Results of Ultra-High-Resolution Seismoacoustic Survey Offshore Taman Bay in the Area of the Ancient City of Phanagoria
— The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of th...
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Veröffentlicht in: | Izvestiya. Atmospheric and oceanic physics 2019-12, Vol.55 (11), p.1749-1754 |
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container_title | Izvestiya. Atmospheric and oceanic physics |
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creator | Gaydalenok, O. V. Shmatkov, A. A. Shmatkova, A. A. Olkhovsky, S. V. |
description | —
The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of this area is confirmed. An analysis of the bedding of the newest marine sediments of the bottom and the submergence of the ancient city of Phanagoria in the beginning of the 1st century AD indicate the Late Holocene tectonic activity of the Taman Bay depression. Two profile areas exhibit signal coherence gaps interpreted as areas of gas accumulations. The gas emissions are probably morphologically related to a wing of the adjacent Akhtaniz Anticline and are interpreted as a result of clay diapirism of the Maikop Group. |
doi_str_mv | 10.1134/S0001433819110021 |
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The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of this area is confirmed. An analysis of the bedding of the newest marine sediments of the bottom and the submergence of the ancient city of Phanagoria in the beginning of the 1st century AD indicate the Late Holocene tectonic activity of the Taman Bay depression. Two profile areas exhibit signal coherence gaps interpreted as areas of gas accumulations. The gas emissions are probably morphologically related to a wing of the adjacent Akhtaniz Anticline and are interpreted as a result of clay diapirism of the Maikop Group.</description><identifier>ISSN: 0001-4338</identifier><identifier>EISSN: 1555-628X</identifier><identifier>DOI: 10.1134/S0001433819110021</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Age composition ; Anticlines ; Clay ; Climatology ; Diapirism ; Earth and Environmental Science ; Earth Sciences ; Geophysics/Geodesy ; High resolution ; Historic sites ; Holocene ; Marine sediments ; Offshore ; Quaternary ; Resolution ; Sediment ; Sediments ; Seismic surveys ; Submergence ; Surveying ; Tectonics</subject><ispartof>Izvestiya. Atmospheric and oceanic physics, 2019-12, Vol.55 (11), p.1749-1754</ispartof><rights>Pleiades Publishing, Ltd. 2019</rights><rights>Pleiades Publishing, Ltd. 2019.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0001433819110021$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0001433819110021$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Gaydalenok, O. V.</creatorcontrib><creatorcontrib>Shmatkov, A. A.</creatorcontrib><creatorcontrib>Shmatkova, A. A.</creatorcontrib><creatorcontrib>Olkhovsky, S. V.</creatorcontrib><title>Results of Ultra-High-Resolution Seismoacoustic Survey Offshore Taman Bay in the Area of the Ancient City of Phanagoria</title><title>Izvestiya. Atmospheric and oceanic physics</title><addtitle>Izv. Atmos. Ocean. Phys</addtitle><description>—
The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of this area is confirmed. An analysis of the bedding of the newest marine sediments of the bottom and the submergence of the ancient city of Phanagoria in the beginning of the 1st century AD indicate the Late Holocene tectonic activity of the Taman Bay depression. Two profile areas exhibit signal coherence gaps interpreted as areas of gas accumulations. The gas emissions are probably morphologically related to a wing of the adjacent Akhtaniz Anticline and are interpreted as a result of clay diapirism of the Maikop Group.</description><subject>Age composition</subject><subject>Anticlines</subject><subject>Clay</subject><subject>Climatology</subject><subject>Diapirism</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics/Geodesy</subject><subject>High resolution</subject><subject>Historic sites</subject><subject>Holocene</subject><subject>Marine sediments</subject><subject>Offshore</subject><subject>Quaternary</subject><subject>Resolution</subject><subject>Sediment</subject><subject>Sediments</subject><subject>Seismic surveys</subject><subject>Submergence</subject><subject>Surveying</subject><subject>Tectonics</subject><issn>0001-4338</issn><issn>1555-628X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1UM9LwzAUDqLgnP4B3gKeq0naptlxDnXCYOI28FbesmTN6JKZpEr_e1sneBBP7_H9erwPoWtKbilNs7sFIYRmaSroiFJCGD1BA5rnecKZeDtFg55Oev4cXYSwI4SzjBQD9PmqQlPHgJ3Gqzp6SKZmWyUd6uomGmfxQpmwdyBdE6KReNH4D9Xiudahcl7hJezB4ntosbE4VgqPvYI-7Xu30igb8cTEtsdeKrCwdd7AJTrTUAd19TOHaPX4sJxMk9n86XkyniWScRETwWCz1pIJ4DkrCNsAK9J1TjNIQXFO8g3Nui8pK4QaSSnXACRXQmeaQaGAp0N0c8w9ePfeqBDLnWu87U6WLB0JkReckU5FjyrpXQhe6fLgzR58W1JS9v2Wf_rtPOzoCZ3WbpX_Tf7f9AVR9ny2</recordid><startdate>20191201</startdate><enddate>20191201</enddate><creator>Gaydalenok, O. 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V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c268t-82adbfc28a652702da273b514a3ae6605d145551278e9cccbaa05e8f4f2a7ea63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Age composition</topic><topic>Anticlines</topic><topic>Clay</topic><topic>Climatology</topic><topic>Diapirism</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geophysics/Geodesy</topic><topic>High resolution</topic><topic>Historic sites</topic><topic>Holocene</topic><topic>Marine sediments</topic><topic>Offshore</topic><topic>Quaternary</topic><topic>Resolution</topic><topic>Sediment</topic><topic>Sediments</topic><topic>Seismic surveys</topic><topic>Submergence</topic><topic>Surveying</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gaydalenok, O. V.</creatorcontrib><creatorcontrib>Shmatkov, A. A.</creatorcontrib><creatorcontrib>Shmatkova, A. A.</creatorcontrib><creatorcontrib>Olkhovsky, S. V.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gaydalenok, O. V.</au><au>Shmatkov, A. A.</au><au>Shmatkova, A. A.</au><au>Olkhovsky, S. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Results of Ultra-High-Resolution Seismoacoustic Survey Offshore Taman Bay in the Area of the Ancient City of Phanagoria</atitle><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle><stitle>Izv. Atmos. Ocean. Phys</stitle><date>2019-12-01</date><risdate>2019</risdate><volume>55</volume><issue>11</issue><spage>1749</spage><epage>1754</epage><pages>1749-1754</pages><issn>0001-4338</issn><eissn>1555-628X</eissn><abstract>—
The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of this area is confirmed. An analysis of the bedding of the newest marine sediments of the bottom and the submergence of the ancient city of Phanagoria in the beginning of the 1st century AD indicate the Late Holocene tectonic activity of the Taman Bay depression. Two profile areas exhibit signal coherence gaps interpreted as areas of gas accumulations. The gas emissions are probably morphologically related to a wing of the adjacent Akhtaniz Anticline and are interpreted as a result of clay diapirism of the Maikop Group.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0001433819110021</doi><tpages>6</tpages></addata></record> |
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subjects | Age composition Anticlines Clay Climatology Diapirism Earth and Environmental Science Earth Sciences Geophysics/Geodesy High resolution Historic sites Holocene Marine sediments Offshore Quaternary Resolution Sediment Sediments Seismic surveys Submergence Surveying Tectonics |
title | Results of Ultra-High-Resolution Seismoacoustic Survey Offshore Taman Bay in the Area of the Ancient City of Phanagoria |
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