自至少1350万年前以来,西藏中部出现了正常的断层
P M Blisniuk1, B R Hacker, J Glodny
1Institut für Geowissenschaften, Universität Potsdam, D-14415 Potsdam, Germany. blisniuk@rz.uni-potsdam.de
Nature
|August 9, 2001
概括
西藏中部的正常断层至少始于1350万年前,支持由深层地力学过程和地稀薄驱动的高原进化模型.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地质物理学 地质物理学
背景情况:
- 西藏高原的东西上层地稀薄是由涉及地潜在能量的增加或与之无关的地力学过程的模型解释的.
- 确定变形的时间对于评估这些构造模型至关重要.
研究的目的:
- 为了确定西藏中部正常故障发生的时间.
- 评估西藏高原演变现有的构造模型.
主要方法:
- 使用Rubidium-Strontium (Rb-Sr) 和Argon-Argon (40Ar-39Ar) 方法测定矿物化的年代.
- 分析西藏中部断层的数据.
主要成果:
- 在西藏中部,格拉本形成的最低年龄约为1350万年.
- 有证据表明,在藏族中,长期存在正常的断层活动.
结论:
- 这些发现支持将正常断层与平原下地力学过程联系起来的模型.
- 上层地的稀薄可能是由于西藏下方地和上层地幔的异质变化而增加的潜在能量造成的.
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