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FORMATIVE MECHANISM OF AKAISHI MOUNTAINS AND ENREI BASIN IN CENTRAL JAPAN

机译:日本中部赤石山与恩里盆地的形成机制

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摘要

@@ 1 IntroductionrnIt is common in mobile belts that uplifting mountains are neighbored by synchronously subsiding basins.The coupling mechanism of such subsidence and uplift is an important target to clarify the dynamics of mobile belts.We investigate the coupled mountain uplift and basin subsidence in the Central Japan highland,the junction of three island arcs (the Northeast Japan,the Southwest Japan and the Izu-Ogasawara arcs).The highland over 3 000 m in height is composed of mountain ranges,plateaus and intramountain basins (Fig.1).
机译:@@ 1引言隆起的山体通常被同步沉降的盆地所包围,这在流动带中是很常见的,这种沉降与隆起的耦合机制是弄清流动带动力学的重要目标。日本中部的高地,三个岛弧的交界处(日本东北,日本西南和伊豆小ara原弧)。海拔超过3000 m的高地由山脉,高原和山间盆地组成(图1)。

著录项

  • 来源
    《大地构造与成矿学(英文版)》 |2001年第1期|45-50|共6页
  • 作者

    Yasuuchi KUBOTA; Takao YANO;

  • 作者单位

    Oyo Co.Ltd.,3-1-30 Minaga,Saeki-ku,Hiroshima,731-5124,Japan;

    Department of Environmental Science,Faculty of Education and Regional Science,Tottori University,Tottori,680-8551,Japan;

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  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 构造运动;
  • 关键词

  • 入库时间 2022-08-19 03:55:18
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