Investigations on River Sediments in Chak Sedimentary Basin, Wardak Province, Afghanistan

Authors

  • Hafizullah Rasouli Department of Geology, Geoscience Faculty, Kabul University, Kabul, Jamal Mina 1006, Kabul, Afghanistan
  • Roya Quraishi Department of Hydrometeorology, Geoscience Faculty, Kabul University, Kabul, Jamal Mina 1006, Kabul,Afghanistan
  • Kaltoum Belhassan Geology Department, Faculty of Sciences Dhar Mehraz, Fez, Morocco

DOI:

https://doi.org/10.30564/jgr.v3i4.3574

Abstract

This sedimentary is from a largest basin of Afghanistan, which covers an area of 9772 km2. It is located about 80 km, at west side of Kabul. In this research, we studied different types of heavy and light minerals, gravel analysis in river sediments. Logar River is core stream flowing over basin,it carries diverse masses of sediments from dissimilar parts of surroding montians. Further, in the months of summer while snowmelting is started,transfer diverse materials and cause different traces to be made. Area of basin is enclosed by mountain range and separated into two sections,majore part is Khawat Olya and second one is Khawat Sufla. The main aim of study is to characterize different sizes and types of minerals in river load for the previous geological periods. This research is therefore essential to explain different sizes and type of minerals in river sediments, which is no any study has been conducted in the study area. This study found out that the category of sediments is related to the parental materials that are placed in the close mountains such as; gneiss, limestone, and granite, dissimilar varities of conglomerate, slate, schist, reefs, conglomerate and sandston.

Keywords:

Minerals; Gravel analysis; Sieving analysis; Sediments; Terraces

References

[1] Anthony E. J. & Héquette A., 2007. The grain-size characterization of coastal sand from the Somme estuary to Belgium: sediment sorting processes and mixing in a tide-and storm-Dominated setting. Sedimentary Geology.

[2] Avouac, J.P., and E. Burov,1996. Erosion as a driving mechanism of intracontinental Mountain growth, J.Geophys. Res., 101, 17,747-17, 769.

[3] Böckh, E.G., 1971.Report on the groundwater resources of the city of Kabul, report for undesanstalt für Geowissenschaften und Rohstoffe BGR file number 0021016, 43 p.

[4] Ball, M. M., 2003. Carbonate sand bodies of Florida and Bahamas. Journal of Sedimentary petrology, P.91.

[5] Banks, David, and Soldal, Oddmund, 2002. Towards a policy for sustainable use of Groundwater by non-governmental organizations in Afghanistan: Hydrogeology Journal, v. 10, no. 3, p. 377.

[6] Belhassan, K. 2020. Hydrogeology of the Ribaa –Bittit springs in the Mikkes Basin (Morocco).International Journal of Water Resources and Environmental Science 9 (1): 07 -15, 2020 ISSN 231-2492, © IDOSI Publications, 2020.

[7] Belhassan, K., 2020. Relationship between River and Groundwater: Water table Piezometery of the Mikkes Basin (Morocco. International Journal of Water Resources and Environmental Science 9 (1):01-06,2020 ISSN 2311-2492, © IDOSI Publications, 2020.

[8] Bentley S. J., Sheremet A. & Jaeger J. M.,2006.Event sedimentation, bioturbation, and Preserved sedimentary fabric: Field and model comparisons in three contrasting marine Settings. Continental Shelf Research 26, P. 2108-2124.

[9] Bohannon, R.G., 2005. Geologic map of quadrangle 3468, Chak-e-Wardak (509) and Kabul (510) quadrangles: Afghan Open-File Report (509/510) 2005-1001.

[10] Bohannon, R.G., and Turner, K.J., 2007. Geologic map of quadrangle 3468, Chak Wardak-Syahgerd (509) and Kabul (510) quadrangles, Afghanistan: U.S.Geological Survey.Open-File Report 2005-1107-A. 1 sheet.

[11] Broshears, R.E., Akbari, M.A., Chornack, M.P.,Mueller, D.K., and Ruddy, B.C.,2005. Inventory of ground-water resources in the Kabul Basin, Afghanistan: U.S. Geological Survey Scientific Investigations Report 2005-5090, 34 p.

[12] Colella, A and di Geronimo, I.,1998. Surface sediments and macro fanas of the Grati submarine fan (Ionian sea, Italy a) sedimentary geology.

[13] Elliontt, T., 2001. Siliciclasstic shorlines Sedimentary Environments and facies, 2nd ed., Black wall scientific pub., Oxford.

