南安第斯高原 (中部普纳),阿根廷西北部的米奥森地表升起和orogenic进化
Heiko Pingel1, Ricardo N Alonso2, Bodo Bookhagen1
1Universität Potsdam, Institut für Geowissenschaften, Potsdam14476, Germany.
概括
稳定同位素和放射测年法揭示了波西托斯盆地2公里的表面升起和持续缩短,挑战了以前的普纳高原升高和盆地形成模型.
科学领域:
- 地质科学 地质科学
- 构造学 构造学 构造学 构造学
- 地质时间学 (Geochronology)
背景情况:
- 讨论了普纳高原的海拔历史和山间盆地形成的机制.
- 之前的研究表明,高海拔地区自欧森时代以来,通过石质层沉形成盆地.
研究的目的:
- 调查波西托斯盆地表面升起和缩短的时间和程度.
- 为了协调有关普纳高原构造演变的相互矛盾的数据.
主要方法:
- 对火山玻璃 (δD) 的稳定同位素分析.
- 放射测年法:U-Pb,U-Th,以及AMS 14C. 这些都是放射测年法.
- 对变形沉积物沉积物的分析.
主要成果:
- 证据表明,自中期至中期米欧纪末期以来,地表升起了2公里.
- 长期地缩持续到今天.
- 与其他普纳部门相比,对比构造学设置.
结论:
- 中部普纳的山间盆地形成是由于地缩缩短的结果,自20万年前.
- 快速地表升起可能与石层层分层有关.
- 这些发现挑战了普纳高原升起和盆地发展的长期模型.
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