Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams
The distribution of composition fields of syn-rift and syncollisional sandstones and fine-grained clastic/clayey rocks of various structures and different ages are compared on the SiO 2 –K 2 O/Na 2 O, F1–F2, and DF1–DF2 diagrams. Syn-rift sedimentary sequences fill intraplate rifts, rifts at diverge...
Gespeichert in:
| Veröffentlicht in: | Geochemistry international 2021-02, Vol.59 (2), p.113-126 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 126 |
|---|---|
| container_issue | 2 |
| container_start_page | 113 |
| container_title | Geochemistry international |
| container_volume | 59 |
| creator | Maslov, A. V. Podkovyrov, V. N. |
| description | The distribution of composition fields of syn-rift and syncollisional sandstones and fine-grained clastic/clayey rocks of various structures and different ages are compared on the SiO
2
–K
2
O/Na
2
O, F1–F2, and DF1–DF2 diagrams. Syn-rift sedimentary sequences fill intraplate rifts, rifts at divergent, conservative and convergent plate boundaries, as well as their triple junctions. Syncollisional sediments are referred to rocks of foredeep and intermontane troughs, which are made up of molasses proper, flysch and schliers, and volcanogenic and nonfolded (distal) molasses. Fields of syn-rift and syncollisional sandstones in the SiO
2
–K
2
O/Na
2
O diagram show significant overlap. In the F1–F2 and DF1–DF2 diagrams, the distribution of the fields of syn-rift and syncollisional fine-grained clastic/clayey rocks is also substantially similar. Hence, the above mentioned diagrams cannot be used for reliable discrimination between syn-rift and syncollisional terrigenous associations. Correspondingly, it is hardly possible to use these diagrams alone for determination of geodynamic nature of sediments. |
| doi_str_mv | 10.1134/S0016702921020051 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_journals_2491962957</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A720567541</galeid><sourcerecordid>A720567541</sourcerecordid><originalsourceid>FETCH-LOGICAL-a378t-b54e68e2031534b2887227f2cc3647dc06077b14c1c1383d2c1cbe85bd8c6c6a3</originalsourceid><addsrcrecordid>eNp1kU1LAzEQhoMoWKs_wNuC5635zu6xtH5BwWL1vGSzSUm7TWqyHvz3Tq3gQSSHDPO-z_Ayg9A1wRNCGL9dYUykwrSmBFOMBTlBIyKELEktq1M0OsjlQT9HFzlvMOac1WqEtsuY_eBjKKIrXqLZ5u_CuyGubfCm0KErZrHvfQaT7ouV7fzOhkGnT6jfP2wwFphQzL1zNoFSLHVvgY7dZ9A7GDH3ep30Ll-iM6f7bK9-_jF6u797nT2Wi-eHp9l0UWqmqqFsBbeyshQzIhhvaVUpSpWjxjDJVWewxEq1hBtiCKtYR6FobSXarjLSSM3G6OY4d58iBMxDs4kfCcLnhvIaFkJrocA1ObrWELfxwcUhaQOvsxA6Bus89KeKYiGV4AQAcgRMijkn65p98jvYQ0NwczhC8-cIwNAjk8Eb1jb9Rvkf-gKCIoh-</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2491962957</pqid></control><display><type>article</type><title>Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams</title><source>SpringerLink Journals</source><creator>Maslov, A. V. ; Podkovyrov, V. N.</creator><creatorcontrib>Maslov, A. V. ; Podkovyrov, V. N.</creatorcontrib><description>The distribution of composition fields of syn-rift and syncollisional sandstones and fine-grained clastic/clayey rocks of various structures and different ages are compared on the SiO
2
–K
2
O/Na
2
O, F1–F2, and DF1–DF2 diagrams. Syn-rift sedimentary sequences fill intraplate rifts, rifts at divergent, conservative and convergent plate boundaries, as well as their triple junctions. Syncollisional sediments are referred to rocks of foredeep and intermontane troughs, which are made up of molasses proper, flysch and schliers, and volcanogenic and nonfolded (distal) molasses. Fields of syn-rift and syncollisional sandstones in the SiO
2
–K
2
O/Na
2
