Morphoneotectonics and prospects of oil and gas presence in deserts of Iraq
- Authors: Al-Gurairy A.Y.1, Naravas A.K1, Usova V.M2
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Affiliations:
- Russian State Geological Prospecting University (Moscow Geological Prospecting Institute)
- Peoples’ Friendship University of Russia (RUDN University)
- Issue: Vol 19, No 3 (2018)
- Pages: 378-390
- Section: Innovative use of mineral resources
- URL: https://journals.rudn.ru/engineering-researches/article/view/19258
- DOI: https://doi.org/10.22363/2312-8143-2018-19-3-378-390
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Abstract
The article deals with the prospects of Iraq’s oil and gas potential. It should be noted that there has not been much attention payed to the desert regions of Iraq located on the Arabian plate. However, recent studies show prospectivity of the Iraq deserts. As a result of the recent investigation of river valleys in the region, the following main morphotectonic processes were identified: rejuvenation of the river network and emergence of new river basins; division of individual rivers into two or more parts; interception of the river network. As a result of long-term field and cameral geological and geomorphological studies in the area of the Western and Southern deserts, it was possible to reconstruct the existing tectonic activity of the area from the Miocene period to the present day. It is established that the regional Euphrates fault on the territory of Iraq occupies an exceptionally important place, which was previously underestimated. Adjacent echelon faults of the following order formed a system of pre-existent tectonic blocks with different kinematics and morphology. The causes and mechanism of neotectonic Neogene-Quaternary movements of the earth’s surface are established. Thus, separate tectonic blocks are identified, which generally form zonal regions of uplifts or valleys. The areas of elevated blocks (for example, the raising of Al-Najaf Al-Ashraf of the third order) are created by plicative dome structures in the cover near the Euphrates fault, favorable for the accumulation of HC.
About the authors
Ahmad Yasien Al-Gurairy
Russian State Geological Prospecting University (Moscow Geological Prospecting Institute)
Author for correspondence.
Email: ahmad.yasien@mail.ru
Postgraduate student of the Department of General Geology and Geological Mapping, Russian State Geological Prospecting University (Moscow Geological Prospecting Institute). Research interests: search and exploration of hydrocarbon fields, study of the geological structure of the Arab plate and Mesopotamia
23, Miklukho-Maklaya str , Moscow, 117997, Russian FederationAnton K Naravas
Russian State Geological Prospecting University (Moscow Geological Prospecting Institute)
Email: gazon91@list.ru
Associate professor of the Department of General Geology and Geological Mapping, Russian State Geological Prospecting University (Moscow Geological Prospecting Institute). Research interests: search and exploration of hydrocarbon fields, study of the geological structure of the Arab plate and Mesopotamia
23, Miklukho-Maklaya str , Moscow, 117997, Russian FederationValentina M Usova
Peoples’ Friendship University of Russia (RUDN University)
Email: usova_vm@pfur.ru
Senior lecturer Department of Geology, Mining and Oil and Gas Engineering, Engineering Academy, Peoples’ Friendship University of Russia (RUDN University). Research interests: search and exploration of hydrocarbon fields, study of the geological structure of the Arab plate and Mesopotamia
6, Miklukho-Maklaya str., Moscow, 117198, Russian FederationReferences
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