Geochemistry of isotopes (δ13C and δ18O) and depositional environment of the upper Kazanian carbonate sediments in the Volga-Vyatka interfluve
This work reports the results of lithological and isotopic study of carbonate rocks from the Pechishchi stratotype section (Kazan) and three adjacent sections of Kazanian rocks of the Volga-Vyatka region at the eastern Russian Platform. These sections were recovered by the Kremeshki, Popovtsevo, and...
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| Veröffentlicht in: | Lithology and Mineral Resources 2009-09, Vol.44 (5), p.465-481 |
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| creator | Kuleshov, V. N. Sedaeva, K. M. |
| description | This work reports the results of lithological and isotopic study of carbonate rocks from the Pechishchi stratotype section (Kazan) and three adjacent sections of Kazanian rocks of the Volga-Vyatka region at the eastern Russian Platform. These sections were recovered by the Kremeshki, Popovtsevo, and Chimbulat quarries (near the town of Sovetsk, southeastern Kirov district). Lithological features and wide variations of δ
13
C (from −6.0 to 6.8‰) and δ
18
O (from 22.9 to 33.4 ‰) indicate that the rocks were formed in a shallow-marine basin with rapidly varying conditions of sedimentation which characterize different facies (and/or paleoecological) zones: lagoonal, supralittoral, littoral, shoal. They also suggest processes of postsedimentary alteration (mainly, under supergene conditions). Numerous short-term hiatuses are also recorded. |
| doi_str_mv | 10.1134/S0024490209050058 |
| format | Article |
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13
C (from −6.0 to 6.8‰) and δ
18
O (from 22.9 to 33.4 ‰) indicate that the rocks were formed in a shallow-marine basin with rapidly varying conditions of sedimentation which characterize different facies (and/or paleoecological) zones: lagoonal, supralittoral, littoral, shoal. They also suggest processes of postsedimentary alteration (mainly, under supergene conditions). Numerous short-term hiatuses are also recorded.</description><identifier>ISSN: 0024-4902</identifier><identifier>EISSN: 1608-3229</identifier><identifier>EISSN: 1573-8892</identifier><identifier>DOI: 10.1134/S0024490209050058</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Carbonate rocks ; Carbonate sediments ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Isotopes ; Mineral Resources ; Mineralogy ; Ocean basins ; Paleoecology ; Sedimentary geology ; Sedimentology</subject><ispartof>Lithology and Mineral Resources, 2009-09, Vol.44 (5), p.465-481</ispartof><rights>Pleiades Publishing, Ltd. 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c315t-8cee9ae09634793368f5f20eff06cb414f51d37be77de142fce6fd32026199783</citedby><cites>FETCH-LOGICAL-c315t-8cee9ae09634793368f5f20eff06cb414f51d37be77de142fce6fd32026199783</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/S0024490209050058$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0024490209050058$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Kuleshov, V. N.</creatorcontrib><creatorcontrib>Sedaeva, K. M.</creatorcontrib><title>Geochemistry of isotopes (δ13C and δ18O) and depositional environment of the upper Kazanian carbonate sediments in the Volga-Vyatka interfluve</title><title>Lithology and Mineral Resources</title><addtitle>Lithol Miner Resour</addtitle><description>This work reports the results of lithological and isotopic study of carbonate rocks from the Pechishchi stratotype section (Kazan) and three adjacent sections of Kazanian rocks of the Volga-Vyatka region at the eastern Russian Platform. These sections were recovered by the Kremeshki, Popovtsevo, and Chimbulat quarries (near the town of Sovetsk, southeastern Kirov district). Lithological features and wide variations of δ
13
C (from −6.0 to 6.8‰) and δ
18
O (from 22.9 to 33.4 ‰) indicate that the rocks were formed in a shallow-marine basin with rapidly varying conditions of sedimentation which characterize different facies (and/or paleoecological) zones: lagoonal, supralittoral, littoral, shoal. They also suggest processes of postsedimentary alteration (mainly, under supergene conditions). Numerous short-term hiatuses are also recorded.</description><subject>Carbonate rocks</subject><subject>Carbonate sediments</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Isotopes</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Ocean basins</subject><subject>Paleoecology</subject><subject>Sedimentary geology</subject><subject>Sedimentology</subject><issn>0024-4902</issn><issn>1608-3229</issn><issn>1573-8892</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</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>eNp1kEtOwzAURS0EEqWwAGYWIxgE_MnPQ1RBQVRiAHQauclz65LawXYqlVWwGNbBmkhaJAaI0fude6V3ETql5JJSHl89EcLiWBBGBEkISfI9NKApySPOmNhHg_4c9fdDdOT9knRzJugAfYzBlgtYaR_cBluFtbfBNuDx-dcn5SMsTYW7Ln-82LYVNNbroK2RNQaz1s6aFZjQS8MCcNs04PCDfJdGS4NL6WYdGgB7qHQPeqzNlpzaei6j6UaGV9ntAjhVt2s4RgdK1h5OfuoQvdzePI_uosnj-H50PYlKTpMQ5SWAkEBEyuNMcJ7mKlGMgFIkLWcxjVVCK57NIMsqoDFTJaSq4oywlAqR5XyIzna-jbNvLfhQLG3ruq98kWcsZ1mc8g6iO6h01nsHqmicXkm3KSgp-tyLP7l3GrbT-I41c3C_xv-LvgFftYcd</recordid><startdate>20090901</startdate><enddate>20090901</enddate><creator>Kuleshov, V. 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M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c315t-8cee9ae09634793368f5f20eff06cb414f51d37be77de142fce6fd32026199783</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Carbonate rocks</topic><topic>Carbonate sediments</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Isotopes</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Ocean basins</topic><topic>Paleoecology</topic><topic>Sedimentary geology</topic><topic>Sedimentology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kuleshov, V. N.</creatorcontrib><creatorcontrib>Sedaeva, K. 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13
C (from −6.0 to 6.8‰) and δ
18
O (from 22.9 to 33.4 ‰) indicate that the rocks were formed in a shallow-marine basin with rapidly varying conditions of sedimentation which characterize different facies (and/or paleoecological) zones: lagoonal, supralittoral, littoral, shoal. They also suggest processes of postsedimentary alteration (mainly, under supergene conditions). Numerous short-term hiatuses are also recorded.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0024490209050058</doi><tpages>17</tpages></addata></record> |
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| subjects | Carbonate rocks Carbonate sediments Earth and Environmental Science Earth Sciences Geochemistry Isotopes Mineral Resources Mineralogy Ocean basins Paleoecology Sedimentary geology Sedimentology |
| title | Geochemistry of isotopes (δ13C and δ18O) and depositional environment of the upper Kazanian carbonate sediments in the Volga-Vyatka interfluve |
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