坎布里亚碳酸盐中的奥特基亚地:阿勒根亚盐迁移的证据
概括
坎布里亚石灰岩中的Authigenic地在低温下从盐水中形成. 这一过程与阿勒根人折叠有关,可能发生在整个阿巴拉契亚流域.
科学领域:
- 地质化学 地质化学
- 沉积岩石学 沉积岩石学
- 同位素地质年代学 同位素地质年代学
背景情况:
- 在阿巴拉契亚山脉的坎布里亚和奥尔多维纪碳酸盐岩石中,奥特基因地丰富.
- 了解它的形成是解读盆地流体历史的关键.
研究的目的:
- 为了调查在科诺科切格石灰岩中异性田形成的起源和时间.
- 评估盐和构造事件在地起源中的作用.
主要方法:
- 对矿子晶体的液体含有物的分析.
- 确定全岩石中与的比例.
- 热化学数据分析.
- 阿尔贡-阿尔贡时代光谱测定地的年龄.
主要成果:
- 有证据表明,地的低温形成来自连结盐和类材料之间的反应.
- 酸盐子晶体和低的Cl/Br比率表明液的起源.
- 阿贡年代测定将田形成定位在宾夕法尼亚晚期到珀米亚早期.
- 形成可能与在阿勒根亚折叠期间的盐水迁移有关.
结论:
- 在Conococheague石灰岩中存在的Authigenic地是在低温下通过盐水-类相互作用形成的.
- 艾利根人折叠很可能动员了这些盐水.
- 这一过程可能在坎布里亚-奥尔多维奇亚亚巴拉契亚碳酸盐岩中广泛存在.
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