Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)
Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu 2–3 , Yu 4 and Yu 6 , Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) whic...
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Veröffentlicht in: | Petroleum chemistry 2019-10, Vol.59 (10), p.1138-1146 |
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creator | Fursenko, E. A. Kim, N. S. |
description | Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu
2–3
, Yu
4
and Yu
6
, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits. |
doi_str_mv | 10.1134/S0965544119100049 |
format | Article |
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2–3
, Yu
4
and Yu
6
, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.</description><identifier>ISSN: 0965-5441</identifier><identifier>EISSN: 1555-6239</identifier><identifier>DOI: 10.1134/S0965544119100049</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Analysis ; Aromatic hydrocarbons ; Bituminous materials ; Chemistry ; Chemistry and Materials Science ; Composition ; Condensates ; Geochemistry ; Industrial Chemistry/Chemical Engineering ; Lipids ; Organic matter</subject><ispartof>Petroleum chemistry, 2019-10, Vol.59 (10), p.1138-1146</ispartof><rights>Pleiades Publishing, Ltd. 2019</rights><rights>COPYRIGHT 2019 Springer</rights><rights>Copyright Springer Nature B.V. 2019</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c355t-9f63cdebae364460b5be0f1d65c35338dbd1d6cb3e14f6c9fe3ecc0a9b2703613</citedby><cites>FETCH-LOGICAL-c355t-9f63cdebae364460b5be0f1d65c35338dbd1d6cb3e14f6c9fe3ecc0a9b2703613</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/S0965544119100049$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0965544119100049$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Fursenko, E. A.</creatorcontrib><creatorcontrib>Kim, N. S.</creatorcontrib><title>Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)</title><title>Petroleum chemistry</title><addtitle>Pet. Chem</addtitle><description>Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu
2–3
, Yu
4
and Yu
6
, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.</description><subject>Analysis</subject><subject>Aromatic hydrocarbons</subject><subject>Bituminous materials</subject><subject>Chemistry</subject><subject>Chemistry and Materials Science</subject><subject>Composition</subject><subject>Condensates</subject><subject>Geochemistry</subject><subject>Industrial Chemistry/Chemical Engineering</subject><subject>Lipids</subject><subject>Organic matter</subject><issn>0965-5441</issn><issn>1555-6239</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kM9KAzEQxoMoWKsP4G3Bi4Jbk82fusdSbBUqClXU05LNTmrqNqnJ9tCbr-Hr-SRmWcGDyByGme_7TSaD0DHBA0Iou5jjXHDOGCE5wRizfAf1COc8FRnNd1GvldNW30cHISwxJkPCaA89T8GpV1iZ0Pht4nQydrYCG2QDoS1vZe22ciXrr4_P8OYgmRioq-T0pe0l92CNDZtanidPEBrwNpmbEryRZ4doT8s6wNFP7qPHydXD-Dqd3U1vxqNZqijnTZprQVUFpQQqGBO45CVgTSrBo07pZVVWsVAlBcK0ULkGCkphmZfZEFNBaB-ddHPX3r1v4hLF0m28jU8WGcWcZxkRLLoGnWshayiM1a7xUsWo4teVs6BN7I8EzoacEkojQDpAeReCB12svVlJvy0ILtqLF38uHpmsY0L02gX431X-h74BT7KC6A</recordid><startdate>20191001</startdate><enddate>20191001</enddate><creator>Fursenko, E. A.</creator><creator>Kim, N. S.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20191001</creationdate><title>Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)</title><author>Fursenko, E. A. ; Kim, N. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c355t-9f63cdebae364460b5be0f1d65c35338dbd1d6cb3e14f6c9fe3ecc0a9b2703613</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Analysis</topic><topic>Aromatic hydrocarbons</topic><topic>Bituminous materials</topic><topic>Chemistry</topic><topic>Chemistry and Materials Science</topic><topic>Composition</topic><topic>Condensates</topic><topic>Geochemistry</topic><topic>Industrial Chemistry/Chemical Engineering</topic><topic>Lipids</topic><topic>Organic matter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fursenko, E. A.</creatorcontrib><creatorcontrib>Kim, N. S.</creatorcontrib><collection>CrossRef</collection><jtitle>Petroleum chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fursenko, E. A.</au><au>Kim, N. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)</atitle><jtitle>Petroleum chemistry</jtitle><stitle>Pet. Chem</stitle><date>2019-10-01</date><risdate>2019</risdate><volume>59</volume><issue>10</issue><spage>1138</spage><epage>1146</epage><pages>1138-1146</pages><issn>0965-5441</issn><eissn>1555-6239</eissn><abstract>Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu
2–3
, Yu
4
and Yu
6
, Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0965544119100049</doi><tpages>9</tpages></addata></record> |
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subjects | Analysis Aromatic hydrocarbons Bituminous materials Chemistry Chemistry and Materials Science Composition Condensates Geochemistry Industrial Chemistry/Chemical Engineering Lipids Organic matter |
title | Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia) |
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