بررسی توسعه کارست های کنگلومرایی بر اساس مطالعات صحرایی و آزمایشگاهی (مطالعه موردی: منطقه تنگه شبیخون، شهرستان خرم آباد)

نویسندگان

1 دانشیار گروه زمین‌شناسی، دانشکده علوم، دانشگاه لرستان، خرم‌آباد، ایران

2 دانشجوی دکترا رسوب‌شناسی و سنگ‌شناسی رسوبی، دانشکده علوم، دانشگاه بوعلی‌سینا، همدان، ایران. کارشناس آزمایشگاه مرکزی دانشگاه لرستان، خرم‌آباد، ایران

چکیده

یکی از پدیده­های قابل­توجه زمین­شناسی در کنگلومرای سازند امیران در منطقه شبیخون شهرستان خرم­آباد، توسعه کارست­ با توزیع، اشکال و اندازه­های مختلف است که باعث ایجاد جاذبه ژئوتوریسمی منحصر به فردی در این منطقه شده است. تاکنون پژوهشی در زمینه توسعه و تشکیل کارست در رخساره­های کنگلومرایی در ایران انجام نشده است. از آنجایی که توسعه کارست در رخساره­های تخریبی درشت دانه نظیر کنگلومراها به ندرت اتفاق می­افتد، لذا در پژوهش حاضر کارست­های توسعه یافته در کنگلومراهای سازند امیران در منطقه مذکور با استفاده از مطالعات صحرایی و آزمایشگاهی بررسی شده­اند. بر اساس مطالعات صحرایی، ویژگی­های سنگ­شناسی، نشت آب در امتداد شکستگی و سطوح لایه­بندی، پوشش خزه، جهت شیب دامنه و قلیایی بودن آب­ از عوامل اصلی توسعه کارست در منطقه تشخیص داده شدند. برای مطالعات آزمایشگاهی، از آزمایش دوام وارفتگی و ویژگی­های سنگ­شناسی استفاده شد. نتایج آزمایش دوام وارفتگی (تا 15 چرخه) روی چهار نمونه مختلف کنگلومرا نشان داد که نمونه با سیمان کلسیتی  (Id15 = 97.56%)میزان فرسایش و تخریب کم­تری نسبت به سایر نمونه­های فاقد سیمان کلسیتی (Id15 = 86.16–93.98%) داشته است. علاوه بر تأثیر نوع سیمان و خمیره رسی در فرسایش و تخریب کنگلومراها و در نتیجه توسعه کارست، قلیایی بودن آب منطقه نیز نقش بسزایی در فرسایش و تخریب کنگلومراهای بدون سیمان کلسیتی و در نتیجه توسعه شدیدتر کارست در آن­ها در مقایسه با کنگلومرای با سیمان کلسیتی داشته است. به هر حال، برخی از کارست­ها به دلیل انحلال سیمان کلسیتی شکل گرفته­اند که فراوانی کم­تری نسبت به کارست­هایی که در سایر کنگلومراهای فاقد سیمان کلسیتی تشکیل شده­اند، دارند. در واقع بررسی­ها نشان­دهنده این است که کارست­های کنگلومرایی غالباً از نوع فرسایشی هستند. به طور کلی، نتایج مطالعات سنگ­شناسی و آزمایشگاهی در تطبیق خوبی با شواهد صحرایی در ارتباط با چگونگی و شدت کارست­زایی منطقه مورد مطالعه هستند.

کلیدواژه‌ها


عنوان مقاله [English]

Investigating the development of conglomeratic karsts based on field and laboratory studies (Case study: Tange Shabikhun region, Khoramabad city)

نویسندگان [English]

  • A. Jamshidi 1
  • M. Sedaghatnia 2
1 Assoc. Prof., Dept., of Geology, Faculty of Science, Lorestan University, Khorramabad, Iran
2 Ph. D., student sedimentology and sedimentary rocks, Faculty of Science, Bu Ali Sina University, Hamedan, Iran. Expert of the Central Laboratory of Lorestan University, Khorramabad, Iran
چکیده [English]