[14] Folk, R. L.,2004. spectral divission of Limestone types. In: Classification of carbonate Rocks(ed w.E.Ham), 62-84, memoirs of the American Association of petroleum geology, Tulsa, Oklahoma.

[15] gela L. Coe ,2003. The sedimentary Records of sea Level change, british Library, ISBN 052,831113 hard back.

[16] González-Álvarez R. et al.,2005. Paleoclimatic evolution of the Galician continental shelf (NW of Spain) during the last 3000 years: from a storm regime to present conditions. Journal of Marine Systems.

[17] Goff J., McFadgen B. & Chagué-Goff C.,2004. Sedimentary differences between the 2002 Easter storm and the 15th-century Okoropunga tsunami, southeastern North Island, New Zealand. Marine geology.

[18] Herman E. K., Toran L. & White W. B.,2009. Quantifying the place of karst aquifers in the Groundwater to surface water continuum: A time series analysis study of storm behavior in Pennsylvania water resources. Journal of Hydrology.

[19] Horikawa K. & Ito M. 2009. Non-uniform acrossshelf variations in thickness, grain size, and frequency of turbidites in a transgressive outer-shelf, the Middle Pleistocene Kakinokidai Formation, Boso Peninsula, Japan. Sedimentary Geology.

[20] Mike Leeder, 2006. Sedimentology and sedimentary basins, by Grphicraft, Ltd, Hong Kong,Raplika press pvt Ltd, Kundli.

[21] Rasouli, H. and Safi, A. G., 2021. Geological, Soil and Sediment Studies in Chelston Sedimentary Basin, Kabul, Afghanistan. International Journal of Geosciences, 12, 170-193. DOI: https://doi.org/10.4236/ijg.2021.122011.

[22] Rasouli H. Sarwari, M. H., Khairuddin R., Said A.H.,2020 Geological Study of Tangi Mahipar Mountain Range along Kabul Jalalabad road, Afghanistan.DOI: https://dx.doi.org/10.4236/ojg.2020.1010044.

[23] Rasouli H.,2020. Application of soil physical and chemical parameters and its Comparing in Kabul sedimentary basins, Kabul, Afghanistan.

[24] Rasouli H., 2020. WELL DESIGN AND STRATIGRAPHY OF SHEERKHANA DEEP WELL IN CHAK DISTRICT, WARDAK, AFGHANISTAN.International Journal of Geology, Earth &Environmental Sciences، ISSN: 2277-2081, and Open Access, Online International Journal Available at 10 (2) May-August, pp.54-68.

[25] Rasouli H., Shamal S. and Sarwari, M.H. 2021. Geological Study of Dasht-e-Top Sedimentary Basin,Wadak Province, Afghanistan. International Journal of Geosciences, 12, 531-540.DOI: https://doi.org/10.4236/ijg.2021.126029.

[26] Rasouli H., 2019. A STUDY ON SOME RIVER SEDIMENTS, HYDROLOGY AND GEOLOGICALCHARACTERISTICS IN CHAK SEDIMENTARY BASIN, WARDAK,AFGHANISTAN. International Journal of Geology, Earth & Environmental Sciences,ISSN: 2277-2081, and Open Access, Online International Journal Available at Vol.9 2 May-August,pp.49-61/Rasouli.

[27] Sun Y., Gao S. & Li J.,2003. Preliminary analysis of grain-size populations with Environmentally sensitive terrigenous components in marginal sea setting.Chinese Science Bulletin P. 184-186.

[28] Tang X., Chen M., Liu J., Zhang L. & Chen Z.,2004.The anisotropy of magnetic Susceptibility of Core NS97-13 sediments from the Nansha Islands sea area in the Southern South China Sea. Acta Oceanologica Sinica P. 69-70 (in Chiness with English Abstract).

[29] Wright, L. D.,2000. River deltas, in Dasvis, R. A.,J.R(ed.), Caostal Sedimentary environments : Springer – Verlag, New Yark.

[30] Xiao S., Liu W., Li A., Yang S. & Lai Z.,2009. Pervasive autocorrelation of the chemical Index of alteration in sedimentary profiles and its palaeoenvironmental implications. Sedimentology.

Downloads

How to Cite

Rasouli, H., Quraishi, R., & Belhassan, K. (2021). Investigations on River Sediments in Chak Sedimentary Basin, Wardak Province, Afghanistan. Journal of Geological Research, 3(4), 21–29. https://doi.org/10.30564/jgr.v3i4.3574

Issue

Article Type

Articles