Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths
In-situ δ 18 O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs within the Upper Rhine Graben. The overgrowths record two types of the evolution...
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| Veröffentlicht in: | International journal of earth sciences : Geologische Rundschau 2021-11, Vol.110 (8), p.2779-2802 |
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| container_title | International journal of earth sciences : Geologische Rundschau |
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| creator | Bossennec, Claire Géraud, Yves Böcker, Johannes Klug, Bernd Mattioni, Luca Sizun, Jean-Pierre Sudo, Masafumi Moretti, Isabelle |
| description | In-situ δ
18
O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs within the Upper Rhine Graben. The overgrowths record two types of the evolution of δ
18
O: 1) a monotonous decrease of the δ
18
O
overgrowth
interpreted as linked to an increasing burial temperature and 2) random fluctuations, interpreted as pointing out the injection of allochthonous fluids in faulted areas, on the cementation processes of the pore network (both intergranular and fracture planes). Fluids causing the quartz cementation are either autochthonous buffered in
18
O from clay illitisation; or allochthonous fluids of meteoric origin with δ
18
O below − 5%. These allochthonous fluids are in thermal disequilibrium with the host sandstone. The measured signal of δ
18
O
overgrowth
measured from samples and calculated curves testing hypothetic δ
18
O
fluid
are compared to T–t evolution during burial. This modelling proposes the initiation of quartz cementation during the Jurassic and is validated by the in-situ
40
Ar/
39
Ar dating results obtained on the feldspar overgrowths predating quartz overgrowths. A similar diagenetic history is recorded on the graben shoulders and in the buried parts of the basin. Here, the beginning of the pore network cementation predates the structuration in blocks of the basin before the Cenozoic graben opening. |
| doi_str_mv | 10.1007/s00531-021-02080-2 |
| format | Article |
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18
O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs within the Upper Rhine Graben. The overgrowths record two types of the evolution of δ
18
O: 1) a monotonous decrease of the δ
18
O
overgrowth
interpreted as linked to an increasing burial temperature and 2) random fluctuations, interpreted as pointing out the injection of allochthonous fluids in faulted areas, on the cementation processes of the pore network (both intergranular and fracture planes). Fluids causing the quartz cementation are either autochthonous buffered in
18
O from clay illitisation; or allochthonous fluids of meteoric origin with δ
18
O below − 5%. These allochthonous fluids are in thermal disequilibrium with the host sandstone. The measured signal of δ
18
O
overgrowth
measured from samples and calculated curves testing hypothetic δ
18
O
fluid
are compared to T–t evolution during burial. This modelling proposes the initiation of quartz cementation during the Jurassic and is validated by the in-situ
40
Ar/
39
Ar dating results obtained on the feldspar overgrowths predating quartz overgrowths. A similar diagenetic history is recorded on the graben shoulders and in the buried parts of the basin. Here, the beginning of the pore network cementation predates the structuration in blocks of the basin before the Cenozoic graben opening.</description><identifier>ISSN: 1437-3254</identifier><identifier>EISSN: 1437-3262</identifier><identifier>DOI: 10.1007/s00531-021-02080-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Allochthonous deposits ; Cementation ; Cenozoic ; Diagenesis ; Earth and Environmental Science ; Earth Sciences ; Environmental Sciences ; Evolution ; Feldspars ; Fluids ; Geochemistry ; Geochronology ; Geochronometry ; Geology ; Geophysics/Geodesy ; Graben ; Intergranular fracture ; Isotopes ; Jurassic ; Mineral Resources ; Mineralogy ; Original Paper ; Quartz ; Radiometric dating ; Sandstone ; Sciences of the Universe ; Sedimentary rocks ; Sedimentology ; Structural Geology ; Temperature</subject><ispartof>International journal of earth sciences : Geologische Rundschau, 2021-11, Vol.110 (8), p.2779-2802</ispartof><rights>The Author(s) 2021</rights><rights>The Author(s) 2021. