Gamma-ray, stable carbon and oxygen isotope chemostratigraphy and sequence stratigraphy of the Lower Mahil Formation (KS-1 Khuff-Equivalent), Northern Oman

被引:0
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作者
Moustafa, Mohamed S. H. [1 ]
Al Raqaishi, Rasha [1 ]
El-Ghali, Mohamed A. K. [1 ,2 ]
Gharbi, Mohamed [3 ]
Abbasi, Iftikhar Ahmed [1 ]
Al Humaidi, Aaraf [4 ]
Al Ghafri, Nada [1 ]
Alshukaili, Marwa Musallam [1 ]
Al-Awah, Hezam [5 ]
机构
[1] Sultan Qaboos Univ, Dept Earth Sci, Muscat, Oman
[2] Sultan Qaboos Univ, Earth Sci Res Ctr, Muscat, Oman
[3] Water Res & Technol Ctr, Georesources Lab, Borj Cedria, Soliman, Tunisia
[4] Petrogas Oil Co, Muscat, Oman
[5] Qatar Univ, Coll Arts & Sci, Dept Chem & Earth Sci, Geol Program, Doha, Qatar
关键词
carbon isotope; oxygen isotope; uranium; total gamma-ray; Mahil Formation; Khuff Formation; SHALLOW-MARINE CARBONATE; AL AZIZIYAH FORMATION; PERSIAN-GULF; NATURAL RADIOACTIVITY; ARABIAN GULF; EVOLUTION; RECORD; MOUNTAINS; SEDIMENTS; FACIES;
D O I
10.3389/feart.2023.1270795
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This research presents findings from a study focused on the Lower Triassic (Induan) Lower Mahil KS-1 Formation, situated on a homoclinal carbonate platform in Northern Oman. The sequence stratigraphy of this formation is characterized by a considerable thickness variation, slumps, and breccia deposits related to active normal faults coupled with intra-basin growth faults. The main objective was to establish a reliable stratigraphic framework for the Lower Mahil KS-1 Formation by integrating high-resolution carbon isotope data along with high-resolution spectral and total gamma-ray data. To achieve this, whole-rock samples were analyzed for delta 13C and delta 18O isotopes. Spectral and total gamma-ray records were obtained for the formation. Isotope sampling is conducted every 0.5 m in the Saiq Plateau and Wadi Sahtan sections. Furthermore, spectral gamma-ray measurements were taken at intervals of 10 cm from the logged sections. Within the third-order sequence, the spectral gamma-ray data revealed a distinct sea-level trend, leading to the division of KS1 into two different parts. Five fourth-order depositional sequences were identified by analyzing stable carbon isotopes, uranium, and total gamma-ray profiles. Four of these sequences displayed complete patterns, reflecting transgression and regression phases, while the fifth sequence was incomplete and solely comprised a transgressive phase. An essential outcome of the study is the correlation of the delta 13C curve of the Lower Mahil KS-1 Formation with other similar formations around the Tethys region. This correlation indicates that the Lower Mahil KS-1 Formation captures the near-primary signal of carbon isotope variations in coeval seawater. As a result, it holds promise as a reference section for future investigations and studies in this field. Compared to the prior investigation, this study utilizes data with higher precision, capturing spectral gamma-ray measurements at 10 cm intervals and isotope measurements at 50 cm intervals. Furthermore, the study's focus is confined explicitly to KS1.
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页数:26
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