约旦安曼北部Al-Baqa地区上白垩统有孔虫生物地层与古测深

I.A. Al-Rifaiy, O.H. Cherif, B.A. El-Bakri
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引用次数: 12

摘要

通过对约旦安曼北部Al-Baqa地区上白垩纪暴露地层中有孔虫组合的垂直变化的研究,我们可以根据海平面的升降变化来评价古代的古深度变化。指数有孔虫物种用于年龄测定和古深度测量。沉积旋回包括上Cenomanian沉积(Fuheis, Hummar, Shueib和Wadi Sir组)似乎与全球海平面的上升变化有关。研究区晚坎帕世沉积旋回(安曼组)也是如此。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Upper cretaceous foraminiferal biostraigraphy and paleobathymetry of the Al-Baqa area, North of Amman (Jordan)

The examination of vertical variations of foraminiferal assemblages in the Upper Cretaceous exposures of the Al-Baqa area to the north of Amman in Jordan enables us to evaluate ancient paleobathymetric changes with regard to eustatic changes in sea level. Index foraminiferal species are used for age determinations and paleobathymetry.

The sedimentary cycle including Upper Cenomanian sediments (Fuheis, Hummar, Shueib and Wadi Sir Formations) appears to be related to global eustatic changes in sea levels. This is also the case of the Late Campanian sedimentary cycle in the study area (Amman Formation).

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