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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
|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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