Geochemistry of isotopes (δ13C, δ18O) and formation conditions of lower-middle permian rocks in the Soyana River region (Arkhangel’sk district)
The results of study of the isotopic-lithological compositions of carbonate and terrigenous-carbonate rocks in the Soyana River section (northern East European Platform, Arkhangel’sk district) are presented. The results make it possible to identify 10 main lithotypes and show a wide variation range...
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| Veröffentlicht in: | Lithology and Mineral Resources 2011-05, Vol.46 (3), p.265-281 |
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| creator | Kuleshov, V. N. Sedaeva, K. M. Stroganova, Yu. Yu |
| description | The results of study of the isotopic-lithological compositions of carbonate and terrigenous-carbonate rocks in the Soyana River section (northern East European Platform, Arkhangel’sk district) are presented. The results make it possible to identify 10 main lithotypes and show a wide variation range of δ
13
C (from −2.2 to +3.6‰, PDB) and δ
18
O (from 22.5 to 30.5‰, SMOW). These lithological features and isotopic compositions suggest that the rocks were formed in a shallow-marine setting characterized by rapidly changing sedimentation conditions in various facies (and/or paleoecological) zones: inlets, lagoons, supralittoral, littoral, and shoals. Periods of aridization and humidization are recorded. The results also indicate numerous synsedimentary short-term hiatuses and stages of increased continental runoff—episodic pulsatory input of clastic material with the continental paleoflows. |
| doi_str_mv | 10.1134/S0024490211020039 |
| format | Article |
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13
C (from −2.2 to +3.6‰, PDB) and δ
18
O (from 22.5 to 30.5‰, SMOW). These lithological features and isotopic compositions suggest that the rocks were formed in a shallow-marine setting characterized by rapidly changing sedimentation conditions in various facies (and/or paleoecological) zones: inlets, lagoons, supralittoral, littoral, and shoals. Periods of aridization and humidization are recorded. The results also indicate numerous synsedimentary short-term hiatuses and stages of increased continental runoff—episodic pulsatory input of clastic material with the continental paleoflows.</description><identifier>ISSN: 0024-4902</identifier><identifier>EISSN: 1608-3229</identifier><identifier>EISSN: 1573-8892</identifier><identifier>DOI: 10.1134/S0024490211020039</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Carbonate rocks ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geological time ; Inlets ; Isotopes ; Lagoons ; Mineral Resources ; Mineralogy ; Paleoecology ; Permian ; Petrology ; Rivers ; Sedimentology ; Shoals</subject><ispartof>Lithology and Mineral Resources, 2011-05, Vol.46 (3), p.265-281</ispartof><rights>Pleiades Publishing, Ltd. 2011</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c315t-daa910c39637636ddac1bc88d14020920db1eb11727c1e6e6354b2438f9b40923</citedby><cites>FETCH-LOGICAL-c315t-daa910c39637636ddac1bc88d14020920db1eb11727c1e6e6354b2438f9b40923</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/S0024490211020039$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0024490211020039$$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><creatorcontrib>Stroganova, Yu. Yu</creatorcontrib><title>Geochemistry of isotopes (δ13C, δ18O) and formation conditions of lower-middle permian rocks in the Soyana River region (Arkhangel’sk district)</title><title>Lithology and Mineral Resources</title><addtitle>Lithol Miner Resour</addtitle><description>The results of study of the isotopic-lithological compositions of carbonate and terrigenous-carbonate rocks in the Soyana River section (northern East European Platform, Arkhangel’sk district) are presented. The results make it possible to identify 10 main lithotypes and show a wide variation range of δ
13
C (from −2.2 to +3.6‰, PDB) and δ
18
