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泥河湾古湖的形成机制及其与早期古人类生存环境的关系

袁宝印 同号文 温锐林 王燕华

袁宝印, 同号文, 温锐林, 等, 2009. 泥河湾古湖的形成机制及其与早期古人类生存环境的关系. 地质力学学报, 15 (1): 77-87.
引用本文: 袁宝印, 同号文, 温锐林, 等, 2009. 泥河湾古湖的形成机制及其与早期古人类生存环境的关系. 地质力学学报, 15 (1): 77-87.
YUAN Bao-yin, TONG Hao-wen, WEN Rui-lin, et al., 2009. THE FORMATION MECHANISM OF THE NIHEWAN PALRO-LAKE AND ITS RELATIONSHIP WITH LIVING ENVIRONMENT FOR EARLY ANCIENT HUMEN. Journal of Geomechanics, 15 (1): 77-87.
Citation: YUAN Bao-yin, TONG Hao-wen, WEN Rui-lin, et al., 2009. THE FORMATION MECHANISM OF THE NIHEWAN PALRO-LAKE AND ITS RELATIONSHIP WITH LIVING ENVIRONMENT FOR EARLY ANCIENT HUMEN. Journal of Geomechanics, 15 (1): 77-87.

泥河湾古湖的形成机制及其与早期古人类生存环境的关系

基金项目: 

科技部基础性工作专项项目 2007FY110200

详细信息
    作者简介:

    袁宝印(1938-), 男, 研究员, 主要从事地貌与第四纪地层工作。E-mail:YBY16888@sina.com

  • 中图分类号: X141;P66;P52

THE FORMATION MECHANISM OF THE NIHEWAN PALRO-LAKE AND ITS RELATIONSHIP WITH LIVING ENVIRONMENT FOR EARLY ANCIENT HUMEN

  • 摘要: 泥河湾盆地位于汾渭裂谷系的东北端, 是裂谷系的重要组成部分。古近纪初恒山-大同一带发育软流圈上涌柱, 导致岩浆喷发和地壳变薄, 距今25~24 Ma, 阳原-石匣一带开始沉陷形成盆地, 北侧出现伸展造山带。受到挤压作用使盆地内地壳缩短并在盆地南侧形成台地。上新世末至早更新世为盆地沉陷最盛时期, 泥河湾古湖形成。距今2.0~0.8 Ma, 该地区为温和的温带气候环境, 有的时段为亚热带气候, 同时火山喷发的火山灰和风成沉积为盆地土壤提供了丰富矿物质养分, 湖泊周边地区动植物繁盛, 为早期古人类在此栖息提供了必要的条件。该裂谷型盆地是适于早期古人类生存和发展的地区, 泥河湾盆地将是我国最有可能发现早期古人类化石的地点。

     

  • 图  1  泥河湾盆地地貌与活动断裂图

    1.基岩山地;2.黄土台地;3.一级河流阶地;4.二级河流阶地;5.湖积台地;6.河漫滩:7.洪积扇;8.居民点:9.活动断裂

    Figure  1.  Geomorphological units and active faults in Nihewan Basin

    图  2  泥河湾盆地熊耳山-凤凰山地貌第四纪地质剖面图

    1.基岩; 2.砂砾石; 3.细砂; 4.亚砂土; 5.亚黏土; 6.古土壤; 7.离石黄土; 8.马兰黄土

    Figure  2.  Map showing geomorphology and Quaternary profile from Xiongershan Mountain to Fenghuangshan Mountain in the Nihewan Basin

    图  3  泥河湾盆地盆山耦合响应理论模型图(据邢作云等2005[10]修改)

    Figure  3.  Theoretical model of basin-mountain coupling response for the Nihewan Basin (Modified from Xing Zuo-yun et al 2005[10])

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  • 收稿日期:  2008-10-23
  • 刊出日期:  2009-03-01

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