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首页> 外文期刊>Carbonates and Evaporites >A biodetrital coral mound complex: Key to early diagenetic processes in the Mississippian Bangor Limestone
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A biodetrital coral mound complex: Key to early diagenetic processes in the Mississippian Bangor Limestone

机译:生物碎屑珊瑚丘复合体:密西西比州班戈石灰岩早期成岩作用的关键

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摘要

The Bangor Limestone is a Mississippian (Chesterian) shallow marine carbonate formation exposed over a large portion of the Interior Low Plateaus province of northern Alabama. It is dominated by oolitic grainstone and skeletal wackestone and packstone, but in one outcrop near Moulton, Alabama, the Bangor contains a five m thick, 25 m wide, oolite-biodetrital mound-tidal flat succession. This sequence is interpreted as a 4th order sea level cycle.
机译:班戈(Bangor)石灰石是密西西比(Chesterian)浅海碳酸盐岩地层,暴露于阿拉巴马州北部内陆高原省的大部分地区。它主要由橄榄质的花岗石,骨架的瓦克石和堆积岩组成,但在阿拉巴马州的莫尔顿附近的一个露头中,班戈包含一个5 m厚,25 m宽的橄榄石-生物碎屑丘-潮滩平面演替。该序列被解释为四级海平面周期。

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