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Information Journal Paper

Title

THE ORIGIN OF AEOLIAN SEDIMENTS IN THE CHAHNIMEH OF ZABOL

Pages

  9-16

Abstract

 In order to control and against the wind erosion in each area, including the Sistan Plain with 8117 km2 and with an unfavorable and dry climate, understanding the origin of the sand or the removal area of the wind deposits are extremely important. This research includes information collecting from the local erosion, general geomorphology of the region and winds, sampling of sediments for granulometry, morphoscopy and mineralogy testing and preparing thin sections of sediments. So, the major objectives of this research have been determined the critical wind erosion centers (source finding), vulnerability of Chahnimeh water reservoirs and recognition the effects of wind damage in the ZABOL region. Based on the results the occurrence of droughts in the Sistan region and consequently the loss of vegetation, the Hamoon lake plain drying and the existence of the 120-DAY WINDS have been provided a suitable condition for the occurrence of wind erosion and dust storms. The Origin of the current deposits in the water reservoirs of the Chahnimeh in ZABOL city was diagnosed the erosional and grueling winds with the angle of 330 to 360 degrees (north to northwest direction). The main removal facies are abandoned lands, sand prairie lands, saline and bloated land, bed Plain of Hamoon Lake and the northern plains (in Afghanistan). The sand storms and the move of sand dunes are considered as threatening factors.

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    APA: Copy

    JADIDOLESLAMI, M., RAHNAMA RAD, J., & BASIRANI, N.. (2011). THE ORIGIN OF AEOLIAN SEDIMENTS IN THE CHAHNIMEH OF ZABOL. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 7(1), 9-16. SID. https://sid.ir/paper/127069/en

    Vancouver: Copy

    JADIDOLESLAMI M., RAHNAMA RAD J., BASIRANI N.. THE ORIGIN OF AEOLIAN SEDIMENTS IN THE CHAHNIMEH OF ZABOL. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2011;7(1):9-16. Available from: https://sid.ir/paper/127069/en

    IEEE: Copy

    M. JADIDOLESLAMI, J. RAHNAMA RAD, and N. BASIRANI, “THE ORIGIN OF AEOLIAN SEDIMENTS IN THE CHAHNIMEH OF ZABOL,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 7, no. 1, pp. 9–16, 2011, [Online]. Available: https://sid.ir/paper/127069/en

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