High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations
The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Guodong Wang [verfasserIn] Rihui Cheng [verfasserIn] Pujun Wang [verfasserIn] Youfeng Gao [verfasserIn] Chengshan Wang [verfasserIn] Yanguang Ren [verfasserIn] Qinghua Huang [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Übergeordnetes Werk: |
In: Geoscience Frontiers - Elsevier, 2016, 6(2015), 6, Seite 895-912 |
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| Übergeordnetes Werk: |
volume:6 ; year:2015 ; number:6 ; pages:895-912 |
| Links: |
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| DOI / URN: |
10.1016/j.gsf.2015.02.003 |
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DOAJ049938312 |
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| 245 | 1 | 0 | |a High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations |
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| 520 | |a The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. | ||
| 650 | 4 | |a Sifangtai Formation and Mingshui Formation | |
| 650 | 4 | |a Sedimentary facies | |
| 650 | 4 | |a Cyclostratigraphy | |
| 650 | 4 | |a SK-1n | |
| 650 | 4 | |a Middle Campanian-Danian | |
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| 700 | 0 | |a Yanguang Ren |e verfasserin |4 aut | |
| 700 | 0 | |a Qinghua Huang |e verfasserin |4 aut | |
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10.1016/j.gsf.2015.02.003 doi (DE-627)DOAJ049938312 (DE-599)DOAJc0a210547b3742518a635cbdb73c08b4 DE-627 ger DE-627 rakwb eng QE1-996.5 Guodong Wang verfasserin aut High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin Geology Rihui Cheng verfasserin aut Pujun Wang verfasserin aut Youfeng Gao verfasserin aut Chengshan Wang verfasserin aut Yanguang Ren verfasserin aut Qinghua Huang verfasserin aut In Geoscience Frontiers Elsevier, 2016 6(2015), 6, Seite 895-912 (DE-627)DOAJ000091189 25889192 nnns volume:6 year:2015 number:6 pages:895-912 https://doi.org/10.1016/j.gsf.2015.02.003 kostenfrei https://doaj.org/article/c0a210547b3742518a635cbdb73c08b4 kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987115000377 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA AR 6 2015 6 895-912 |
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10.1016/j.gsf.2015.02.003 doi (DE-627)DOAJ049938312 (DE-599)DOAJc0a210547b3742518a635cbdb73c08b4 DE-627 ger DE-627 rakwb eng QE1-996.5 Guodong Wang verfasserin aut High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin Geology Rihui Cheng verfasserin aut Pujun Wang verfasserin aut Youfeng Gao verfasserin aut Chengshan Wang verfasserin aut Yanguang Ren verfasserin aut Qinghua Huang verfasserin aut In Geoscience Frontiers Elsevier, 2016 6(2015), 6, Seite 895-912 (DE-627)DOAJ000091189 25889192 nnns volume:6 year:2015 number:6 pages:895-912 https://doi.org/10.1016/j.gsf.2015.02.003 kostenfrei https://doaj.org/article/c0a210547b3742518a635cbdb73c08b4 kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987115000377 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA AR 6 2015 6 895-912 |
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10.1016/j.gsf.2015.02.003 doi (DE-627)DOAJ049938312 (DE-599)DOAJc0a210547b3742518a635cbdb73c08b4 DE-627 ger DE-627 rakwb eng QE1-996.5 Guodong Wang verfasserin aut High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin Geology Rihui Cheng verfasserin aut Pujun Wang verfasserin aut Youfeng Gao verfasserin aut Chengshan Wang verfasserin aut Yanguang Ren verfasserin aut Qinghua Huang verfasserin aut In Geoscience Frontiers Elsevier, 2016 6(2015), 6, Seite 895-912 (DE-627)DOAJ000091189 25889192 nnns volume:6 year:2015 number:6 pages:895-912 https://doi.org/10.1016/j.gsf.2015.02.003 kostenfrei https://doaj.org/article/c0a210547b3742518a635cbdb73c08b4 kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987115000377 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA AR 6 2015 6 895-912 |
