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Information Journal Paper

Title

THE STUDY OF ORIGINAL AND ECONOMIC APPLIED CLAY MINERALS OF TORRENTIAL DEPOSITS OF WATER SHED AT CHANDAB

Pages

  3261-3274

Abstract

 Clay minerals spectrum of Chandab basin from abundance following: Crronsite %46.67, Illite %40, MONTMORIONITE %13.33. There is cholorite in the subbasines (1-1-1, 1-1-2, 1-1-3) by reason of abundance of Fe minerals-which is from kind of SEGONFLANT. Mix mineral CORRONSITE (make from Chlorite and smectite) therefore abundance of Mg in the pyroclastic rocks which exist in subbasines (1-1-3, 1-1-2). Because of reduce Fe consistency along Chandab basin which reduced from SEGONFLANT mineral and increased CORRONSITE mineral. About %60 from basin clay minerals have high expansive and in period of time which make. ARGILITe zone and reduce soil capilarity. According to study on clay soil basin, it suitable for making the brick.

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    APA: Copy

    ANSARIRAD, P., AMINSOBHANI, E., & MOTAMED, A.. (2002). THE STUDY OF ORIGINAL AND ECONOMIC APPLIED CLAY MINERALS OF TORRENTIAL DEPOSITS OF WATER SHED AT CHANDAB. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 11(42), 3261-3274. SID. https://sid.ir/paper/70424/en

    Vancouver: Copy

    ANSARIRAD P., AMINSOBHANI E., MOTAMED A.. THE STUDY OF ORIGINAL AND ECONOMIC APPLIED CLAY MINERALS OF TORRENTIAL DEPOSITS OF WATER SHED AT CHANDAB. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2002;11(42):3261-3274. Available from: https://sid.ir/paper/70424/en

    IEEE: Copy

    P. ANSARIRAD, E. AMINSOBHANI, and A. MOTAMED, “THE STUDY OF ORIGINAL AND ECONOMIC APPLIED CLAY MINERALS OF TORRENTIAL DEPOSITS OF WATER SHED AT CHANDAB,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 11, no. 42, pp. 3261–3274, 2002, [Online]. Available: https://sid.ir/paper/70424/en

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