Baleid Ali Hatem , Mohammed Hail Hakimi , Khairul Azlan Mustapha , Wan Hasiah Abdullah , Alok Kumar
{"title":"也门东南部Shabwah凹陷页岩油潜力:地球化学和盆地模拟视角","authors":"Baleid Ali Hatem , Mohammed Hail Hakimi , Khairul Azlan Mustapha , Wan Hasiah Abdullah , Alok Kumar","doi":"10.1016/j.jafrearsci.2025.105848","DOIUrl":null,"url":null,"abstract":"<div><div>The Lam and Meem organic-rich shale facies of the Upper Jurassic Madbi Formation in the Shabwah Depression are subjected to multi-scale geochemical, petrographical and mineralogical investigation, alongside bulk kinetics and basin modeling analyses for understanding the unconventional oil shale reservoir potential. The studied shales exhibit significant organic matter, with total organic carbon (TOC) between 1 wt % and 12.3 wt %. The Lam and Meem shale facies are also charactersied by hydrogen rich kerogen types II and II/III. The dominance of such hydrogen-rich kerogen was confirmed from the Py-GC and FTIR structures of the kerogen fraction, exhibiting the possibility of producing commercial amounts of paraffinic–naphthenic–aromatic oils with low wax content. The studied shale facies is currently thermally mature, with the Meem shale facies entered the peak-stage of the oil window, based on measured vitrinite reflectance (VRo) values and high oil saturation index (OSI) values. This claim agrees with the bulk kinetic results, which suggest that the commercial amounts of oil can generate by kerogen conversion of up to 50 % during the peak stage of oil window at geological temperature values between 132 °C and 155 °C, consistent with computed vitrinite reflectance values of 0.77–1.07 %Ro. 1-D basin modeling suggests the Meem shale source rock system is more than the Lam shale source rock, entering the main oil generation during the lower Cretaceous to Late Oligocene time, resulting in commercial quantities of oil, having transformation ratio (TR) i.e. up to 55 %. This high maximum oil generation, alongside high brittleness index leads to create non-fabric fracture pores within the Meem shale facies, which may have increased by elevated pressure during the deep burial depths. Therefore, the Meem shale facies is considered for unconventional shale oil reservoir with recommendation of hydraulic fracturing techniques for unconventional production.</div></div>","PeriodicalId":14874,"journal":{"name":"Journal of African Earth Sciences","volume":"233 ","pages":"Article 105848"},"PeriodicalIF":2.2000,"publicationDate":"2025-09-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Shale–oil potential in Shabwah depression, southeast Yemen: A geochemical and basin modeling perspective\",\"authors\":\"Baleid Ali Hatem , Mohammed Hail Hakimi , Khairul Azlan Mustapha , Wan Hasiah Abdullah , Alok Kumar\",\"doi\":\"10.1016/j.jafrearsci.2025.105848\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Lam and Meem organic-rich shale facies of the Upper Jurassic Madbi Formation in the Shabwah Depression are subjected to multi-scale geochemical, petrographical and mineralogical investigation, alongside bulk kinetics and basin modeling analyses for understanding the unconventional oil shale reservoir potential. The studied shales exhibit significant organic matter, with total organic carbon (TOC) between 1 wt % and 12.3 wt %. The Lam and Meem shale facies are also charactersied by hydrogen rich kerogen types II and II/III. The dominance of such hydrogen-rich kerogen was confirmed from the Py-GC and FTIR structures of the kerogen fraction, exhibiting the possibility of producing commercial amounts of paraffinic–naphthenic–aromatic oils with low wax content. The studied shale facies is currently thermally mature, with the Meem shale facies entered the peak-stage of the oil window, based on measured vitrinite reflectance (VRo) values and high oil saturation index (OSI) values. This claim agrees with the bulk kinetic results, which suggest that the commercial amounts of oil can generate by kerogen conversion of up to 50 % during the peak stage of oil window at geological temperature values between 132 °C and 155 °C, consistent with computed vitrinite reflectance values of 0.77–1.07 %Ro. 1-D basin modeling suggests the Meem shale source rock system is more than the Lam shale source rock, entering the main oil generation during the lower Cretaceous to Late Oligocene time, resulting in commercial quantities of oil, having transformation ratio (TR) i.e. up to 55 %. This high maximum oil generation, alongside high brittleness index leads to create non-fabric fracture pores within the Meem shale facies, which may have increased by elevated pressure during the deep burial depths. Therefore, the Meem shale facies is considered for unconventional shale oil reservoir with recommendation of hydraulic fracturing techniques for unconventional production.</div></div>\",\"PeriodicalId\":14874,\"journal\":{\"name\":\"Journal of African Earth Sciences\",\"volume\":\"233 \",\"pages\":\"Article 105848\"},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2025-09-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of African Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1464343X25003152\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of African Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1464343X25003152","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Shale–oil potential in Shabwah depression, southeast Yemen: A geochemical and basin modeling perspective
The Lam and Meem organic-rich shale facies of the Upper Jurassic Madbi Formation in the Shabwah Depression are subjected to multi-scale geochemical, petrographical and mineralogical investigation, alongside bulk kinetics and basin modeling analyses for understanding the unconventional oil shale reservoir potential. The studied shales exhibit significant organic matter, with total organic carbon (TOC) between 1 wt % and 12.3 wt %. The Lam and Meem shale facies are also charactersied by hydrogen rich kerogen types II and II/III. The dominance of such hydrogen-rich kerogen was confirmed from the Py-GC and FTIR structures of the kerogen fraction, exhibiting the possibility of producing commercial amounts of paraffinic–naphthenic–aromatic oils with low wax content. The studied shale facies is currently thermally mature, with the Meem shale facies entered the peak-stage of the oil window, based on measured vitrinite reflectance (VRo) values and high oil saturation index (OSI) values. This claim agrees with the bulk kinetic results, which suggest that the commercial amounts of oil can generate by kerogen conversion of up to 50 % during the peak stage of oil window at geological temperature values between 132 °C and 155 °C, consistent with computed vitrinite reflectance values of 0.77–1.07 %Ro. 1-D basin modeling suggests the Meem shale source rock system is more than the Lam shale source rock, entering the main oil generation during the lower Cretaceous to Late Oligocene time, resulting in commercial quantities of oil, having transformation ratio (TR) i.e. up to 55 %. This high maximum oil generation, alongside high brittleness index leads to create non-fabric fracture pores within the Meem shale facies, which may have increased by elevated pressure during the deep burial depths. Therefore, the Meem shale facies is considered for unconventional shale oil reservoir with recommendation of hydraulic fracturing techniques for unconventional production.
期刊介绍:
The Journal of African Earth Sciences sees itself as the prime geological journal for all aspects of the Earth Sciences about the African plate. Papers dealing with peripheral areas are welcome if they demonstrate a tight link with Africa.
The Journal publishes high quality, peer-reviewed scientific papers. It is devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be considered. Papers must have international appeal and should present work of more regional than local significance and dealing with well identified and justified scientific questions. Specialised technical papers, analytical or exploration reports must be avoided. Papers on applied geology should preferably be linked to such core disciplines and must be addressed to a more general geoscientific audience.