Permian–Triassic Transition and the Saiq/Mahil Boundary in the Oman Mountains: Proposed correction for lithostratigraphic nomenclature

Geoarabia Pub Date : 2013-07-01 DOI:10.2113/geoarabia180387
A. Baud, S. Richoz
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引用次数: 17

Abstract

This note discusses the lithostratigraphic nomenclature used to characterise the Permian–Triassic transition at outcrop in the Oman Mountains, with emphasis on the position of the boundary between the Saiq and Mahil formations. Two inconsistent criteria for picking the Saiq/Mahil Boundary (SMB) prevail in the literature causing confusion regarding the correct position of the Permian/Triassic Boundary (PTB). The position of the PTB plays a central role in the correlation of these two formations from outcrop to the subsurface Khuff and overlying Sudair formations. The Khuff Formation contains one of the world’s greatest reserves of non-associated gas, and its outcrop equivalent in the Oman Mountains is increasingly being studied for the purposes of regional correlations, reservoir characterisation and exploration. Therefore an agreement on the position of the SMB is a pre-requisite for precise communication among geoscientists. In this note we review the historical source of the confusion and recommend applying stratigraphic rules to resolve the position of the Saiq/Mahil Boundary (SMB).
阿曼山区二叠纪-三叠纪过渡与Saiq/Mahil界线:岩石地层命名法的修正建议
本文讨论了用于表征阿曼山脉露头二叠纪-三叠纪过渡的岩石地层命名法,重点讨论了Saiq组和Mahil组之间的边界位置。文献中普遍存在两种不一致的选择Saiq/Mahil边界(SMB)的标准,这导致了对二叠纪/三叠纪边界(PTB)正确位置的混淆。PTB的位置对这两组从露头到地下的Khuff和上覆的Sudair组的对比起着核心作用。Khuff组含有世界上最大的非伴生气储量之一,其在阿曼山脉的露头当量正越来越多地用于区域对比、储层特征和勘探。因此,就SMB的位置达成一致是地球科学家之间精确沟通的先决条件。在本文中,我们回顾了混淆的历史根源,并建议应用地层学规则来解决赛克/马希尔边界(SMB)的位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geoarabia
Geoarabia 地学-地球科学综合
自引率
0.00%
发文量
0
审稿时长
>12 weeks
期刊介绍: Cessation. Published from 1996 to 2015, GeoArabia, The Journal of the Middle Eastern Geosciences was a quarterly journal covering the petroleum geosciences in the Middle East. The journal covers subjects such as: - sedimentology - tectonics - geophysics - petroleum reservoir characterization
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