of GPS station migration show that about half the rate of the northwestern drift of the Komandorsky Block is consumed for movement of the block of the southern side of the fault. The remainder of movement of the Komandorsky Block is consumed for movements (probably, underthrusting) at the eastern continental slope of the Kamchatsky Peninsula. |
format |
Article in Journal/Newspaper |
author |
Kozhurin, A. I. Pinegina, T. K. Ponomareva, Vera V. Zelenin, E. A. Mikhailyukova, P. G. |
spellingShingle |
Kozhurin, A. I. Pinegina, T. K. Ponomareva, Vera V. Zelenin, E. A. Mikhailyukova, P. G. Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
author_facet |
Kozhurin, A. I. Pinegina, T. K. Ponomareva, Vera V. Zelenin, E. A. Mikhailyukova, P. G. |
author_sort |
Kozhurin, A. I. |
title |
Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
title_short |
Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
title_full |
Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
title_fullStr |
Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
title_full_unstemmed |
Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka |
title_sort |
rate of collisional deformation in kamchatsky peninsula, kamchatka |
publisher |
MAIK Nauka/Interperiodica |
publishDate |
2014 |
url |
https://oceanrep.geomar.de/id/eprint/28469/ https://oceanrep.geomar.de/id/eprint/28469/1/Kozhurin_et_%20al_%202014_en%20.pdf https://doi.org/10.1134/S001685211402006X |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
https://oceanrep.geomar.de/id/eprint/28469/1/Kozhurin_et_%20al_%202014_en%20.pdf Kozhurin, A. I., Pinegina, T. K., Ponomareva, V. V., Zelenin, E. A. and Mikhailyukova, P. G. (2014) Rate of collisional deformation in Kamchatsky Peninsula, Kamchatka. Open Access Geotectonics, 48 (2). pp. 122-138. DOI 10.1134/S001685211402006X <https://doi.org/10.1134/S001685211402006X>. doi:10.1134/S001685211402006X |
op_rights |
cc_by_nc_3.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1134/S001685211402006X |
container_title |
Geotectonics |
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48 |
container_issue |
2 |
container_start_page |
122 |
op_container_end_page |
138 |
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1789334167728685056 |