在弧形岩中微量元素演变的相位平衡建模:对石化和铜矿指标的含义
Caroline R Soderman1, Owen M Weller1
1Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ UK.
概括
在弧形岩石中的动态矿物溶解分离挑战了传统的微量元素解释. 新的模型显示,高的Sr/Y比率,通常与石系统相关,可以在各种条件下形成,而不仅仅是深水的水.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 马格玛创世记是一本书.
背景情况:
- 弧形 magma 中的微量元素比率是理解形与荒系统的关键.
- 整个岩石特征与石质条件 (压力,水,氧化还原) 之间的定量联系是具有挑战性的,因为在分量结晶过程中矿物质组合的演变.
研究的目的:
- 开发和验证一种热力学建模框架,用于跟踪弧形 magma 中的微量元素演变.
- 为了研究动态矿物溶解分区在不同地条件下对微量元素特征的影响.
主要方法:
- 集成更新的热力学模型与动态矿物溶解分区.
- 基准模型与已发表的实验数据相比,包括阿帕酸和度.
- 模拟了原始弧形岩在不同压力,水含量和氧化还原条件下的分量结晶.
主要成果:
- 该模型成功地复制了相组合和组合.
- 动态分区显示,两体和石榴石可以在深水的条件下产生重叠的微量元素向量.
- 高的Sr/Y比率,一个常见的矿指标,可以来自各种石化遗传途径,不仅仅是深度,氧化或水性环境.
结论:
- 动态矿物溶解分离显著影响弧形岩石中的微量元素演变.
- 对于矿勘探的微量元素比率的传统解释可能需要重新评估.
- 该建模框架为评估弧形岩石化和微量元素行为提供了一个强大的工具.
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