安第斯类型的原始的前体岩,保存在岩混合区
Daniel Gómez-Frutos1, Antonio Castro2, Jesús de la Rosa3
1Museo Nacional de Ciencias Naturales (MNCN), Consejo Superior de Investigaciones Científicas (CSIC), C. José Gutiérrez Abascal 2, 28006, Madrid, Spain. daniel.gomez@csic.es.
Scientific reports
|February 29, 2024
概括
研究人员在岩混合区中确定了原始的中间球体,作为安第斯类型宝石石的潜在父母岩. 这些球体在塞维利亚发现,显示最小的分成,提供了一个独特的窗口到早期的岩组成.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 火山学 火山学是一门学科.
背景情况:
- 中间岩组成越来越多地被认为是安第斯类型岩的父母.
- 之前的地质化学和实验研究已经为这些巴索利石建模了假设的父母组成.
- 匹配这些模拟组合的天然浮动样本很少,这是由于巴索石内部的广泛分化.
研究的目的:
- 为了研究塞维利亚西埃拉诺尔特巴索利石中格雷纳岩混合区内的中间岩.
- 为了分析灭的黑色球体和宿主颗粒石,以获得地质化学洞察力.
- 为了确定这些球体是否代表了安第斯类型的岩的父母岩组成.
主要方法:
- 对暗球体和宿主颗粒石的地球化学分析.
- 地质化学数据与宿主宝石石的双模态趋势的对比.
- 地化学建模以评估分离和父性岩潜力.
主要成果:
- 规模较小的暗球体显示出极少的显著分离的证据.
- 地化学建模支持这样一个假设,即这些暗色球体代表了父母的岩组成.
- 格雷纳岩混合区为研究原始岩组成提供了宝贵的自然实验室.
结论:
- 岩混合区是识别安第斯类型岩的父母岩的理想地点.
- 在这些区域内原始的黑色人格,中间球体是此类调查的关键目标.
- 这项研究提供了关键的证据,支持中介岩在大型巴索石的起源中的作用.
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