PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling

Wybrane pełne teksty z tego czasopisma
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
We present various geological models to examine the geothermal energy potential at the Rahat volcanic field, Saudi Arabia. The method involves the application of geophysical techniques of gravity and seismic tomography results to derive a 3D subsurface geological structure representing possible subsurface structural information beneath the northern Rahat volcanic field. Results show a secluded subsurface structure within the basement crust with low densities (< 2500 kg/m3) and a slightly high P-wave velocity, enclosed by a high density (> 2800kg/m3) and low P-wave velocity structure. Identified secluded subsurface structure could depict a magma intrusion within the basement and its depth proximity to the basalt deposition in the region signals the viability of this location for geothermal exploration. Deductions also show that the geothermal reservoir could be reached at starting depths of ~ 1.3 km, whereas its effect could be accessed at depths < 1 km. Within the geothermal active region of northern Harrat Rahat, this study has suggested possible locations with high potential for further geothermal exploration.
Czasopismo
Rocznik
Strony
1713--1729
Opis fizyczny
Bibliogr. 49 poz.
Twórcy
autor
  • Geohazards Research Center, King Abdulaziz University, Jeddah, Saudi Arabia
autor
  • Department of Geology/Geophysics, Alex Ekwueme Federal University, Ndufu-Alike Ikwo, P.M.B. 1010, Abakaliki, Ebonyi State, Nigeria
  • Geohazards Research Center, King Abdulaziz University, Jeddah, Saudi Arabia
  • Department of Petroleum Geology and Sedimentology, Faculty of Earth Sciences, King Abdulaziz University, Jeddah, Saudi Arabia
  • Geohazards Research Center, King Abdulaziz University, Jeddah, Saudi Arabia
  • Department of Petroleum Geology and Sedimentology, Faculty of Earth Sciences, King Abdulaziz University, Jeddah, Saudi Arabia
Bibliografia
  • 1. Abdelwahed MF, El-Masry N, Moufti MR, Kenedi CL, Zhao D, Zah-ran H, Shawali J (2016) Imaging of magma intrusions beneath Harrat Al-Madinah in Saudi Arabia. J Southeast Asian Earth Sci 120:17-28
  • 2. Aboud E, El-Masry N, Qaddah A, Alqahtani F, Moufti MRH (2015) Magnetic and gravity data analysis of Rahat volcanic field, El-Madinah city, Saudi Arabia. NRIAG J Astron Geophys 4:154-162
  • 3. Aboud E, Alqahtani F, Elmasry N, Abdulfarraj M, Osman H (2022) Geothermal anomaly detection using potential field geophysical Data in Rahat volcanic field, Madinah, Saudi Arabia. J Geol Geophys 11:1026
  • 4. Al-Amri AM, Mellors R, Harris D, El-Sayed KA (2016) Geothermal and volcanic evaluation of Harrat Rahat, Northwestern Arabian Peninsula; Profect No.: 11-SPA 2208-02; National Plan for Science, Tech. & Innovation; King Saud University: Riyadh, Saudi Arabia
  • 5. Al-Amri A, Abdelrahman K, Mellors R, Harris D (2020) Geothermal potential of Harrat Rahat, Northern Arabian shield: geological constraits. Arabian Journal of Geosciences, LLNL-JRNL-815125
  • 6. Al-Arifi N, Lashin A, Al-Humidan S (2012) Migration of local earthquakes in the Gulf of Aqaba, Saudi Arabia. Earth Sci Res J 16(1):35-40
  • 7. Alqahtani F, Abraham EM, Aboud E, Rajab M (2022) Two-dimensional gravity inversion of basement relief for geothermal energy potentials at the Harrat Rahat volcanic field, Saudi Arabia, using particle swarm optimization. Energies 15(8):2887. https://doi.org/10.3390/en15082887
