A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf
The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneat...
Gespeichert in:
| Veröffentlicht in: | Geotectonics 2013, Vol.47 (1), p.1-30 |
|---|---|
| Hauptverfasser: | , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 30 |
|---|---|
| container_issue | 1 |
| container_start_page | 1 |
| container_title | Geotectonics |
| container_volume | 47 |
| creator | Laverov, N. P. Lobkovsky, L. I. Kononov, M. V. Dobretsov, N. L. Vernikovsky, V. A. Sokolov, S. D. Shipilov, E. V. |
| description | The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneath the continent caused by subduction of the Pacific lithosphere under the Eurasian and North American lithospheric plates. The structure of the Amerasia and Eurasia basins of the Arctic is shown to have formed progressively due to destruction of the ancient Arctida continent, a retained fragment of which comprises the structural units of the central segment of the Arctic Ocean, including the Lomonosov Ridge, the Alpha-Mendeleev Rise, and the Podvodnikov and Makarov basins. The proposed model is considered to be a scientific substantiation of the updated Russian territorial claim to the UN Commission on the determination of the Limits of the Continental Shelf in the Arctic Region. |
| doi_str_mv | 10.1134/S0016852113010044 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1315623059</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1315623059</sourcerecordid><originalsourceid>FETCH-LOGICAL-a372t-c992c369650dbc6351f063e3fef954f7ee191bf90972fa06ad252022b26d99253</originalsourceid><addsrcrecordid>eNp1kctKxDAUhoMoOF4ewF3AjZtqLk1qlsPgDRTBy7pk2pMxQ5tokgr6OD6pKeOgKK7Cyf99PyEHoQNKjinl5ck9IVSeCpYHQgkpyw00oULIgqpKbqLJGBdjvo12YlwSwklOJ-hjihfg2zene9vg3rfQYW9wegIMr74bkvVufTENTcrQXEfrsHYt1u1SN-ASThCCTT5YiDhnI3wD0b_7jI_gDNz3MKZ-yArubG_Tuv1uiNFqh2feJetyq-7w_RN0Zg9tGd1F2P86d9Hj-dnD7LK4vr24mk2vC80rlopGKdZwqaQg7byRXFBDJAduwChRmgqAKjo3iqiKGU2kbplghLE5k21WBd9FR6ve5-BfBoip7m1soOu0Az_EmnIqJMv_pjJ6-Atd-iG4_LqaslNOS1Yxnim6oprgYwxg6udgex3eakrqcWv1n61lh62cmFm3gPCj-V_pE0mqmZg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1283142723</pqid></control><display><type>article</type><title>A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf</title><source>SpringerLink Journals</source><creator>Laverov, N. P. ; Lobkovsky, L. I. ; Kononov, M. V. ; Dobretsov, N. L. ; Vernikovsky, V. A. ; Sokolov, S. D. ; Shipilov, E. V.</creator><creatorcontrib>Laverov, N. P. ; Lobkovsky, L. I. ; Kononov, M. V. ; Dobretsov, N. L. ; Vernikovsky, V. A. ; Sokolov, S. D. ; Shipilov, E. V.</creatorcontrib><description>The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneath the continent caused by subduction of the Pacific lithosphere under the Eurasian and North American lithospheric plates. The structure of the Amerasia and Eurasia basins of the Arctic is shown to have formed progressively due to destruction of the ancient Arctida continent, a retained fragment of which comprises the structural units of the central segment of the Arctic Ocean, including the Lomonosov Ridge, the Alpha-Mendeleev Rise, and the Podvodnikov and Makarov basins. The proposed model is considered to be a scientific substantiation of the updated Russian territorial claim to the UN Commission on the determination of the Limits of the Continental Shelf in the Arctic Region.</description><identifier>ISSN: 0016-8521</identifier><identifier>EISSN: 1556-1976</identifier><identifier>DOI: 10.1134/S0016852113010044</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Arctic zone ; Cenozoic ; Continental dynamics ; Continental shelves ; Earth and Environmental Science ; Earth Sciences ; Geology ; Lithosphere ; Mesozoic ; Paleozoic ; Plate tectonics ; Structural Geology ; Upper mantle</subject><ispartof>Geotectonics, 2013, Vol.47 (1), p.1-30</ispartof><rights>Pleiades Publishing, Ltd. 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a372t-c992c369650dbc6351f063e3fef954f7ee191bf90972fa06ad252022b26d99253</citedby><cites>FETCH-LOGICAL-a372t-c992c369650dbc6351f063e3fef954f7ee191bf90972fa06ad252022b26d99253</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0016852113010044$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0016852113010044$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Laverov, N. P.</creatorcontrib><creatorcontrib>Lobkovsky, L. I.</creatorcontrib><creatorcontrib>Kononov, M. V.</creatorcontrib><creatorcontrib>Dobretsov, N. L.</creatorcontrib><creatorcontrib>Vernikovsky, V. A.</creatorcontrib><creatorcontrib>Sokolov, S. D.</creatorcontrib><creatorcontrib>Shipilov, E. V.</creatorcontrib><title>A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf</title><title>Geotectonics</title><addtitle>Geotecton</addtitle><description>The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneath the continent caused by subduction of the Pacific lithosphere under the Eurasian and North American lithospheric plates. The structure of the Amerasia and Eurasia basins of the Arctic is shown to have formed progressively due to destruction of the ancient Arctida continent, a retained fragment of which comprises the structural units of the central segment of the Arctic Ocean, including the Lomonosov Ridge, the Alpha-Mendeleev Rise, and the Podvodnikov and Makarov basins. The proposed model is considered to be a scientific substantiation of the updated Russian territorial claim to the UN Commission on the determination of the Limits of the Continental Shelf in the Arctic Region.