概括
-测定的摩利布丁揭示了两种不同的间隔的基础金属合金矿化在拉拉米德orogeny. 这些广泛,同步的事件表明区域地和地的相互作用,而不是局部的过程.
科学领域:
- 经济地质学 地质学
- 地质时间学 (Geochronology)
- 构造学 构造学 构造学 构造学
背景情况:
- 北美西南部 (90-50万年前) 的拉拉米德石矿产与40多个基本金属矿矿床有关.
- молибденит是一种富含的硫化物,是这些矿石矿床中常见的矿物.
研究的目的:
- 准确地追溯与拉拉米德矿铜沉积物相关的矿化事件.
- 研究矿物化的时间和空间分布.
- 了解推动矿石形成的基础地质过程.
主要方法:
- - (Re-Os) 同位素的地球时代学被应用到来自各种沉积物的卜丁酸盐样本上.
- 地质绘图和地下层年龄分析被用于将矿化时间置于背景.
主要成果:
- 个体矿床的矿化始终发生在岩活动的晚期,无论岩持续时间或强度如何.
- -测年确定了两个主要的矿化间隔:74-70万年前和60-55万年前.
- 较老的沉积物主要位于亚利桑那州西北部的前剑桥时代地下室;较年轻的沉积物位于亚利桑那州南部和墨西哥北部的前剑桥时代地下室.
结论:
- 在不同的地质环境中同步,广泛的矿物化表明区域范围的地地相互作用.
- 这些发现挑战了这些矿石矿床是由局部的岩过程形成的概念.
- 这两种不同的年龄集群表明,拉拉米德金质生成过程中发生了脉冲性金属生成事件.
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