  • 8. Al-Shaibani A, Lloyd JW, Abokhodair AA, Al-Ahmari A (2007) Hydrogeological and quantitative groundwater assessment of the basaltic aquifer, northern Harrat Rahat, Saudi Arabia. Arab Gulf J Sci Res 25(1/2):39-49
  • 9. Al-Shaibani AM (2003) Lava fields as potential groundwater sources in western Saudi Arabia. In: Sherif S, Singh VP, Al-Rashed M (ed) Hydrology and water resources: volume 5, proceedings of the international conference on water resources management in arid regions (WaRMAR), Swets and Zeitlinger, Lisse, ISBN 90-5809-548-7, pp 103-120
  • 10. Baer G, Hamiel Y (2010) Form and growth of an embryonic continental rift: InSAR observations and modelling of the 2009 western Arabia rifting episode. Geophys J Int 182:155-167
  • 11. Berthier F, Demange J, Iundt F, Verzier P (1981) Geothermal resources of the Kingdom of Saudi Arabia. In: Saudi Arabian Deputy Ministry for Mineral Resources Open-File Report BRGM-OF-01-24; Ministry of Petroleum and Mineral Resources: Jiddah, Saudi Arabia, 1981; p. 116
  • 12. Bob M, Rahman NA, Taher S, Elamin A (2015) Multi-objective assessment of groundwater quality in Madinah City, Saudi Arabia. Water Qual Exposure Health J 7:53-66
  • 13. Burchardt S (2019) Progressive growth of the cerro bayo cryptodome, Chachahuén volcano, Argentina—implications for viscous magma emplacement. J Geophys Res Solid Earth 124(8):7934-7961. https://doi.org/10.1029/2019JB017543
  • 14. Camp VE, Roobol MJ (1989) The Arabian continental alkali basalt province: part I, evolution of Harrat Rahat, Kingdom of Saudi Arabia. Geol Soc Am Bull 101:71-95
  • 15. Camp VE, Roobol MJ (1992) Upwelling asthenosphere beneath western Arabia and its regional implications. J Geophys Res 97(B11):15255-15271
  • 16. Camp VE, Hooper PR, Roobol MJ, White DL (1987) The Madinah eruption, Saudi Arabia: magma mixing and simultaneous extrusion of three basaltic chemical types. Bull Volcanol 49:489-508
  • 17. Camp VE, Roobol MJ (1991) Geologic map of the Cenozoic lava field of Harrat Rahat, Kingdom of Saudi Arabia. In: Saudi Arabian Directorate General of Mineral Resources, Geoscience Map GM-123, scale 1:250,000
  • 18. Chi G, Xue C (2011) An overview of hydrodynamic studies of mineralization. Geosci Front 2(3):423-438. https://doi.Org/10.1016/j. gsf.2011.05.001
  • 19. Coleman RG, Gregory RT, Brown GF (1983) Cenozoic volcanic rocks of Saudi Arabia, U.S., Geological Survey Open File Report, USGSW-OF-03-93, p 82
  • 20. Comps J, Muffler LJP (1973) Exploration for geothermal resources: In geothermal energy- resources, production, stimulation. Kruger P, Otte C Eds. Stanford University Press, Stanford, pp 95-128
  • 21. Constable SC, Parker RL, Constable CG (1987) Occam’s inversion— a practical algorithm for generating smooth models from electromagnetic sounding data. Geophysics 52:289-300
  • 22. deGroot-Hedlin CS, Constable S (1990) Occam’s inversion to generate smooth, two-dimensional models from magnetotelluric data. Geophysics 55:1613-1624
  • 23. Faizy SM (2021) Assessing a modeling standard in volcanic-Geothermal systems: the effect of the lower system boundary. Department of Earth Sciences, Uppsala University ISSN 16506553 Nr 508
  • 24. Garven G (1995) Continental-scale groundwater flow and geologic processes. Annu Rev Earth Planet Sci 23:89-118
  • 25. George M, Shorbaji H (1987) Explanatory notes to the hydrogeologic and hydrochemical maps of the Al-Madinah quadrangle, Sheet 24D, Kingdom of Saudi Arabia, Directorate General of Mineral Resources, Jiddah, Saudi Arabia, Open-File Report BRGM-OF-23, 23, 65 p.
