Sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan
In this paper, we discuss depositional process and sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan. On the basis of sedimentary facies and fossil data such as molluscan and diatom assemblages, the Kioroshi Format...
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| Veröffentlicht in: | Chishitsugaku zasshi 2006, Vol.112(5), pp.349-368 |
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| container_title | Chishitsugaku zasshi |
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| creator | Nakazawa, Tsutomu Nakashima, Rei Ueki, Takeyuki Tanabe, Susumu Oshima, Hideaki Horiuchi, Seiji |
| description | In this paper, we discuss depositional process and sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan. On the basis of sedimentary facies and fossil data such as molluscan and diatom assemblages, the Kioroshi Formation can be subdivided into the lower and upper parts which were formed by a incised-valley system and a barrier-island system, respectively. Each part represents successive upward-fining and upward-coarsening units composed mainly of mud and/or thin-interbedded sand and mud. Based on the correlation between pollen zones, tephrochronology, and the MIS curve, the lower part is considered to have deposited during the sea-level rise of MIS 6 to early MIS 5e and most of the upper part during the gentle sea-level fall of late MIS 5e. The sea levels suggest that the incised-valley system is interpreted as lowstand and transgressive systems tracts and the barrier island system as a highstand systems tract. |
| doi_str_mv | 10.5575/geosoc.112.349 |
| format | Article |
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On the basis of sedimentary facies and fossil data such as molluscan and diatom assemblages, the Kioroshi Formation can be subdivided into the lower and upper parts which were formed by a incised-valley system and a barrier-island system, respectively. Each part represents successive upward-fining and upward-coarsening units composed mainly of mud and/or thin-interbedded sand and mud. Based on the correlation between pollen zones, tephrochronology, and the MIS curve, the lower part is considered to have deposited during the sea-level rise of MIS 6 to early MIS 5e and most of the upper part during the gentle sea-level fall of late MIS 5e. 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The sea levels suggest that the incised-valley system is interpreted as lowstand and transgressive systems tracts and the barrier island system as a highstand systems tract.</description><subject>Bacillariophyceae</subject><subject>central Kanto</subject><subject>depositional system</subject><subject>Kioroshi Formation</subject><subject>Mollusca</subject><subject>Pleistocene</subject><subject>pollen assemblage</subject><subject>sequence stratigraphy</subject><issn>0016-7630</issn><issn>1349-9963</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNpdkUFP3DAQha2qSF0B154tVeqJbO04duJjRQstIIEEnK1ZZ7IxSuzU9h72F_C367KIVr3MSOPvPc34EfKRs7WUrfyyxZCCXXNer0Wj35EVL63SWon3ZMUYV1WrBPtATlNyG8aYFkq09Yo83-OvHXqLNOUI2W0jLOOehoHmEendhC7lYNEjvXYhhjQ6ehHiXMjgz-j96OaQgF7GsFvopmCQxxfl7ez2QB-XCXx_RotBcZ_oNfgciis4_3d4BQv4E3I0wJTw9LUfk8eL7w_nP6qb28uf519vKqhVqyslOwkt9I3oVd1JZC1qKep-sFzjoKTedKwVHFnd27YDhSCUsr2WANaiFuKYfD74LjGUw1M2s0sWp7Inhl0yNeukZB0r4Kf_wKewi77sZnjT6EY2UnWFWh8oW_4mRRzMEt0McW84M3-CMYdgTAnGlESK4NtB8JQybPENh5idnfBfXL7WInt7tiNEg178BhiqnBM</recordid><startdate>20060101</startdate><enddate>20060101</enddate><creator>Nakazawa, Tsutomu</creator><creator>Nakashima, Rei</creator><creator>Ueki, Takeyuki</creator><creator>Tanabe, Susumu</creator><creator>Oshima, Hideaki</creator><creator>Horiuchi, Seiji</creator><general>The Geological Society of Japan</general><general>Japan Science and Technology Agency</general><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>M7N</scope></search><sort><creationdate>20060101</creationdate><title>Sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan</title><author>Nakazawa, Tsutomu ; Nakashima, Rei ; Ueki, Takeyuki ; Tanabe, Susumu ; Oshima, Hideaki ; Horiuchi, Seiji</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2679-6585a7ad43d6285e07e9532dfc19ef659b80731e02dc78a6ea366cd95aacce933</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng ; jpn</language><creationdate>2006</creationdate><topic>Bacillariophyceae</topic><topic>central Kanto</topic><topic>depositional system</topic><topic>Kioroshi Formation</topic><topic>Mollusca</topic><topic>Pleistocene</topic><topic>pollen assemblage</topic><topic>sequence stratigraphy</topic><toplevel>online_resources</toplevel><creatorcontrib>Nakazawa, Tsutomu</creatorcontrib><creatorcontrib>Nakashima, Rei</creatorcontrib><creatorcontrib>Ueki, Takeyuki</creatorcontrib><creatorcontrib>Tanabe, Susumu</creatorcontrib><creatorcontrib>Oshima, Hideaki</creatorcontrib><creatorcontrib>Horiuchi, Seiji</creatorcontrib><collection>CrossRef</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><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Chishitsugaku zasshi</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Nakazawa, Tsutomu</au><au>Nakashima, Rei</au><au>Ueki, Takeyuki</au><au>Tanabe, Susumu</au><au>Oshima, Hideaki</au><au>Horiuchi, Seiji</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan</atitle><jtitle>Chishitsugaku zasshi</jtitle><addtitle>Jour. Geol. Soc. Japan</addtitle><date>2006-01-01</date><risdate>2006</risdate><volume>112</volume><issue>5</issue><spage>349</spage><epage>368</epage><pages>349-368</pages><issn>0016-7630</issn><eissn>1349-9963</eissn><abstract>In this paper, we discuss depositional process and sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan. On the basis of sedimentary facies and fossil data such as molluscan and diatom assemblages, the Kioroshi Formation can be subdivided into the lower and upper parts which were formed by a incised-valley system and a barrier-island system, respectively. Each part represents successive upward-fining and upward-coarsening units composed mainly of mud and/or thin-interbedded sand and mud. Based on the correlation between pollen zones, tephrochronology, and the MIS curve, the lower part is considered to have deposited during the sea-level rise of MIS 6 to early MIS 5e and most of the upper part during the gentle sea-level fall of late MIS 5e. The sea levels suggest that the incised-valley system is interpreted as lowstand and transgressive systems tracts and the barrier island system as a highstand systems tract.</abstract><cop>Tokyo</cop><pub>The Geological Society of Japan</pub><doi>10.5575/geosoc.112.349</doi><tpages>20</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Bacillariophyceae central Kanto depositional system Kioroshi Formation Mollusca Pleistocene pollen assemblage sequence stratigraphy |
| title | Sequence stratigraphy of the Pleistocene Kioroshi Formation, Shimosa Group beneath the Omiya Upland, central Kanto Plain, central Japan |
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