One of the significant geological phenomena in the conglomerate of the Amiran Formation in Shabikhun region of Khorramabad city is the karsts development with different distribution, shapes and sizes, which has created a unique geotourism attraction in this region. Since the development of karst rarely occurred in the coarse-grained detrital facies such as conglomerates, therefore, in the present study, the karsts developed in the conglomerate of Amiran Formation in the mentioned region have been investigated using field and laboratory studies. Based on field studies, petrographic characteristics, water seepage along fractures and bedding surfaces, algal cover, dip direction of slope and alkalinity of water were identified as the main agents of karst development. For laboratory studies, the slake durability test and petrographic characteristics were used. The results of the slake durability test (up to 15 cycles) on four various samples of the conglomerate showed that sample with calcite cement (Id15 = 97.56%) had less erosion and decay than other samples without calcite cement (Id15 = 86.16–93.98%). In addition to effect of the cement type and clay matrix in the erosion and decay of the conglomerates and as a result the karst development, the alkalinity of region water also plays a significant role in the erosion and decay of the conglomerates without calcite cement, and thus more severe development of karst in them compared to conglomerates with calcite cement. However, some karsts are formed due to dissolution of calcite cement, which have been less abundant than those formed in other conglomerates without calcite cement. In fact, investigations indicated that conglomeratic karsts are mostly erosional type. Generally, studies result of petrographic and laboratory are in good agreement with field evidences in relation to the way and intensity of the karstification in the study region.

کلیدواژه‌ها [English]