</description><subject>Arctic zone</subject><subject>Cenozoic</subject><subject>Continental dynamics</subject><subject>Continental shelves</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geology</subject><subject>Lithosphere</subject><subject>Mesozoic</subject><subject>Paleozoic</subject><subject>Plate tectonics</subject><subject>Structural Geology</subject><subject>Upper mantle</subject><issn>0016-8521</issn><issn>1556-1976</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kctKxDAUhoMoOF4ewF3AjZtqLk1qlsPgDRTBy7pk2pMxQ5tokgr6OD6pKeOgKK7Cyf99PyEHoQNKjinl5ck9IVSeCpYHQgkpyw00oULIgqpKbqLJGBdjvo12YlwSwklOJ-hjihfg2zene9vg3rfQYW9wegIMr74bkvVufTENTcrQXEfrsHYt1u1SN-ASThCCTT5YiDhnI3wD0b_7jI_gDNz3MKZ-yArubG_Tuv1uiNFqh2feJetyq-7w_RN0Zg9tGd1F2P86d9Hj-dnD7LK4vr24mk2vC80rlopGKdZwqaQg7byRXFBDJAduwChRmgqAKjo3iqiKGU2kbplghLE5k21WBd9FR6ve5-BfBoip7m1soOu0Az_EmnIqJMv_pjJ6-Atd-iG4_LqaslNOS1Yxnim6oprgYwxg6udgex3eakrqcWv1n61lh62cmFm3gPCj-V_pE0mqmZg</recordid><startdate>2013</startdate><enddate>2013</enddate><creator>Laverov, N. P.</creator><creator>Lobkovsky, L. I.</creator><creator>Kononov, M. V.</creator><creator>Dobretsov, N. L.</creator><creator>Vernikovsky, V. A.</creator><creator>Sokolov, S. D.</creator><creator>Shipilov, E. V.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>2013</creationdate><title>A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf</title><author>Laverov, N. P. ; Lobkovsky, L. I. ; Kononov, M. V. ; Dobretsov, N. L. ; Vernikovsky, V. A. ; Sokolov, S. D. ; Shipilov, E. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a372t-c992c369650dbc6351f063e3fef954f7ee191bf90972fa06ad252022b26d99253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Arctic zone</topic><topic>Cenozoic</topic><topic>Continental dynamics</topic><topic>Continental shelves</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geology</topic><topic>Lithosphere</topic><topic>Mesozoic</topic><topic>Paleozoic</topic><topic>Plate tectonics</topic><topic>Structural Geology</topic><topic>Upper mantle</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Laverov, N. P.</creatorcontrib><creatorcontrib>Lobkovsky, L. I.</creatorcontrib><creatorcontrib>Kononov, M. V.</creatorcontrib><creatorcontrib>Dobretsov, N. L.</creatorcontrib><creatorcontrib>Vernikovsky, V. A.</creatorcontrib><creatorcontrib>Sokolov, S. D.</creatorcontrib><creatorcontrib>Shipilov, E. V.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Geotectonics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Laverov, N. P.</au><au>Lobkovsky, L. I.</au><au>Kononov, M. V.</au><au>Dobretsov, N. L.</au><au>Vernikovsky, V. A.</au><au>Sokolov, S. D.</au><au>Shipilov, E. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf</atitle><jtitle>Geotectonics</jtitle><stitle>Geotecton</stitle><date>2013</date><risdate>2013</risdate><volume>47</volume><issue>1</issue><spage>1</spage><epage>30</epage><pages>1-30</pages><issn>0016-8521</issn><eissn>1556-1976</eissn><abstract>The tectonic evolution of the Arctic Region in the Mesozoic and Cenozoic is considered with allowance for the Paleozoic stage of evolution of the ancient Arctida continent. A new geodynamic model of the evolution of the Arctic is based on the idea of the development of upper mantle convection beneath the continent caused by subduction of the Pacific lithosphere under the Eurasian and North American lithospheric plates. The structure of the Amerasia and Eurasia basins of the Arctic is shown to have formed progressively due to destruction of the ancient Arctida continent, a retained fragment of which comprises the structural units of the central segment of the Arctic Ocean, including the Lomonosov Ridge, the Alpha-Mendeleev Rise, and the Podvodnikov and Makarov basins. The proposed model is considered to be a scientific substantiation of the updated Russian territorial claim to the UN Commission on the determination of the Limits of the Continental Shelf in the Arctic Region.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0016852113010044</doi><tpages>30</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0016-8521 |
| ispartof | Geotectonics, 2013, Vol.47 (1), p.1-30 |
| issn | 0016-8521 1556-1976 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1315623059 |
| source | SpringerLink Journals |
| subjects | Arctic zone Cenozoic Continental dynamics Continental shelves Earth and Environmental Science Earth Sciences Geology Lithosphere Mesozoic Paleozoic Plate tectonics Structural Geology Upper mantle |
| title | A geodynamic model of the evolution of the Arctic basin and adjacent territories in the Mesozoic and Cenozoic and the outer limit of the Russian Continental Shelf |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-13T05%3A25%3A37IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20geodynamic%20model%20of%20the%20evolution%20of%20the%20Arctic%20basin%20and%20adjacent%20territories%20in%20the%20Mesozoic%20and%20Cenozoic%20and%20the%20outer%20limit%20of%20the%20Russian%20Continental%20Shelf&rft.jtitle=Geotectonics&rft.au=Laverov,%20N.%20P.&rft.date=2013&rft.volume=47&rft.issue=1&rft.spage=1&rft.epage=30&rft.pages=1-30&rft.issn=0016-8521&rft.eissn=1556-1976&rft_id=info:doi/10.1134/S0016852113010044&rft_dat=%3Cproquest_cross%3E1315623059%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1283142723&rft_id=info:pmid/&rfr_iscdi=true |