Nature of the North Caspian gravity anomaly

With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Geotectonics 2007-05, Vol.41 (3), p.195-209
Hauptverfasser: Segalovich, V. I., Volozh, Yu. A., Antipov, M. P., Vasil’ev, O. A.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 209
container_issue 3
container_start_page 195
container_title Geotectonics
container_volume 41
creator Segalovich, V. I.
Volozh, Yu. A.
Antipov, M. P.
Vasil’ev, O. A.
description With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12 km. This complex was formed contemporaneously with spreading of the Ural-Turkistan ocean and mark a rift zone in the south of passive margin of the East European continent. The rift was conjugated with an ancient triple junction on the floor of the Ural-Turkistan paleocean.[PUBLICATION ABSTRACT]
doi_str_mv 10.1134/S0016852107030028
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_20359053</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1221137417</sourcerecordid><originalsourceid>FETCH-LOGICAL-a359t-55d20993f042ae1daa0d5d26ac795bfd29b78512308f4caa1e67c0f8722c095f3</originalsourceid><addsrcrecordid>eNp90E1LxDAQBuAgCq6rP8Bb8SCCVGeSpmmOsvgFy3pQz2W2Tdwu3WZNWqH_3izrScFTYN6HGfIydo5wgyiy21cAzAvJERQIAF4csAlKmaeoVX7IJrs43eXH7CSENUQU0wm7XlA_eJM4m_Qrkyyc71fJjMK2oS758PTV9GNCndtQO56yI0ttMGc_75S9P9y_zZ7S-cvj8-xunpKQuk-lrDloLSxknAzWRFDHUU6V0nJpa66XqpDIBRQ2q4jQ5KoCWyjOK9DSiim73O_devc5mNCXmyZUpm2pM24IJYd4B6SI8OpfiJzHclSGKtKLX3TtBt_Fb5RK6lxnmYSIcI8q70LwxpZb32zIjyVCuau5_FOz-Ab3tmyP</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>759694450</pqid></control><display><type>article</type><title>Nature of the North Caspian gravity anomaly</title><source>SpringerLink Journals - AutoHoldings</source><creator>Segalovich, V. I. ; Volozh, Yu. A. ; Antipov, M. P. ; Vasil’ev, O. A.</creator><creatorcontrib>Segalovich, V. I. ; Volozh, Yu. A. ; Antipov, M. P. ; Vasil’ev, O. A.</creatorcontrib><description>With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12 km. This complex was formed contemporaneously with spreading of the Ural-Turkistan ocean and mark a rift zone in the south of passive margin of the East European continent. The rift was conjugated with an ancient triple junction on the floor of the Ural-Turkistan paleocean.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0016-8521</identifier><identifier>EISSN: 1556-1976</identifier><identifier>DOI: 10.1134/S0016852107030028</identifier><language>eng</language><publisher>Washington: Springer Nature B.V</publisher><subject>Geology ; Paleozoic</subject><ispartof>Geotectonics, 2007-05, Vol.41 (3), p.195-209</ispartof><rights>Nauka/Interperiodica 2007</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a359t-55d20993f042ae1daa0d5d26ac795bfd29b78512308f4caa1e67c0f8722c095f3</citedby><cites>FETCH-LOGICAL-a359t-55d20993f042ae1daa0d5d26ac795bfd29b78512308f4caa1e67c0f8722c095f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Segalovich, V. I.</creatorcontrib><creatorcontrib>Volozh, Yu. A.</creatorcontrib><creatorcontrib>Antipov, M. P.</creatorcontrib><creatorcontrib>Vasil’ev, O. A.</creatorcontrib><title>Nature of the North Caspian gravity anomaly</title><title>Geotectonics</title><description>With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12 km. This complex was formed contemporaneously with spreading of the Ural-Turkistan ocean and mark a rift zone in the south of passive margin of the East European continent. The rift was conjugated with an ancient triple junction on the floor of the Ural-Turkistan paleocean.[PUBLICATION ABSTRACT]</description><subject>Geology</subject><subject>Paleozoic</subject><issn>0016-8521</issn><issn>1556-1976</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp90E1LxDAQBuAgCq6rP8Bb8SCCVGeSpmmOsvgFy3pQz2W2Tdwu3WZNWqH_3izrScFTYN6HGfIydo5wgyiy21cAzAvJERQIAF4csAlKmaeoVX7IJrs43eXH7CSENUQU0wm7XlA_eJM4m_Qrkyyc71fJjMK2oS758PTV9GNCndtQO56yI0ttMGc_75S9P9y_zZ7S-cvj8-xunpKQuk-lrDloLSxknAzWRFDHUU6V0nJpa66XqpDIBRQ2q4jQ5KoCWyjOK9DSiim73O_devc5mNCXmyZUpm2pM24IJYd4B6SI8OpfiJzHclSGKtKLX3TtBt_Fb5RK6lxnmYSIcI8q70LwxpZb32zIjyVCuau5_FOz-Ab3tmyP</recordid><startdate>20070501</startdate><enddate>20070501</enddate><creator>Segalovich, V. I.</creator><creator>Volozh, Yu. A.</creator><creator>Antipov, M. P.</creator><creator>Vasil’ev, O. A.</creator><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>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>20070501</creationdate><title>Nature of the North Caspian gravity anomaly</title><author>Segalovich, V. I. ; Volozh, Yu. A. ; Antipov, M. P. ; Vasil’ev, O. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a359t-55d20993f042ae1daa0d5d26ac795bfd29b78512308f4caa1e67c0f8722c095f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Geology</topic><topic>Paleozoic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Segalovich, V. I.</creatorcontrib><creatorcontrib>Volozh, Yu. A.</creatorcontrib><creatorcontrib>Antipov, M. P.</creatorcontrib><creatorcontrib>Vasil’ev, O. A.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; 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 Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; 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 &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric &amp; 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>Segalovich, V. I.</au><au>Volozh, Yu. A.</au><au>Antipov, M. P.</au><au>Vasil’ev, O. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nature of the North Caspian gravity anomaly</atitle><jtitle>Geotectonics</jtitle><date>2007-05-01</date><risdate>2007</risdate><volume>41</volume><issue>3</issue><spage>195</spage><epage>209</epage><pages>195-209</pages><issn>0016-8521</issn><eissn>1556-1976</eissn><abstract>With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12 km. This complex was formed contemporaneously with spreading of the Ural-Turkistan ocean and mark a rift zone in the south of passive margin of the East European continent. The rift was conjugated with an ancient triple junction on the floor of the Ural-Turkistan paleocean.[PUBLICATION ABSTRACT]</abstract><cop>Washington</cop><pub>Springer Nature B.V</pub><doi>10.1134/S0016852107030028</doi><tpages>15</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0016-8521
ispartof Geotectonics, 2007-05, Vol.41 (3), p.195-209
issn 0016-8521
1556-1976
language eng
recordid cdi_proquest_miscellaneous_20359053
source SpringerLink Journals - AutoHoldings
subjects Geology
Paleozoic
title Nature of the North Caspian gravity anomaly
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-01T19%3A25%3A26IST&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=Nature%20of%20the%20North%20Caspian%20gravity%20anomaly&rft.jtitle=Geotectonics&rft.au=Segalovich,%20V.%20I.&rft.date=2007-05-01&rft.volume=41&rft.issue=3&rft.spage=195&rft.epage=209&rft.pages=195-209&rft.issn=0016-8521&rft.eissn=1556-1976&rft_id=info:doi/10.1134/S0016852107030028&rft_dat=%3Cproquest_cross%3E1221137417%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=759694450&rft_id=info:pmid/&rfr_iscdi=true