在秘鲁南部海岸沿线的晚期前坎布里亚变态地下室中,有20亿年历史的颗粒
概括
与的约会揭示了秘鲁20亿年前的一次orogenic事件. 这个古老的变形复合体影响着现代的火山活动,影响了秘鲁-智利沟沿线的同位素比率.
科学领域:
- 地质地质地质地质地质地
- 地质年代学地质年代学.
- 石化学 石化学是一门学科.
背景情况:
- 秘鲁沿海地区的特点是一个中等级的变态复合体,具有高压颗粒体和charnockitic组件.
- 了解这个综合体的地质历史对于解释区域地质化学异常至关重要.
研究的目的:
- 为了确定秘鲁沿海地区的变态核的年龄.
- 为了研究古老的orogenic事件和最近的火山地质化学之间的关系.
主要方法:
- - (U-Pb) 同位素约会被用来确定变态岩石的年龄.
- 地质化学分析,特别是同位素比率,用于研究最近的火山活动.
主要成果:
- -数据表明,颗粒和charnockitic核与大约20亿年前的一次orogenic事件有关.
- 这座古老的颗粒岩地下室已经通过晚期前坎布里亚时期的orogeny进行了改造.
- 这个古老的地下室的存在是解释最近的-火山活动中观察到的高同位素比率的一个重要因素.
结论:
- 秘鲁海岸的变态复合体有着深厚的前坎布里亚时代的根源,与20亿年前的一次orogenic事件有关.
- 在晚期前坎布里亚时期对这个古老的地下室的改造影响了现代火山运动的地化学特征.
- 地质历史,包括古老的地质事件和地下层构成,对于理解该地区火山弧中的同位素异常至关重要.
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