马菲石板融对原生纪大山脉类型非正方位的贡献
Duncan S Keller1, Cin-Ty A Lee1, William H Peck2
1Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX 77005, USA.
Science advances
|August 14, 2024
概括
巨峰类型的无线岩石由来自海洋地的变化而形成的地融化而形成. 这项研究将它们的形成与大陆边缘下的俯冲过程联系起来,解释了它们的时间限制.
科学领域:
- 地质地质地质地质地质地
- 石化学 石化学是一门学科.
- 同位素地球化学 同位素地球化学
背景情况:
- 大类型的异构体是大型的,神秘的,富含质质的入物,位于地球地中.
- 它们的形成,主要是在10亿至20亿年前,是有争议的,其中包括地幔融化,下地融化和弧形岩主义等假设.
- 之前的研究尚未就父母岩或其时间限制的原因达成共识.
研究的目的:
- 为了研究大岩类型无正岩石的父母岩石的起源.
- 为了了解大岩类型的无正岩石形成的时间限制.
- 为了阐明anorthosite大山位位的构造学设置.
主要方法:
- 对B,O,Nd和Sr同位素的分析.
- 大量化学分析.
- 石油产物学模型.
主要成果:
- 马西和莫林无极岩,北美关键的例子,起源于岩,有显著的输入来自从改变的海洋地中获得的巨型融.
- 同位素的签名表明了沉积板块石质的参与,例如蛇形岩.
- 这一发现表明,甲基体形成和潜水过程之间存在遗传联系.
结论:
- 巨峰类型的异构岩石,形成在汇聚的大陆边缘下方.
- 沉积或沉积板块的大量化提供了父母岩石.
- 岩岩石巨层的形成与地球的热和构造进化有关,特别是在显著的沉降活动期间.
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