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>Attribution</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2422-1bd283fabee6086198a04263f740db794429c3bd3e6330ad367461374b3d219b3</citedby><cites>FETCH-LOGICAL-c2422-1bd283fabee6086198a04263f740db794429c3bd3e6330ad367461374b3d219b3</cites><orcidid>0000-0003-3227-4869</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00531-021-02080-2$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00531-021-02080-2$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,885,27924,27925,41488,42557,51319</link.rule.ids><backlink>$$Uhttps://ifp.hal.science/hal-03563492$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Bossennec, Claire</creatorcontrib><creatorcontrib>Géraud, Yves</creatorcontrib><creatorcontrib>Böcker, Johannes</creatorcontrib><creatorcontrib>Klug, Bernd</creatorcontrib><creatorcontrib>Mattioni, Luca</creatorcontrib><creatorcontrib>Sizun, Jean-Pierre</creatorcontrib><creatorcontrib>Sudo, Masafumi</creatorcontrib><creatorcontrib>Moretti, Isabelle</creatorcontrib><title>Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths</title><title>International journal of earth sciences : Geologische Rundschau</title><addtitle>Int J Earth Sci (Geol Rundsch)</addtitle><description>In-situ δ
18
O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs within the Upper Rhine Graben. The overgrowths record two types of the evolution of δ
18
O: 1) a monotonous decrease of the δ
18
O
overgrowth
interpreted as linked to an increasing burial temperature and 2) random fluctuations, interpreted as pointing out the injection of allochthonous fluids in faulted areas, on the cementation processes of the pore network (both intergranular and fracture planes). Fluids causing the quartz cementation are either autochthonous buffered in
18
O from clay illitisation; or allochthonous fluids of meteoric origin with δ
18
O below − 5%. These allochthonous fluids are in thermal disequilibrium with the host sandstone. The measured signal of δ
18
O
overgrowth
measured from samples and calculated curves testing hypothetic δ
18
O
fluid
are compared to T–t evolution during burial. This modelling proposes the initiation of quartz cementation during the Jurassic and is validated by the in-situ
40
Ar/
39
Ar dating results obtained on the feldspar overgrowths predating quartz overgrowths. A similar diagenetic history is recorded on the graben shoulders and in the buried parts of the basin. Here, the beginning of the pore network cementation predates the structuration in blocks of the basin before the Cenozoic graben opening.</description><subject>Allochthonous deposits</subject><subject>Cementation</subject><subject>Cenozoic</subject><subject>Diagenesis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Sciences</subject><subject>Evolution</subject><subject>Feldspars</subject><subject>Fluids</subject><subject>Geochemistry</subject><subject>Geochronology</subject><subject>Geochronometry</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Graben</subject><subject>Intergranular fracture</subject><subject>Isotopes</subject><subject>Jurassic</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Original Paper</subject><subject>Quartz</subject><subject>Radiometric dating</subject><subject>Sandstone</subject><subject>Sciences of the Universe</subject><subject>Sedimentary rocks</subject><subject>Sedimentology</subject><subject>Structural Geology</subject><subject>Temperature</subject><issn>1437-3254</issn><issn>1437-3262</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp9kc1u1TAQhSNEJUrhBVhZYkMXaf0XJ1leqnKLuFKliq4tJ3YSV6mdjp1bXZ6Ld2DHM-E0VbtjYdlz_M2ZkU6WfSL4jGBcngeMC0ZyTJeDK5zTN9kx4azMGRX07cu74O-y9yHcYbwI5Dj7c7n34xytd8h3SFvVG2eibVHrnbaLHpByGjUzWDWiwYbo4YCsQ19nF0P6CtGkajudoQ5UG2cwGq26dyagL7fTZADdDNYZtAXVGHeaSH-fPPJg44z-_ibV9TL9YVYQfz2N43gD56zeAOqNbwfwzo--PyzUj7wzow6TAuT3Bnrwj3EIH7KjTo3BfHy-T7Lbb5c_L67y3fX2-8Vml7eUU5qTRtOKdWkLI3AlSF0pzKlgXcmxbsqac1q3rNHMCMaw0kyUXBBW8oZpSuqGnWSnq--gRjmBvVdwkF5ZebXZyUXDrBCM13RPEvt5ZSfwD7MJUd75GVxaT9KiKmouimqh6Eq14EMA073YEiyXcOUarkzhyqdwJU1NbG0KCXa9gVfr_3T9A_uhqO4</recordid><startdate>20211101</startdate><enddate>20211101</enddate><creator>Bossennec, Claire</creator><creator>Géraud, Yves</creator><creator>Böcker, Johannes</creator><creator>Klug, Bernd</creator><creator>Mattioni, Luca</creator><creator>Sizun, Jean-Pierre</creator><creator>Sudo, Masafumi</creator><creator>Moretti, Isabelle</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><general>Springer Verlag</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0003-3227-4869</orcidid></search><sort><creationdate>20211101</creationdate><title>Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths</title><author>Bossennec, Claire ; Géraud, Yves ; Böcker, Johannes ; Klug, Bernd ; Mattioni, Luca ; Sizun, Jean-Pierre ; Sudo, Masafumi ; Moretti, Isabelle</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2422-1bd283fabee6086198a04263f740db794429c3bd3e6330ad367461374b3d219b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Allochthonous deposits</topic><topic>Cementation</topic><topic>Cenozoic</topic><topic>Diagenesis</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Sciences</topic><topic>Evolution</topic><topic>Feldspars</topic><topic>Fluids</topic><topic>Geochemistry</topic><topic>Geochronology</topic><topic>Geochronometry</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Graben</topic><topic>Intergranular fracture</topic><topic>Isotopes</topic><topic>Jurassic</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Original Paper</topic><topic>Quartz</topic><topic>Radiometric dating</topic><topic>Sandstone</topic><topic>Sciences of the Universe</topic><topic>Sedimentary rocks</topic><topic>Sedimentology</topic><topic>Structural Geology</topic><topic>Temperature</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bossennec, Claire</creatorcontrib><creatorcontrib>Géraud, Yves</creatorcontrib><creatorcontrib>Böcker, Johannes</creatorcontrib><creatorcontrib>Klug, Bernd</creatorcontrib><creatorcontrib>Mattioni, Luca</creatorcontrib><creatorcontrib>Sizun, Jean-Pierre</creatorcontrib><creatorcontrib>Sudo, Masafumi</creatorcontrib><creatorcontrib>Moretti, Isabelle</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>International journal of earth sciences : Geologische Rundschau</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bossennec, Claire</au><au>Géraud, Yves</au><au>Böcker, Johannes</au><au>Klug, Bernd</au><au>Mattioni, Luca</au><au>Sizun, Jean-Pierre</au><au>Sudo, Masafumi</au><au>Moretti, Isabelle</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths</atitle><jtitle>International journal of earth sciences : Geologische Rundschau</jtitle><stitle>Int J Earth Sci (Geol Rundsch)</stitle><date>2021-11-01</date><risdate>2021</risdate><volume>110</volume><issue>8</issue><spage>2779</spage><epage>2802</epage><pages>2779-2802</pages><issn>1437-3254</issn><eissn>1437-3262</eissn><abstract>In-situ δ
18
O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs within the Upper Rhine Graben. The overgrowths record two types of the evolution of δ
18
O: 1) a monotonous decrease of the δ
18
O
overgrowth
interpreted as linked to an increasing burial temperature and 2) random fluctuations, interpreted as pointing out the injection of allochthonous fluids in faulted areas, on the cementation processes of the pore network (both intergranular and fracture planes). Fluids causing the quartz cementation are either autochthonous buffered in
18
O from clay illitisation; or allochthonous fluids of meteoric origin with δ
18
O below − 5%. These allochthonous fluids are in thermal disequilibrium with the host sandstone. The measured signal of δ
18
O
overgrowth
measured from samples and calculated curves testing hypothetic δ
18
O
fluid
are compared to T–t evolution during burial. This modelling proposes the initiation of quartz cementation during the Jurassic and is validated by the in-situ
40
Ar/
39
Ar dating results obtained on the feldspar overgrowths predating quartz overgrowths. A similar diagenetic history is recorded on the graben shoulders and in the buried parts of the basin. Here, the beginning of the pore network cementation predates the structuration in blocks of the basin before the Cenozoic graben opening.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00531-021-02080-2</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0003-3227-4869</orcidid><oa>free_for_read</oa></addata></record> |
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| ispartof | International journal of earth sciences : Geologische Rundschau, 2021-11, Vol.110 (8), p.2779-2802 |
| issn | 1437-3254 1437-3262 |
| language | eng |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | Allochthonous deposits Cementation Cenozoic Diagenesis Earth and Environmental Science Earth Sciences Environmental Sciences Evolution Feldspars Fluids Geochemistry Geochronology Geochronometry Geology Geophysics/Geodesy Graben Intergranular fracture Isotopes Jurassic Mineral Resources Mineralogy Original Paper Quartz Radiometric dating Sandstone Sciences of the Universe Sedimentary rocks Sedimentology Structural Geology Temperature |
| title | Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths |
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