دانشگاه بوعلی سینا

 News

 Statistics

Number of Journals22
Number of Issues501
Number of Articles5,252
Article View9,906,545
PDF Download6,602,421
Jamshidi, A., Sedaghatnia, M., Mirbiyk sabzevari, K. (2021). The role of structural factors in directing methane and carbon dioxide to the Nosud water transmission tunnel (Azgeleh - northwest of Kermanshah). Comparative Linguistic Research, 15(29), 28-38. doi: 10.22084/nfag.2020.21511.1417
A. Jamshidi; M. Sedaghatnia; K. Mirbiyk sabzevari. "The role of structural factors in directing methane and carbon dioxide to the Nosud water transmission tunnel (Azgeleh - northwest of Kermanshah)". Comparative Linguistic Research, 15, 29, 2021, 28-38. doi: 10.22084/nfag.2020.21511.1417
Jamshidi, A., Sedaghatnia, M., Mirbiyk sabzevari, K. (2021). 'The role of structural factors in directing methane and carbon dioxide to the Nosud water transmission tunnel (Azgeleh - northwest of Kermanshah)', Comparative Linguistic Research, 15(29), pp. 28-38. doi: 10.22084/nfag.2020.21511.1417
Jamshidi, A., Sedaghatnia, M., Mirbiyk sabzevari, K. The role of structural factors in directing methane and carbon dioxide to the Nosud water transmission tunnel (Azgeleh - northwest of Kermanshah). Comparative Linguistic Research, 2021; 15(29): 28-38. doi: 10.22084/nfag.2020.21511.1417

The role of structural factors in directing methane and carbon dioxide to the Nosud water transmission tunnel (Azgeleh - northwest of Kermanshah)

یافته‌های نوین زمین‌شناسی کاربردی
Article 3, Volume 15, Issue 29, March 2021, Pages 28-38    PDF (2.69 M)
DOI: 10.22084/nfag.2020.21511.1417
Authors
A. Jamshidi* ; M. Sedaghatnia; K. Mirbiyk sabzevari
Abstract
Nosud water transfer tunnel with a length of 45 km has been constructed to guide and transfer water in the northwest of Kermanshah. The tunnel passes through several anticlines and synclines and as soon as its axis enters the Garo and Gurpi formations, gases with a volume of more than 400 ppm are drained into the tunnel, which is mainly related to the Azgleh and Kurdish Qasman anticlines. In the Zagros Basin, the Garou and Gurpi Formations are known as high potential oil source rocks. In the study area, despite the predominant type III kerogen, which is mainly of dry origin, a large volume of gases, mainly methane and carbon dioxide, are found. Due to the expansion of Garo and Gurpi formations in the region, gas-prone zones in the tunnel axis are divided into four parts A, B, C, D, which is the largest volume of gas produced in the Kurdish anticline of Qasman and is related to zone D. The gases produced from these areas along with a large volume of water are led into the tunnel through tectonic fractures, which are mainly joints and faults, among which faults play a very important role in the Kurdish anticline of Qasman and the anticline of the herd.
Keywords
Garou formation; Tectonic structures; Gas production; Nosud water supply tunnel; Kermanshah
References

اربابی، م (1390) نقش سازند گرو در اسیدی شدن آب­های تونل آبرسانی نوسود، ازگله، شمال­غرب کرمانشاه. پایان نامه کارشناسی­ارشد، دانشگاه بوعلی­سینا همدان، 111 ص.

اشکان، ع. م (1383) اصول مطالعات ژئوشیمیایی سنگ­های منشأ هیدروکربوری و نفت­ها با نگرش ویژه به حوضه رسوبی زاگرس. انتشارات شرکت ملی نفت ایران. 355 ص.

رفیعی، ب. اربابی، م. محسنی، ح. بیاتی، م (1392) ژئوشیمی آلی، بلوغ حرارتی و پتانسیل هیدروکربن­زایی سازند گورپی، ازگله، شمال­غرب کرمانشاه. نشریه رسوب­شناسی کاربردی، دوره 1، شماره 2، ص 37-29.

مطیعی، ه (1382) زمین­شناسی نفت زاگرس، جلد 1 و 2، سازمان زمین­شناسی کشور، طرح تدوین کتاب زمین شناسی ایران.

مهندسین مشاور ایمن­سازان (1385) بررسی پتانسیل ورود گاز به تونل و نکات ایمنی.

مهندسین مشاور لار (1385) مطالعات مرحله یک تونل انتقال آب نوسود.

شرکت ملی نفت ایران (1388) نقشه زمین­شناسی 100000/1 باینگان.

Ala, M. A., Kinghorn, R. R. F., Rahman, M (1980) Organic geochemistry and source rock characteristics of the Zagros petroleum province, Southwest of  Iran. Petroleum Geology, 3: 61-86.

Bordenave, M. L., Burwood, R (1990) Source rock distribution and maturation in the Zagros Orogenic Belt: Provenance of Asmari and Bangestan reservoir oil accumulations. Organic Geochemistry, 16: 366-387.

Bordenave, M. L., Huc, A.Y (1995) The Cretaceous source rock in the Zagros Foothills of Iran. Reve De Institut Francais Du Petrol50, 727-754.

Frasson, A., Hemqvist, L (2010) Geology, water inflow and grout selection for tunnel sealing: case studies from two tunnels in hard rock, Sweden. In: Proceedings of the ITA- AITES World Tunnel Congress, Vancouver.

Goel, R. K (2014) Tunneling through weak and fragile rocks of Himalayas. International Journal of Mining Science and Technology, 24: 783-790.      

Hunt, J. M (1996) Petrpleum geochemistry and geology.W.H. Freeman and Company, New York, 743p.

Lin, H. I., Lee, C. H (2009) An approach to assessing the hydraulic conductivity disturbance in fractured rocks around the Syueshan tunnel, Taiwan. Tunneling and Underground Space Technology, 24: 222 – 230.

Murris, R. J (1980) Middle East: stratigraphic evolution and oil habitat. AAPG Bulletin, 4: 597-618.

Pasley, M., Gregory, W., Hart, G. F (1991) Organic matter variations in transsgressive and regressive shale. Organic. Geochemistry, 17(4): 483-509.

Riedmuller, G (1987) Neo formation and transformation of clay mineral in tectonic shear zones. Tschermaks mineralogische und petrographische Mitteilungen, 25: 219-242.

Statistics
Article View: 554
PDF Download: 329


Journal management system. designed by sinaweb