  • 26. Hashem B (2012) Geothermal development roadmap for the Kingdom of Saudi Arabia, 2012, GHC Bulletin, August
  • 27. Hinze W, Von Frese R, Saad A (2013) Gravity anomaly interpretation. Gravity and magnetic exploration: Principles, practices, and Applications. Cambridge University Press, Cambridge, pp 175-212
  • 28. Hussein MT, Lashin A, Al Bassam A, Al-Arifi N, Al Zahrani I (2013) Geothermal power potential at the western coastal part of Saudi Arabia. Renew Sustain Energy Rev 2013(26):668-684
  • 29. Koulakov I, El-Khrepy S, Al-Arifi N, Sychev I, Kuznetsov P (2014) Evidence of magma activation beneath the Lunayyir basaltic field (Saudi Arabia) from attenuation tomography. Solid Earth Discuss 6:1401-1421
  • 30. Koulakov I, El-Khrepy S, Al-Arifi N, Kuzetsov P, Kasatkina E (2015) Structural cause of a missed eruption in the Harrat Lunayyir basaltic field (Saudi Arabia) in 2009. Geology. https://doi.org/ 10.1130/G36271.1
  • 31. Langenheim VE, Ritzinger BT, Zahran H, Shareef A, Al-dahri M (2019) Crustal structure of the northern Harrat Rahat volcanic field (Saudi Arabia) from gravity and aeromagnetic data. Tectonophysics 750(2019):9-21
  • 32. Lashin A, Al Arifi N (2012) The geothermal potential of Jizan area, Southwestern parts of Saudi Arabia. Int J Phys Sci 2012(4):664-675
  • 33. Lashin A, Al Arifi N (2014) Geothermal energy potential of southwestern of Saudi Arabia “exploration and possible power generation”: A case study at Al Khouba area-Jizan. Renew Sustain Energy Rev 30:771-778
  • 34. Lashin A, Arifi NA, Chandrasekharam D, Al Bassam A, Rehman S, Pipan M (2015) Geothermal energy resources of Saudi Arabia: country update. In: Proceedings world geothermal congress 2015, Melbourne, Australia, 19-25 April
  • 35. Moufti MR, Moghazi AM, Ali KA (2012) Geochemistry and Sr-Nd-Pb isotopic composition of the Harrat Al-Madinah Volcanic Field. Saudi Arabia Gondwana Res 21:670-689
  • 36. Moufti MR, Moghazi AM, Ali KA (2013) 40 Ar/ 39 Ar geochronology of the Neogene-Quaternary Harrat Al-Madinah intercontinental volcanic field, Saudi Arabia: Implications for duration and migration of volcanic activity. J Asian Earth Sci 62:253-268
  • 37. Moufti MR, El-Difrawy MAM, Soliman MAW, El-Moghazi AKM, Matsah MI, (2010) Assessing volcanic hazards of a Quaternary lava field in the Kingdom of Saudi Arabia. King Abdulaziz City for Science and Technology (KACST), Final Report ARP-26-79
  • 38. Nielson DL, Shervais JW, Glen J (2019) Conceptual model for a basalt-related geothermal system: mountain home AFB, Idaho, USA. In: Proceedings, 44th workshop on geothermal reservoir engineering Stanford university, Stanford, California, SGP-TR-214
  • 39. Ocampo-Diaz JDD, Rojas BM, Leon VJ (2005) Decision analysis applied to Las Tres Virgenes Geothermal Field Mexico. Proceedings World Geothermal Congress, Antalya Turkey
  • 40. Pallister JS, McCauland WA, Jonsson S, Zhong L, Zahran HM, Had-didy SE, Aburukbah A, Stewart ICF, Lundgren PR, White RA, Moufti MRH (2010) Broad accommodation of rift-related extension recorded by dyke intrusion in Saudi Arabia. Nat Geosci 3:705-712. https://doi.org/10.1038/NGE0966
  • 41. Pearson-Grant SC, Bertrand EA (2021) Topography as a major influence on geothermal circulation in the Taupo Volcanic Zone, New Zealand. Geophys Res Lett 48:e2020GL092248. https://doi.org/ 10.1029/2020GL092248
  • 42. Pirttijärvi M (2014) GRABLOX2: Gravity interpretation and modelling using 3-D block models; User's guide to version 2.1. University of Oulu, Finland
  • 43. Press WH, Flannery BP, Teukolsky SA, Vetterling WT (1988) Numerical recipes, the art of scientific computing. Cambridge University Press, Cambridge
  • 44. Roobol MJ, Pint JJ, Al-Shanti MA, Al-Juaid AJ, Al-Amoudi SA, Pint S, Al-Eisa AM, Allam F, Al-Sulaimani GS, Banakhar AS (2002) Preliminary survey for lava-tube caves on Harrat Kishb, kingdom of Saudi Arabia, p 46
  • 45. Roobol MJ, Bankher K, Bamufleh S (2007) Geothermal anomalies along the MMN volcanic line including the cities of Al Madinah Al Munnawwarah and Makkah Al Mukkarramah. Jeddah: Saudi Geological Survey
  • 46. Rowland JV, Sibson RH (2004) Structural controls on hydrothermal flow in a segmented rift system, Taupo Volcanic Zone, New Zealand. Geofluids 4:259-283
  • 47. Titi YLA, Minarto E (2017) The Subsurface Three-Dimensional Modeling of Volcano Arc of Flores Island Based on Gravity Data Analysis. In: International conference on engineering, science and nanotechnology 2016 (ICESNANO 2016) AIP Conf. Proc. 1788, 030106-1-030106-6. https://doi.org/10.1063/1.4968359
  • 48. Worldometer (2022) Saudi Arabia Electricity. https://www.worldomete rs.info/electricity/Saudi-arabia-electricity/
  • 49. Yan-lin S, Ai-lingc Z, You-bin H, Ke-yan X (2011) 3D geological modeling and its application under complex geological conditions. Procedia Engineering 12:41-46
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-db167b47-22fc-430f-8702-1a2e7bf7f29c
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.