O diagram show significant overlap. In the F1–F2 and DF1–DF2 diagrams, the distribution of the fields of syn-rift and syncollisional fine-grained clastic/clayey rocks is also substantially similar. Hence, the above mentioned diagrams cannot be used for reliable discrimination between syn-rift and syncollisional terrigenous associations. Correspondingly, it is hardly possible to use these diagrams alone for determination of geodynamic nature of sediments.</description><identifier>ISSN: 0016-7029</identifier><identifier>EISSN: 1556-1968</identifier><identifier>DOI: 10.1134/S0016702921020051</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Distribution ; Earth and Environmental Science ; Earth Sciences ; Fields ; Flysch ; Geochemistry ; Molasses ; Plate boundaries ; Potassium oxides ; Rock ; Rocks ; Sandstone ; Sediment ; Sediments ; Silica ; Silicon dioxide ; Syrups & sweeteners ; Terrigenous sediments ; Triple junctions</subject><ispartof>Geochemistry international, 2021-02, Vol.59 (2), p.113-126</ispartof><rights>Pleiades Publishing, Ltd. 2021. ISSN 0016-7029, Geochemistry International, 2021, Vol. 59, No. 2, pp. 113–126. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Geokhimiya, 2021, Vol. 66, No. 2, pp. 99–113.</rights><rights>COPYRIGHT 2021 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a378t-b54e68e2031534b2887227f2cc3647dc06077b14c1c1383d2c1cbe85bd8c6c6a3</citedby><cites>FETCH-LOGICAL-a378t-b54e68e2031534b2887227f2cc3647dc06077b14c1c1383d2c1cbe85bd8c6c6a3</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/S0016702921020051$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0016702921020051$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41466,42535,51296</link.rule.ids></links><search><creatorcontrib>Maslov, A. V.</creatorcontrib><creatorcontrib>Podkovyrov, V. N.</creatorcontrib><title>Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams</title><title>Geochemistry international</title><addtitle>Geochem. Int</addtitle><description>The distribution of composition fields of syn-rift and syncollisional sandstones and fine-grained clastic/clayey rocks of various structures and different ages are compared on the SiO
2
–K
2
O/Na
2
O, F1–F2, and DF1–DF2 diagrams. Syn-rift sedimentary sequences fill intraplate rifts, rifts at divergent, conservative and convergent plate boundaries, as well as their triple junctions. Syncollisional sediments are referred to rocks of foredeep and intermontane troughs, which are made up of molasses proper, flysch and schliers, and volcanogenic and nonfolded (distal) molasses. Fields of syn-rift and syncollisional sandstones in the SiO
2
–K
2
O/Na
2
O diagram show significant overlap. In the F1–F2 and DF1–DF2 diagrams, the distribution of the fields of syn-rift and syncollisional fine-grained clastic/clayey rocks is also substantially similar. Hence, the above mentioned diagrams cannot be used for reliable discrimination between syn-rift and syncollisional terrigenous associations. Correspondingly, it is hardly possible to use these diagrams alone for determination of geodynamic nature of sediments.</description><subject>Distribution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fields</subject><subject>Flysch</subject><subject>Geochemistry</subject><subject>Molasses</subject><subject>Plate boundaries</subject><subject>Potassium oxides</subject><subject>Rock</subject><subject>Rocks</subject><subject>Sandstone</subject><subject>Sediment</subject><subject>Sediments</subject><subject>Silica</subject><subject>Silicon dioxide</subject><subject>Syrups & sweeteners</subject><subject>Terrigenous sediments</subject><subject>Triple junctions</subject><issn>0016-7029</issn><issn>1556-1968</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1kU1LAzEQhoMoWKs_wNuC5635zu6xtH5BwWL1vGSzSUm7TWqyHvz3Tq3gQSSHDPO-z_Ayg9A1wRNCGL9dYUykwrSmBFOMBTlBIyKELEktq1M0OsjlQT9HFzlvMOac1WqEtsuY_eBjKKIrXqLZ5u_CuyGubfCm0KErZrHvfQaT7ouV7fzOhkGnT6jfP2wwFphQzL1zNoFSLHVvgY7dZ9A7GDH3ep30Ll-iM6f7bK9-_jF6u797nT2Wi-eHp9l0UWqmqqFsBbeyshQzIhhvaVUpSpWjxjDJVWewxEq1hBtiCKtYR6FobSXarjLSSM3G6OY4d58iBMxDs4kfCcLnhvIaFkJrocA1ObrWELfxwcUhaQOvsxA6Bus89KeKYiGV4AQAcgRMijkn65p98jvYQ0NwczhC8-cIwNAjk8Eb1jb9Rvkf-gKCIoh-</recordid><startdate>20210201</startdate><enddate>20210201</enddate><creator>Maslov, A. V.</creator><creator>Podkovyrov, V. N.