O (from 22.5 to 30.5‰, SMOW). These lithological features and isotopic compositions suggest that the rocks were formed in a shallow-marine setting characterized by rapidly changing sedimentation conditions in various facies (and/or paleoecological) zones: inlets, lagoons, supralittoral, littoral, and shoals. Periods of aridization and humidization are recorded. The results also indicate numerous synsedimentary short-term hiatuses and stages of increased continental runoff—episodic pulsatory input of clastic material with the continental paleoflows.</description><subject>Carbonate rocks</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geological time</subject><subject>Inlets</subject><subject>Isotopes</subject><subject>Lagoons</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Paleoecology</subject><subject>Permian</subject><subject>Petrology</subject><subject>Rivers</subject><subject>Sedimentology</subject><subject>Shoals</subject><issn>0024-4902</issn><issn>1608-3229</issn><issn>1573-8892</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</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>eNp1UM1KAzEQDqJgrT6At-CpBVczyf4eS9EqFAr-nJdskm3T7m5qslV68x08-R4-hw_hk5ilggfxNDN8PzPzIXQK5AKAhZf3hNAwzAgFIJQQlu2hHsQkDRil2T7qdXDQ4YfoyLkl8XOSQQ-9TZQRC1Vr19otNiXWzrRmrRwefH4AG59jX9LZEPNG4tLYmrfaNFiYRuquc52mMi_KBrWWslJ4rWyteYOtESuHdYPbhcL3Zssbju_0s7LYqnnnMRjZ1YI3c1V9vb67FZbdDVq0w2N0UPLKqZOf2keP11cP45tgOpvcjkfTQDCI2kByngERLItZErNYSi6gEGkqIfQRZJTIAlQBkNBEgIpVzKKwoCFLy6wIPc766Gznu7bmaaNcmy_NxjZ-ZZ7GMY1SiMCTYEcS1jhnVZmvra653eZA8i76_E_0XkN3Gue5_kH7a_y_6BvOd4eh</recordid><startdate>20110501</startdate><enddate>20110501</enddate><creator>Kuleshov, V. 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Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c315t-daa910c39637636ddac1bc88d14020920db1eb11727c1e6e6354b2438f9b40923</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Carbonate rocks</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Geological time</topic><topic>Inlets</topic><topic>Isotopes</topic><topic>Lagoons</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Paleoecology</topic><topic>Permian</topic><topic>Petrology</topic><topic>Rivers</topic><topic>Sedimentology</topic><topic>Shoals</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kuleshov, V. N.</creatorcontrib><creatorcontrib>Sedaeva, K. M.</creatorcontrib><creatorcontrib>Stroganova, Yu. 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N.</au><au>Sedaeva, K. M.</au><au>Stroganova, Yu. Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemistry of isotopes (δ13C, δ18O) and formation conditions of lower-middle permian rocks in the Soyana River region (Arkhangel’sk district)</atitle><jtitle>Lithology and Mineral Resources</jtitle><stitle>Lithol Miner Resour</stitle><date>2011-05-01</date><risdate>2011</risdate><volume>46</volume><issue>3</issue><spage>265</spage><epage>281</epage><pages>265-281</pages><issn>0024-4902</issn><eissn>1608-3229</eissn><eissn>1573-8892</eissn><abstract>The results of study of the isotopic-lithological compositions of carbonate and terrigenous-carbonate rocks in the Soyana River section (northern East European Platform, Arkhangel’sk district) are presented. The results make it possible to identify 10 main lithotypes and show a wide variation range of δ
13
C (from −2.2 to +3.6‰, PDB) and δ
18
O (from 22.5 to 30.5‰, SMOW). These lithological features and isotopic compositions suggest that the rocks were formed in a shallow-marine setting characterized by rapidly changing sedimentation conditions in various facies (and/or paleoecological) zones: inlets, lagoons, supralittoral, littoral, and shoals. Periods of aridization and humidization are recorded. The results also indicate numerous synsedimentary short-term hiatuses and stages of increased continental runoff—episodic pulsatory input of clastic material with the continental paleoflows.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0024490211020039</doi><tpages>17</tpages></addata></record> |
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| subjects | Carbonate rocks Earth and Environmental Science Earth Sciences Geochemistry Geological time Inlets Isotopes Lagoons Mineral Resources Mineralogy Paleoecology Permian Petrology Rivers Sedimentology Shoals |
| title | Geochemistry of isotopes (δ13C, δ18O) and formation conditions of lower-middle permian rocks in the Soyana River region (Arkhangel’sk district) |
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