  • Karst
  • Conglomerate
  • Alkaline water
  • Wetting and drying
  • Khorramabad
Aghanabati, A (2004) Geology of Iran. Geological Survey and Mineral Exploration of Iran Press. (In Persian).
Ahmadi, F., Alijani, F., Nasseri, H (2018) Application of remote sensing and geoelectric methods in groundwater exploration in karst areas of southern Kuhdasht, Lorestan. Hydrogeology, 2(2): 29–43. doi.org/10.22034/hydro.2018.5686 (In Persian).
Alavi, M (2004) Regional stratigraphy of the Zagros Fold-and-Thrust Belt of Iran and Its Prof Orland evolution. Amrican Journal of Science, 304: 1– 20. doi.org/10.2475/ajs.304.1.1.
Behzadtabar, P., Ghobadi, M. H (2016) Assessment of Karst development base on lithological, morphological and structural characteristics in the Bid Sorkh region, East of Sahneh, East of Kermanshah. New Findings in Applied Geology, 10(20): 76–91. doi.org/10.22084/nfag.2017.1694 (In Persian).
Cargill, J. S., Shakoor, A (1990) Evaluation of empirical methods for measuring the uniaxial compressive strength of rock. International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 27: 495–503. doi.org/10.1016/0148-9062 (90)91001-N.
Dhakal, G., Yoneda, T., Kato, M., Kaneko, K (2002) Slake durability and mineralogical properties of some pyroclastic and sedimentary rocks. Engineering Geology, 65: 31–45. doi.org/10.1016/S0013-7952 (01)00101-6.
Falcon, N. L (1961) Major earth–Flexuring in the Zagros Mountains of south-west Iran. Quarterly Journal of the Geological Society of London, 117: 367–376. doi.org/10.1144/gsjgs.117.1.036.
Fereidooni, D., Khajevand, R (2019) Utilization of the accelerated weathering test method for evaluating the durability of sedimentary rocks. Bulletin of Engineering Geology and the Environment, 78: 2697–2716. doi.org/10.1007/s10064-018-1267-9.
Ford, D. C., Williams, P. W (2012) Karst Geomorphology and Hydrology. Publisher: Springer Dordrecht.
Franklin, J. A., Chandra, A (1972) The slake durability test. International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 9: 325–341. doi.org/10.1016/0148-9062(72)90001-0.
Geological Survey and Mineral Exploration of Iran (2023) https://gsi.ir, Accessed 7 September 2023.
Ghobadi, M., Mousavi, S (2014) The effect of pH and salty solutions on durability of sandstones of the Aghajari Formation in Khouzestan province, southwest of Iran. Arabian Journal of Geosciences, 7: 641–653. doi.org/10.1007/s12517-012-0741-0.
Ghobadi, M. H (2007) Karst Engineering Geology. Bu Ali Sina University Press. (In Persian).
Ghobadi, M. H., Ghorbani Saber, A (2011) Studying the characteristics of karst geomorphology in Khorramabad city. Proceedings of: 6th Conference of Engieering Geology and the Environment, Tarbiat Modares University, Tehran, Iran. (In Persian).
Ghobadi, M. H., Karrari, S. S., Almasikia, H (2019) Evaluation of formation Karst potential with analysis hierarchy method in Khozestan province. New Findings in Applied Geology, 13(25): 72–84.
Ghobadi, M. H., Taleb Beydokhti, A. R., Nikudel, M.R., Asiabanha, A., Karakus, M (2016) The effect of freeze–thaw process on the physical and mechanical properties of tuff. Environmental Earth Sciences, 75: 846. doi.org/10.1007/s12665-016-5664-8.
Gupta, V., Ahmed, I (2007) The effect of pH of water and mineralogical properties on the slake durability (degradability) of different rocks from the Lesser Himalaya, India. Engineering Geology, 95: 79–87.
Han, Z., Tang, C., Wu, P., Zhang, R., Zhang, C., Sun, J (2015) Hydrogeochemical characteristics and associated mechanism based on groundwater dating in a karstic basin, Guizhou Province, China. Environmental Earth Sciences, 73: 67–76. doi.org/10.1007/s12665-014-3395-2
Hatamifard, R., Saffari, A., Myamani, M., Karimi, H (2018) Evaluating hydrodynamic behavior and karst development in the ‎Gareen anticline ‎(case study: Alashtar and NourAbad karstic aquifers)‎. Geography and Environmental Planning, 29(3): 15–34. doi.org/10.22108/gep.2018.101464.1014 (In Persian).
Iran Meteorological Organization (2023) https://www.irimo.ir, Accessed 1 September 2023.
ISRM (1981) In: Brown ET (ed) ISRM suggested: rock characterization, testing and monitoring methods. Pergamon, Oxford.
James, G. A., Wynd, J. G (1965) Stratigraphic Nomenclature of Iranian Oil Consortium Agreement Area1. AAPG Bulletin, 49(12): 2182–2245.
Jamshidi, A (2023) Slake durability evaluation of granitic rocks under dry conditions and slaking solution and its prediction using petrographic and strength characteristics. Bulletin of Engineering Geology and the Environment, 82: 120. doi.org/10.1007/s10064-023-03134-2.
Jamshidi, A., Sedaghatnia, M (2023) The slake durability of argillaceous and non-argillaceous rocks: insights from effects of the wetting–drying and rock lumps abrasion. Rock Mechanics and Rock Engineering, 56: 5115–5131. doi.org/10.1007/s00603-023-03318-y.