</creator><general>Pleiades Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20210201</creationdate><title>Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams</title><author>Maslov, A. V. ; Podkovyrov, V. N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a378t-b54e68e2031534b2887227f2cc3647dc06077b14c1c1383d2c1cbe85bd8c6c6a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Distribution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fields</topic><topic>Flysch</topic><topic>Geochemistry</topic><topic>Molasses</topic><topic>Plate boundaries</topic><topic>Potassium oxides</topic><topic>Rock</topic><topic>Rocks</topic><topic>Sandstone</topic><topic>Sediment</topic><topic>Sediments</topic><topic>Silica</topic><topic>Silicon dioxide</topic><topic>Syrups & sweeteners</topic><topic>Terrigenous sediments</topic><topic>Triple junctions</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Maslov, A. V.</creatorcontrib><creatorcontrib>Podkovyrov, V. N.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</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>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geochemistry international</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Maslov, A. V.</au><au>Podkovyrov, V. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams</atitle><jtitle>Geochemistry international</jtitle><stitle>Geochem. Int</stitle><date>2021-02-01</date><risdate>2021</risdate><volume>59</volume><issue>2</issue><spage>113</spage><epage>126</epage><pages>113-126</pages><issn>0016-7029</issn><eissn>1556-1968</eissn><abstract>The distribution of composition fields of syn-rift and syncollisional sandstones and fine-grained clastic/clayey rocks of various structures and different ages are compared on the SiO
2
–K
2
O/Na
2
O, F1–F2, and DF1–DF2 diagrams. Syn-rift sedimentary sequences fill intraplate rifts, rifts at divergent, conservative and convergent plate boundaries, as well as their triple junctions. Syncollisional sediments are referred to rocks of foredeep and intermontane troughs, which are made up of molasses proper, flysch and schliers, and volcanogenic and nonfolded (distal) molasses. Fields of syn-rift and syncollisional sandstones in the SiO
2
–K
2
O/Na
2
O diagram show significant overlap. In the F1–F2 and DF1–DF2 diagrams, the distribution of the fields of syn-rift and syncollisional fine-grained clastic/clayey rocks is also substantially similar. Hence, the above mentioned diagrams cannot be used for reliable discrimination between syn-rift and syncollisional terrigenous associations. Correspondingly, it is hardly possible to use these diagrams alone for determination of geodynamic nature of sediments.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0016702921020051</doi><tpages>14</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0016-7029 |
| ispartof | Geochemistry international, 2021-02, Vol.59 (2), p.113-126 |
| issn | 0016-7029 1556-1968 |
| language | eng |
| recordid | cdi_proquest_journals_2491962957 |
| source | SpringerLink Journals |
| subjects | Distribution Earth and Environmental Science Earth Sciences Fields Flysch Geochemistry Molasses Plate boundaries Potassium oxides Rock Rocks Sandstone Sediment Sediments Silica Silicon dioxide Syrups & sweeteners Terrigenous sediments Triple junctions |
| title | Position of Rocks of Riftogenic and Collisional Sedimentary Sequences on Different Paleogeodynamic Diagrams |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-28T08%3A50%3A19IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Position%20of%20Rocks%20of%20Riftogenic%20and%20Collisional%20Sedimentary%20Sequences%20on%20Different%20Paleogeodynamic%20Diagrams&rft.jtitle=Geochemistry%20international&rft.au=Maslov,%20A.%20V.&rft.date=2021-02-01&rft.volume=59&rft.issue=2&rft.spage=113&rft.epage=126&rft.pages=113-126&rft.issn=0016-7029&rft.eissn=1556-1968&rft_id=info:doi/10.1134/S0016702921020051&rft_dat=%3Cgale_proqu%3EA720567541%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2491962957&rft_id=info:pmid/&rft_galeid=A720567541&rfr_iscdi=true |