首页> 外文期刊>地質調查研究報告 >関東平野中央部,埼玉県菖蒲町で掘削された350mボーリングコア(GS-SB-1 )の層相と堆積物物性
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関東平野中央部,埼玉県菖蒲町で掘削された350mボーリングコア(GS-SB-1 )の層相と堆積物物性

机译:关东平原中部Sa玉县翔武町开挖的350m钻孔岩心(GS-SB-1)的生理和沉积特性

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A 350-m-long sediment core, the GS-SB-1, was recovered at Shobu Town, central Kanto plain. Thiscore was obtained to achieve a standard stratigraphy of the Lower to Upper Pleistocene subsurface geology inthe central Kanto plain. This paper describes basic lithofacies, tephras and physical properties of the GS-SB-1.Physical properties including density, elastic wave velocity, spontaneous potential, and electric resistivity weremeasured. Sixty-nine facies units (unit 1 to unit 69 in descending order) were identified and their relation tophysical properties was discussed. Thirty-nine tephras were found from GS-SB-1 core, and two of them correlateto the Ontake Pm-1 tephra (9.90-10.90m in depth, ca 100ka), and the Ks5 tephra (182.85-182.87m in depth).Stratigraphic boundary between the Shimosa Group and the Kazusa Group is situated between 165m and 184m indepth. Nine marine deposits were identified based on sedimentary facies and diatom assemblages reported by Nayaet al. (2009).
机译:在关东平原中部的Shobu镇,发现了一个350米长的沉积岩心GS-SB-1。获得该岩心是为了实现关东中部中下至上更新世地下地质的标准地层。本文介绍了GS-SB-1的基本岩相,特弗拉斯和物理性质,并测量了密度,弹性波速度,自发电势和电阻率等物理性质。识别了69个相单元(降序排列的单元1至单元69),并讨论了它们与物理性质的关系。从GS-SB-1岩心中发现了39颗特弗拉,其中两个与Ontake Pm-1特弗拉(深度9.90-10.90m,约100ka)和Ks5特弗拉(深度182.85-182.87m)相关。 Shimosa集团和Kazusa集团之间的地层边界位于165m至184m之间。根据Nayaet等人报道的沉积相和硅藻组合,确定了9个海洋沉积物。 (2009)。

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