Structural and Crystal-Chemical Features of Mixed-Layer Illite-Containing Minerals from Catagenetically Altered Upper Jurassic Oil-Source Rocks
Illite-smectite (I-S) minerals from the Upper Jurassic oil-source shales of Denmark and the North Sea were studied by a complex of diffraction and spectroscopic methods. Detailed structures were identified to reveal the mechanism of postsedimentary transformations of these shales. Usually, oil is ge...
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| Veröffentlicht in: | Lithology and Mineral Resources 2023-06, Vol.58 (3), p.183-195 |
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| creator | Drits, V. A. Sakharov, B. A. Zviagina, B. B. |
| description | Illite-smectite (I-S) minerals from the Upper Jurassic oil-source shales of Denmark and the North Sea were studied by a complex of diffraction and spectroscopic methods. Detailed structures were identified to reveal the mechanism of postsedimentary transformations of these shales. Usually, oil is generated in the oil-source rocks of sedimentary basins simultaneously with the diagenetic and catagenetic I-S transformations. The results obtained demonstrate the relationship between these two reactions: NH
3
molecules released from kerogen during the maximum oil formation are fixed as NH
4
cations in smectite or vermiculite interlayers, forming mica or tobelite structural fragments. This solid-phase transformation produces the mixed-layer structures consisting of illite, tobelite, smectite, and vermiculite (I-T-S-V) layers. |
| doi_str_mv | 10.1134/S0024490223700128 |
| format | Article |
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3
molecules released from kerogen during the maximum oil formation are fixed as NH
4
cations in smectite or vermiculite interlayers, forming mica or tobelite structural fragments. This solid-phase transformation produces the mixed-layer structures consisting of illite, tobelite, smectite, and vermiculite (I-T-S-V) layers.</description><identifier>ISSN: 0024-4902</identifier><identifier>EISSN: 1608-3229</identifier><identifier>EISSN: 1573-8892</identifier><identifier>DOI: 10.1134/S0024490223700128</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Ammonia ; Cations ; Diagenesis ; Earth and Environmental Science ; Earth Sciences ; Illite ; Illites ; Interlayers ; Jurassic ; Kerogen ; Mica ; Mineral Resources ; Mineralogy ; Minerals ; Oil ; Phase transitions ; Rocks ; Sedimentary basins ; Sedimentology ; Shales ; Smectites ; Solid phases ; Vermiculite ; Vermiculites</subject><ispartof>Lithology and Mineral Resources, 2023-06, Vol.58 (3), p.183-195</ispartof><rights>Pleiades Publishing, Inc. 2023. ISSN 0024-4902, Lithology and Mineral Resources, 2023, Vol. 58, No. 3, pp. 183–195. © Pleiades Publishing, Inc., 2023. Russian Text © The Author(s), 2023, published in Litologiya i Poleznye Iskopaemye, 2023, No. 3, pp. 215–229.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a291t-25e586bc6cf289e1d9d2d55ae4a1a4d8881d1d94a5ec06490dc52f49cd7e65533</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/S0024490223700128$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0024490223700128$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Drits, V. A.</creatorcontrib><creatorcontrib>Sakharov, B. A.</creatorcontrib><creatorcontrib>Zviagina, B. B.</creatorcontrib><title>Structural and Crystal-Chemical Features of Mixed-Layer Illite-Containing Minerals from Catagenetically Altered Upper Jurassic Oil-Source Rocks</title><title>Lithology and Mineral Resources</title><addtitle>Lithol Miner Resour</addtitle><description>Illite-smectite (I-S) minerals from the Upper Jurassic oil-source shales of Denmark and the North Sea were studied by a complex of diffraction and spectroscopic methods. Detailed structures were identified to reveal the mechanism of postsedimentary transformations of these shales. Usually, oil is generated in the oil-source rocks of sedimentary basins simultaneously with the diagenetic and catagenetic I-S transformations. The results obtained demonstrate the relationship between these two reactions: NH
