Khuff序列KS4:阿曼苏丹国阿曼山脉中Khuff颗粒岩包的高分辨率解剖。阿拉伯板块的二叠纪-三叠纪序列,EAGE第三届阿拉伯板块地质研讨会摘要,科威特。摘要

M. Haase
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引用次数: 0

摘要

此次露头研究是阿曼山区Saiq组(类似于Khuff组的露头)大型项目的一部分,重点研究了Khuff层序4下部(KS4)的小尺度非均质性。该层段以块状颗粒岩为主,乍一看似乎极为均匀,尽管白云化强烈,但可探测到明显的槽状交错层理。锯齿状的伽马射线模式使得小规模的周期解释变得困难。因此,有必要进行非常详细的相层序分析,以破译颗粒岩的垂向微相组成,并将其与潜在的孔隙类型联系起来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Khuff Sequence KS4: High-resolution anatomy of a Middle Khuff grainstone package, Oman Mountains, Sultanate of Oman. In The Permo–Triassic Sequence of the Arabian Plate, Abstracts of the EAGE’s Third Arabian Plate Geology Workshop, Kuwait. Abstract,
This outcrop study is part of a larger-scale project on the Saiq Formation in the Oman Mountains (outcrop analog of Khuff Formation), and focussed on the small-scale heterogeneities of the lower part of Khuff Sequence 4 (KS4). This interval is dominated by massive grainstones that at first glance seem extremely homogenous with distinct trough cross-bedding detectable in spite of strong dolomitization. Serrated gamma-ray patterns made small-scale cycle interpretations difficult. Therefore a very detailed facies and sequence analysis was necessary to decipher the vertical microfacies make-up of the grainstones and link it with potential pore types.
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