北美大陆的排水在法纳热纪期间,来自同位素的
1P. J. Patchett, Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA. E-mail: patchett@geo.arizona.edu. G. M. Ross, Geological Survey of Canada, 3303 33rd Street NW, Calgary AB T2L 2A7, Canada. J. D. Gleason, Lunar and Planetary La.
概括
的同位素数据显示,北美沉积岩的来源随着时间的推移发生了显著变化. 古代盾牌早期占主导地位,其次是卡莱多尼亚-阿巴拉契亚山脉,后来是西 Cordillera.
科学领域:
- 地质化学 地质化学
- 沉积地质的地质学
- 同位素地质学 同位素地质学
背景情况:
- 沉积岩记录了它们来源地区的历史.
- 了解沉积物来源是重建古地理和构造事件的关键.
研究的目的:
- 用新 (Nd) 同位素追踪北美沉积岩的来源.
- 为了确定过去6亿年来主要沉积物供应变化的时间表.
主要方法:
- 在沉积岩中分析 (Nd) 的同位素组成.
- 解释同位素特征以识别沉积物来源和运输途径.
主要成果:
- 一致的Nd同位素图案表明,大陆级沉积物来源于北美.
- 古代大陆盾源在6亿至4.5亿年前 (Ma) 占主导地位.
- 来自喀里多尼亚-阿巴拉契亚山脉的碎片在450万年前左右成为主导,持续到大约150万年前,可能是由于沉积岩的回收利用.
- 大约150万年前,西 Cordillera 的出现将新的碎片引入了系统.
结论:
- 新同位素为追踪长期沉积物来源变化提供了强大的工具.
- 北美沉积源的历史反映了主要的构造事件和古地理重建.
- 沉积物回收在掩盖或延长主要沉积物来源的信号方面发挥着重要作用.
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