3
molecules released from kerogen during the maximum oil formation are fixed as NH
4
cations in smectite or vermiculite interlayers, forming mica or tobelite structural fragments. This solid-phase transformation produces the mixed-layer structures consisting of illite, tobelite, smectite, and vermiculite (I-T-S-V) layers.</description><subject>Ammonia</subject><subject>Cations</subject><subject>Diagenesis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Illite</subject><subject>Illites</subject><subject>Interlayers</subject><subject>Jurassic</subject><subject>Kerogen</subject><subject>Mica</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Oil</subject><subject>Phase transitions</subject><subject>Rocks</subject><subject>Sedimentary basins</subject><subject>Sedimentology</subject><subject>Shales</subject><subject>Smectites</subject><subject>Solid phases</subject><subject>Vermiculite</subject><subject>Vermiculites</subject><issn>0024-4902</issn><issn>1608-3229</issn><issn>1573-8892</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1kE1OwzAQhS0EEqVwAHaWWBtsx06cZRXxU1RUidJ1ZOxJSUmTYLsSOQVXxlGRWCBWo5n33jf2IHTJ6DVjibhZUcqFyCnnSUYp4-oITVhKFUk4z4_RZJTJqJ-iM--3NPZZziboaxXc3oS90w3WrcWFG3zQDSneYFebOLwDHVXwuKvwU_0Jliz0AA7Pm6YOQIquDbpu63YT1RYixuPKdTtc6KA30EIYKc2AZ00ABxav-z6mH-NC72uDl3VDVt3eGcDPnXn35-ikigy4-KlTtL67fSkeyGJ5Py9mC6J5zgLhEqRKX01qKq5yYDa33EqpQWimhVVKMRuHQkswNI3_tkbySuTGZpBKmSRTdHXg9q772IMP5Ta-oo0rS66YYpnIMhld7OAyrvPeQVX2rt5pN5SMluPdyz93jxl-yPjobTfgfsn_h74BXCGGVg</recordid><startdate>20230601</startdate><enddate>20230601</enddate><creator>Drits, V. 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A.</creatorcontrib><creatorcontrib>Sakharov, B. A.</creatorcontrib><creatorcontrib>Zviagina, B. B.</creatorcontrib><collection>CrossRef</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Materials Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Lithology and Mineral Resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Drits, V. A.</au><au>Sakharov, B. A.</au><au>Zviagina, B. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Structural and Crystal-Chemical Features of Mixed-Layer Illite-Containing Minerals from Catagenetically Altered Upper Jurassic Oil-Source Rocks</atitle><jtitle>Lithology and Mineral Resources</jtitle><stitle>Lithol Miner Resour</stitle><date>2023-06-01</date><risdate>2023</risdate><volume>58</volume><issue>3</issue><spage>183</spage><epage>195</epage><pages>183-195</pages><issn>0024-4902</issn><eissn>1608-3229</eissn><eissn>1573-8892</eissn><abstract>Illite-smectite (I-S) minerals from the Upper Jurassic oil-source shales of Denmark and the North Sea were studied by a complex of diffraction and spectroscopic methods. Detailed structures were identified to reveal the mechanism of postsedimentary transformations of these shales. Usually, oil is generated in the oil-source rocks of sedimentary basins simultaneously with the diagenetic and catagenetic I-S transformations. The results obtained demonstrate the relationship between these two reactions: NH
3
molecules released from kerogen during the maximum oil formation are fixed as NH
4
cations in smectite or vermiculite interlayers, forming mica or tobelite structural fragments. This solid-phase transformation produces the mixed-layer structures consisting of illite, tobelite, smectite, and vermiculite (I-T-S-V) layers.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0024490223700128</doi><tpages>13</tpages></addata></record> |
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| subjects | Ammonia Cations Diagenesis Earth and Environmental Science Earth Sciences Illite Illites Interlayers Jurassic Kerogen Mica Mineral Resources Mineralogy Minerals Oil Phase transitions Rocks Sedimentary basins Sedimentology Shales Smectites Solid phases Vermiculite Vermiculites |
| title | Structural and Crystal-Chemical Features of Mixed-Layer Illite-Containing Minerals from Catagenetically Altered Upper Jurassic Oil-Source Rocks |
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