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• W4387133041 abstract "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 δ 13 C and δ 18 O 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 δ 13 C 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." @default.
• W4387133041 created "2023-09-29" @default.
• W4387133041 creator A5039875706 @default.
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• W4387133041 creator A5092960348 @default.
• W4387133041 creator A5092960349 @default.
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• W4387133041 date "2023-09-28" @default.
• W4387133041 modified "2023-09-29" @default.
• W4387133041 title "Gamma-ray, stable carbon and oxygen isotope chemostratigraphy and sequence stratigraphy of the Lower Mahil Formation (KS-1 Khuff-Equivalent), Northern Oman" @default.
• W4387133041 cites W121857346 @default.
• W4387133041 cites W1233342656 @default.
• W4387133041 cites W1530011460 @default.
• W4387133041 cites W1583491481 @default.
• W4387133041 cites W1584354900 @default.
• W4387133041 cites W1682777677 @default.
• W4387133041 cites W1965846255 @default.
• W4387133041 cites W1982376419 @default.
• W4387133041 cites W1986916739 @default.
• W4387133041 cites W1991055563 @default.
• W4387133041 cites W1994218077 @default.
• W4387133041 cites W1997252211 @default.
• W4387133041 cites W1999285007 @default.
• W4387133041 cites W2008155461 @default.
• W4387133041 cites W2015252853 @default.
• W4387133041 cites W2021780626 @default.
• W4387133041 cites W2022895897 @default.
• W4387133041 cites W2034273125 @default.
• W4387133041 cites W2035486592 @default.
• W4387133041 cites W203584942 @default.
• W4387133041 cites W2038022413 @default.
• W4387133041 cites W2048601982 @default.
• W4387133041 cites W2049124719 @default.
• W4387133041 cites W2050440902 @default.
• W4387133041 cites W2065589860 @default.
• W4387133041 cites W2066663906 @default.
• W4387133041 cites W2077274745 @default.
• W4387133041 cites W2081243991 @default.
• W4387133041 cites W2081732342 @default.
• W4387133041 cites W2084355798 @default.
• W4387133041 cites W2091673323 @default.
• W4387133041 cites W2095977532 @default.
• W4387133041 cites W2102372154 @default.
• W4387133041 cites W2104659005 @default.
• W4387133041 cites W2106722441 @default.
• W4387133041 cites W2108911062 @default.
• W4387133041 cites W2116221979 @default.
• W4387133041 cites W211761628 @default.
• W4387133041 cites W2127221748 @default.
• W4387133041 cites W2128679491 @default.
• W4387133041 cites W2134839040 @default.
• W4387133041 cites W2137642639 @default.
• W4387133041 cites W2139711367 @default.
• W4387133041 cites W2143514857 @default.
• W4387133041 cites W2146761970 @default.
• W4387133041 cites W2148013722 @default.
• W4387133041 cites W2152946280 @default.
• W4387133041 cites W2153211086 @default.
• W4387133041 cites W2153304268 @default.
• W4387133041 cites W2153848828 @default.
• W4387133041 cites W2156954622 @default.
• W4387133041 cites W2160907875 @default.
• W4387133041 cites W2164737401 @default.
• W4387133041 cites W2169166182 @default.
• W4387133041 cites W2169964049 @default.
• W4387133041 cites W2178258189 @default.
• W4387133041 cites W2253137977 @default.
• W4387133041 cites W2279977096 @default.
• W4387133041 cites W2287111010 @default.
• W4387133041 cites W2300583568 @default.
• W4387133041 cites W2332345260 @default.
• W4387133041 cites W2333772853 @default.
• W4387133041 cites W2335642403 @default.
• W4387133041 cites W2395183450 @default.
• W4387133041 cites W2516667427 @default.
• W4387133041 cites W2545266442 @default.
• W4387133041 cites W2574973601 @default.
• W4387133041 cites W2729384632 @default.
• W4387133041 cites W2795204788 @default.
• W4387133041 cites W2896581192 @default.
• W4387133041 cites W2910362007 @default.
• W4387133041 cites W2915361100 @default.
• W4387133041 cites W2935685348 @default.
• W4387133041 cites W2939888277 @default.
• W4387133041 cites W2944320642 @default.
• W4387133041 cites W2947835304 @default.
• W4387133041 cites W2981138633 @default.
• W4387133041 cites W2984888820 @default.
• W4387133041 cites W3000314751 @default.
• W4387133041 cites W3005267156 @default.
• W4387133041 cites W3007039886 @default.
• W4387133041 cites W3043985757 @default.
• W4387133041 cites W3094631112 @default.
• W4387133041 cites W3111073335 @default.
• W4387133041 cites W3209459582 @default.
• W4387133041 cites W4211105773 @default.

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