日本西南爱媛县Hiji kawa河沿岸河流阶地的地质年代检验和地貌演化——基于地形连续性和砾石风化程度

IF 0.2 Q4 GEOGRAPHY, PHYSICAL
M. Yanagida, M. Ikeda, N. Nishizaka, K. Onishi, K. Kimura
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引用次数: 0

摘要

为了从河流阶地面分布中揭示区域地壳变形,需要基于阶地精确对比和年代学检验的河流阶地剖面。穿插或覆盖在阶地沉积物上的阶地层被用作准确关联阶地表面的有益信息。另一方面,在缺乏低温沉积物的情况下,阶地表面的对比主要基于地貌特征(如解剖程度、相对高程)和地质特征(如沉积物相、阶地砾石风化程度)。根据每项研究中定义的标准,基于定性指标的阶地表面相关性可能导致不确定性或变异性。在本研究中,引入了阶地沉积物中砾石风化程度作为另一个定量指标来验证或补偿阶地表面相关性。检查流程如下:研究对象为四国西部的Hiji-kawa河,沿河分布着多个阶地面(P、HH、H、M、L)。阶地沉积物中很少有低温沉积。0.6 Ma的温层嵌套在P面矿床的上部。0.3 Ma tephra嵌套在Hf1表面矿床上部。对火山灰颗粒的分析表明,M表面覆盖着Aso-4火山灰(85 ~ 90ka)。首先,其他非老化阶地表面的年龄是根据与老化阶地的高度差来估计的。其次,测量了从15个阶地沉积物阶段收集的几种砾石的实际密度值。最后,将实际密度测量值归一化为当前河床砾石的实测值。相对密度值(RDV)显示负软木*株式会社阪神コンサルタンツ* *株式会社四国総合研究所* * *四国電力株式会社* * * *株式会社ナイバ+現所属:ケイジオ*阪神顾问有限公司,有限公司,东京,101 - 0037年,日本* *四国研究所INC .,高松,761 - 0192年,日本* * *四国电力有限公司,高松,760 - 8573年,日本* * * * Naiba有限公司,有限公司,高松,763 - 0062年,日本+目前地址:K-Geo,松山,791 - 1101年,日本地学雑誌地理杂志》(Chigaku Zasshi) 2022 131 (5) 521 - 544 . doi: 10.5026 / jgeography.131.521
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochronological Examination and Geomorphic Evolution of River Terraces Distributed along the Hiji-kawa River in Ehime Prefecture, Southwest Japan: Based on Topographic Continuity and Weathered Degree of Gravels
Terrace profiles along rivers based on accurate correlations of terraces and geochronological examination are needed to reveal regional crustal deformation from the distribution of river terrace surfaces. Tephra beds, which are intercalated or cover terrace sediments, are used as beneficial information to correlate terrace surfaces accurately. On the other hand, in cases lacking tephric sediments, the correlation of terrace surfaces is mainly based on geomorphic characteristics, such as degree of dissection, relative elevation, and geologic properties, such as facies of sediments and weathered degree of terrace gravels. A terrace surface correlation based on qualitative indicators may cause uncertainty or variability depending on the criteria defined in each study. In this research, weathered degree of gravels in terrace sediments is introduced as another quantitative indicator to validate or compensate for the terrace surface correlation. The examination process is as follows. The research target is the Hiji-kawa River in western Shikoku, along which many terrace surfaces (P, HH, H, M, and L) are distributed. Few tephric sediments exist in terrace sediments. The 0.6 Ma tephra is intercalated at the upper part of P Surface deposits. 0.3 Ma tephra is intercalated at the upper part of Hf1 Surface deposits. An analysis of volcanic ash grains suggests that M surfaces are covered with Aso-4 tephra (85 to 90 ka). First, the ages of other non-aged-terrace surfaces are estimated based on height differences from aged-terraces. Second, real density values are measured for several gravels collected from 15 stages of terrace sediments. Finally, measured real density values are normalized by measured values of current riverbed gravels. Relative density values (RDV) show a negative cor* 株式会社阪神コンサルタンツ ** 株式会社四国総合研究所 *** 四国電力株式会社 **** 株式会社ナイバ + 現所属:ケイジオ * Hanshin Consultants CO., LTD., Tokyo, 101-0037, Japan ** Shikoku Research Institute INC., Takamatsu, 761-0192, Japan *** Shikoku Electric Power Co., INC., Takamatsu, 760-8573, Japan **** Naiba CO., LTD., Takamatsu, 763-0062, Japan + Present address: K-Geo, Matsuyama, 791-1101, Japan 地学雑誌 Journal of Geography(Chigaku Zasshi) 131(5)521­544 2022 doi:10.5026/jgeography.131.521
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CiteScore
1.50
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33.30%
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28
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