TY - JOUR
T1 - Microfacies and depositional model of the Lower Mahil Formation (outcrop Khuff-equivalent (KS-1)) in Jabal Akhdar, Northern Oman
T2 - Implications for reservoir characterization
AU - Al Raqaishi, Rasha Ali
AU - Moustafa, Mohamed S.h.
AU - El-Ghali, Mohamed A.K.
AU - Abbasi, Iftikhar Ahmed
AU - Al-Awah, Hezam
AU - Al Sarmi, Musaab Shakir
AU - Al-Sayigh, Abdulrazak
AU - Al-Shukaili, Marwa
N1 - Funding Information:
This work is part of the MSc thesis project.The authors thank The Research Council ( TRC ) for funding this project ( RC/RG-DVC/ESRC/18/01 ).The authors thank Michael C.Pope for his excellent recommendation and editing of the manuscript.Many regards went to the technicians and staff of the Department of Earth Science at SQU, particularly Mr.Said Al-Abri, Mr.Bader Al Waili, Mr.Hilal Al Zeidi, and Mr.Hamdan Al-Zidi, for their help in thin-section preparation.Special thanks to the Bachelor's students Najiya, Nada, Nawf, Aaraf, Basema, and Nasser for their assistance in the field trips.We would like to thank the two anonymous reviewers for their valuable comments that improved the quality of the paper.
Publisher Copyright:
© 2022 Elsevier Ltd
PY - 2023/3
Y1 - 2023/3
N2 - This study presents a detailed microfacies analysis of the Lower Triassic Mahil Formation (Khuff outcrop equivalent (KS-1)) in Jabal Akhdar, at the Saiq Plateau and Wadi Sahtan areas of Northern Oman.Two sections were measured and sedimentologically logged along a depositional dip profile emphasizing color, lithology, grain components, bed thickness, the nature of bed contact, lateral continuity of beds, and fossil content.One hundred and eighty fresh rock samples were collected from various lithofacies.The collected samples were thin-sectioned after blue epoxy was impregnated, and then they were half stained with Alizarin Red S and Potassium Ferricyanide for mineralogical identification.The point-counted compositions were determined by counting 300 points for each thin section to reconstruct the original components, obtain precise quantification, develop representative microfacies, and construct the depositional model for the Lower Mahil Formation.Accordingly, eighteen microfacies types representing different carbonate ramp environments were identified; two are only recognized in the Wadi Sahtan logged section, ten are restricted to the Saiq Plateau logged section, and six are common for both sections.The Lower Mahil Formation consists of backshoal (inner ramp) to foreshoal (mid-ramp) carbonate facies, with shoal (ramp crest) facies restricted to the Saiq Plateau logged section.The backshoal facies was characterized by abundant non-skeletal grains with breccia.The shoals were predominantly oolitic and intraclastic packstone-grainstone.Foreshoal carbonate facies, on the other hand, has mixed skeletal and non-skeletal grains with weakly developed hummocky cross-stratified beds.The shallow-water foraminiferal and oolitic packstone/grainstone facies are the potential reservoir intervals, whereas the wackestone facies is the non-reservoir intervals within the Lower Mahil Formation.The detailed sedimentological and microfacies analysis helped characterize the Lower Mahil Formation for better recognizing the potential reservoir vs.no-reservoir.This study can be a key reference to correlate the Lower Mahil Formation locally and regionally.
AB - This study presents a detailed microfacies analysis of the Lower Triassic Mahil Formation (Khuff outcrop equivalent (KS-1)) in Jabal Akhdar, at the Saiq Plateau and Wadi Sahtan areas of Northern Oman.Two sections were measured and sedimentologically logged along a depositional dip profile emphasizing color, lithology, grain components, bed thickness, the nature of bed contact, lateral continuity of beds, and fossil content.One hundred and eighty fresh rock samples were collected from various lithofacies.The collected samples were thin-sectioned after blue epoxy was impregnated, and then they were half stained with Alizarin Red S and Potassium Ferricyanide for mineralogical identification.The point-counted compositions were determined by counting 300 points for each thin section to reconstruct the original components, obtain precise quantification, develop representative microfacies, and construct the depositional model for the Lower Mahil Formation.Accordingly, eighteen microfacies types representing different carbonate ramp environments were identified; two are only recognized in the Wadi Sahtan logged section, ten are restricted to the Saiq Plateau logged section, and six are common for both sections.The Lower Mahil Formation consists of backshoal (inner ramp) to foreshoal (mid-ramp) carbonate facies, with shoal (ramp crest) facies restricted to the Saiq Plateau logged section.The backshoal facies was characterized by abundant non-skeletal grains with breccia.The shoals were predominantly oolitic and intraclastic packstone-grainstone.Foreshoal carbonate facies, on the other hand, has mixed skeletal and non-skeletal grains with weakly developed hummocky cross-stratified beds.The shallow-water foraminiferal and oolitic packstone/grainstone facies are the potential reservoir intervals, whereas the wackestone facies is the non-reservoir intervals within the Lower Mahil Formation.The detailed sedimentological and microfacies analysis helped characterize the Lower Mahil Formation for better recognizing the potential reservoir vs.no-reservoir.This study can be a key reference to correlate the Lower Mahil Formation locally and regionally.
KW - Breccia
KW - Carbonate ramp
KW - Khuff KS-1
KW - Lower Mahil Formation
KW - Oolitic grainstone
KW - Oolitic shoal lithofacies
KW - Saiq Plateau
KW - Wadi Sahtan
UR - http://www.scopus.com/inward/record.url?scp=85144568041&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85144568041&partnerID=8YFLogxK
U2 - 10.1016/j.marpetgeo.2022.106066
DO - 10.1016/j.marpetgeo.2022.106066
M3 - Article
AN - SCOPUS:85144568041
SN - 0264-8172
VL - 149
JO - Marine and Petroleum Geology
JF - Marine and Petroleum Geology
M1 - 106066
ER -