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10.1016/j.gsf.2015.02.003 doi (DE-627)DOAJ049938312 (DE-599)DOAJc0a210547b3742518a635cbdb73c08b4 DE-627 ger DE-627 rakwb eng QE1-996.5 Guodong Wang verfasserin aut High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin Geology Rihui Cheng verfasserin aut Pujun Wang verfasserin aut Youfeng Gao verfasserin aut Chengshan Wang verfasserin aut Yanguang Ren verfasserin aut Qinghua Huang verfasserin aut In Geoscience Frontiers Elsevier, 2016 6(2015), 6, Seite 895-912 (DE-627)DOAJ000091189 25889192 nnns volume:6 year:2015 number:6 pages:895-912 https://doi.org/10.1016/j.gsf.2015.02.003 kostenfrei https://doaj.org/article/c0a210547b3742518a635cbdb73c08b4 kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987115000377 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA AR 6 2015 6 895-912 |
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10.1016/j.gsf.2015.02.003 doi (DE-627)DOAJ049938312 (DE-599)DOAJc0a210547b3742518a635cbdb73c08b4 DE-627 ger DE-627 rakwb eng QE1-996.5 Guodong Wang verfasserin aut High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin Geology Rihui Cheng verfasserin aut Pujun Wang verfasserin aut Youfeng Gao verfasserin aut Chengshan Wang verfasserin aut Yanguang Ren verfasserin aut Qinghua Huang verfasserin aut In Geoscience Frontiers Elsevier, 2016 6(2015), 6, Seite 895-912 (DE-627)DOAJ000091189 25889192 nnns volume:6 year:2015 number:6 pages:895-912 https://doi.org/10.1016/j.gsf.2015.02.003 kostenfrei https://doaj.org/article/c0a210547b3742518a635cbdb73c08b4 kostenfrei http://www.sciencedirect.com/science/article/pii/S1674987115000377 kostenfrei https://doaj.org/toc/1674-9871 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA AR 6 2015 6 895-912 |
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QE1-996.5 High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations Sifangtai Formation and Mingshui Formation Sedimentary facies Cyclostratigraphy SK-1n Middle Campanian-Danian Songliao Basin |
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High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations |
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high resolution continuous sedimentary records of upper cretaceous obtained from the continental drilling (sk-1) borehole in songliao basin: sifangtai and mingshui formations |
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QE1-996.5 |
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High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations |
| abstract |
The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. |
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The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. |
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The Sifangtai and Mingshui formations were continuously cored in the SK-1n borehole (China Cretaceous Continental Scientific Drilling–SongKe1-the north borehole). The core is 767.96 m long, and the recovery is 94.7%. The ages of the formations range from middle Campanian to Danian. The sequence and process of lithology-lithofacies and cyclic stratigraphy were described in detail. Eight litho-types compose the Sifangtai Formation, and 15 litho-types compose the Mingshui Formation. Deposition was predominantly in meandering river and lacustrine environments, including 10 microfacies in the Sifangtai Formation and 15 microfacies in the Mingshui Formation. The complete sequence is composed of 535 m-scale cycles (sixth-order cycle), 152 fifth-order cycles, 42 fourth-order cycles and five third-order cycles. The centimeter-scale description of the section revealed some previously unknown horizons such as a special type of mudstone, marl, volcanic ash and favorable sand reservoirs in the formations. The new-found evidence is very important for the interpretation of the evolution of the basin, conditions such as lake oxic events, the K/Pg boundary, tectonism in the late sag basin stage, and the reservoir-cap rock assemblages in the shallow stratigraphy. |
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High resolution continuous sedimentary records of Upper Cretaceous obtained from the continental drilling (SK-1) borehole in Songliao Basin: Sifangtai and Mingshui Formations |
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