冰川、水流和扇:加利福尼亚死亡谷萨拉托加山新元古代双晶岩的起源

S. Al-Tofaif
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引用次数: 0

摘要

新元古代冰川沉积物在加利福尼亚死亡谷地区露头。萨拉托加山的露头显示了厚厚的冰川地层序列,显示了床层厚度的显著变化,以及用来证明即使在很短的横向距离内流动的巨大变化的碎屑成分。该序列显示了从冰川近端到冰川远端束的逐渐变化,被解释为新元古代冰川作用的第一个槽口扇。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Glaciers, flows, and fans: origins of a Neoproterozoic diamictite in the Saratoga Hills, Death Valley, California
The Neoproterozoic glacial deposits outcrop throughout Death Valley area in California. The outcrop in Saratoga Hills show a thick succession of the glacial stratigraphy showing significant variation in bed thickness, and clast-compositions that are used to prove the great variation of the flows even within a short lateral distance. This sequence shows a gradual change from glacio-proximal to glacio-distal tracts that are interpreted as the first documented trough mouth fan of the Neoproterozoic glaciation.
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