Kayabali, K., Beyaz, T., Kolay, E (2006) The effect of the pH of the testing liquid on the slake durability of gypsum. Bulletin of Engineering Geology and the Environment, 65: 65–71. doi.org/10.1007/s10064-005-0027-9.
Kazemi, R., Ghermezcheshmeh, B (2021) Investigating the impact of drought on flow duration curve in karst catchments (case study: Kaka-Reza catchment). Environment and Water Engineering, 7(3): 433–443. doi.org/10.22034/jewe.2021.265822.1499 (In Persian).
Khajevand, R., Fereidooni, D (2022) The effects of water acidity and engineering properties on rock durability. Earth Sciences Research Journal, 26: 69–82. doi.org/10.15446/esrj.v26n1.76468.
Khanlari, G. R, Momeni, A. A (2012) Geomorphology, hydrogeology and the study of factors affecting to karst development in Garin area, west of Iran. Geography and Territorial Spatial Arrangement, 2(3): 61–74. doi.org/10.22111/gaij.2012.699 (In Persian).
Khosrow Tehrani, Kh., Abyat, A., Afghah, M (2009) Stratigraphy of lower part of Amiran Formation in N.W and S.E of Khorramabad. Applied Geology, 4(3): 121–132. (In Persian).
Maghsoudi, M., Yamani, M., Moghimi, E., Rezvani, M., Baharvand, M (2018) Identification and evaluation of karst geomorphosites using the combined model of Kubalikova and Kirchner (Case Study: Karst geomorphosites in Poldokhtar- Lorestan province). Quantitative Geomorphological Research, 7(1): 1–12. (In Persian).
Milanovic, S., Stevanovic, Z., Jemcov, I (2010) Water losses risk assessment: an example from Carpathian karst. Environmental Earth Sciences, 60(4): 817–827. doi.org/10.1007/s12665-009-0219-x.
Millanovic, P. T (1981) Karst Hydrology. Water Resources Publications, Littleton, Colo.
Molaee, M (2014) Investigating factors affecting karst development in the Green anticline. Unpublished MSc Dissertation, Kharazmi University, Tehran, Iran. (In Persian).
Motiee, H (2003) Geology of Iran (Stratigraphy of Zagros). Geological Survey and Mineral Exploration of Iran Press.
Mustafa, O., Merkel, B (2015) Classification of karst springs based on discharge and water chemistry in Makook karst system, Kurdistan Region, Iraq. FOG-Freiberg Online Geoscience, 39: 1–24.
Nabavi, M. H (1976) An introduction to the geology of Iran. Geological Survey and Mineral Exploration of Iran Press. (In Persian).
Nikudel, M. R., Jamshidi, A., Hafezi Moghaddas, N (2011) An investigation on dissolution and deterioration of building stones in sulfuric and nitric acids solutions. Scientific Quarterly Journal of Geosciences, 20(80): 135–142. doi.org/10.22071/gsj.2018.55244 (In Persian).
Parvin, M., Hatamifard, R (2019) Investigating Karst Geomorphology and the Effects of Drought on Quantitative and Qualitative Characteristics of Water Resources in Gareen Mountains (Lorestan Province). Journal of Geography and Environmental Hazards, 8(3): 1–18. doi.org/10.22067/geo.v0i0.79453 (In Persian).
Parvizpour, S., Jamshidi, A., Sarikhani, R. Ghassemi Dehnavi, A (2022) The pH effect of sulfuric acid on the physico-mechanical properties of Atashkuh travertine, Central Iran. Environmental Earth Sciences, 81: 159. doi.org/10.1007/s12665-022-10282-3.
Raeisi, E (2002) Carbonate Karst Caves in Iran, Evolution of karst: from prekarst to Cessation, Ljubljana- Postojna, 339–344.
Rezaei Banafsheh, M., Kakoolvand, Y (2015) Zoning Lorestan province by using of cluster analysis. Physical Geography Quarterly, 7(26): 41–50. (In Persian).
Ritter, D. F., Kochel, R. C, Miller, J. R (1995) Process Geomorphology, 3rd Edition, Wm. C. Brown Publishers, Dubuque, IA.
Sepahvand, A., Nazari Samani A. A., Mohammadian, H., Ahmadi, H., Feiz Nia, S (2020) Seasonal Variation of the Solute and Determine the Solubility of Limestone Formations. Iranian Journal of Watershed Management Science and Engineering, 14(48): 21–32. (In Persian).
Servati, M. R., Eshghi, A (2005) Geomorphological characteristics of karst landscapes in the Karde watershed (east of Kope-Dagh zone). Geographical Research Quarterly, 48: 1–15 (In Persian).
Stocklin, J (1968) Structural History and Tectonic of Iran: A Review. American Association of Petroleum Geologists Bulletin, 52: 1229–1258.
Taghipour, M., Nikudel, M. R., Farhadian, M. B (2016) Engineering properties and durability of limestones used in Persepolis complex, Iran, against acid solutions. Bulletin of Engineering Geology and the Environment, 75: 967–978. doi.org/10.1007/s10064-015-0821-y.
Torabi-Kaveh, M., Mehrnahad, H., Morshedi, S., Jamshidi, A (2022) Investigating the durability of weak rocks to forecast their long-term behaviors. Bulletin of Engineering Geology and the Environment, 81: 8. doi.org/10.1007/s10064-021-02504-y.
Tucker, M. E (2001) Sedimentary petrology: an introduction to the origin of sedimentary rocks. John Wiley and Sons.
Velayati, S., Khanalizadeh, F (2012) Tectonic strauctures and karst form (The case study: Karde Basin). Geography, 9(31): 171–189. (In Persian).
Yagiz, S (2018) The Effect of pH of the testing liquid on the degradability of carbonate rocks. Geotechnical and Geological Engineering, 36: 2351–2363.