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Information Journal Paper

Title

THE ROLE OF TECTONIC IN THE SHAZAND KARST GENESIS

Pages

  302-317

Abstract

 The Shazand watershed is at 40 kilo meters south west Arak city, this basin is part of sareband city. This area in view water resources is important areas in Markazi province. The mean of this research distinguish TECTONIC properties and relationship with genes and development of KARSTic AQUIFERE. Meteorology, geology, geophisic, hydrology and HYDROGEOLOGY properties and methods of KARST study did for example research on spring for distinguish KARST structure. Research results show the shazand KARST origins are two TECTONIC and meteoric processes. The shazand KARST formed in limbe of a cynclinal. KARST lithololgy formed massive Limestone's k3, marly limestone k4 and reef limestone's k5. KARST hydrologic regime relat to KARSTic AQUIFERE greatness. Major and minor chanels of ground and meteoric waters apparent as single, duplicate, and triple discharge regimes. Therefore KARSTic AQUIFERE areas different in view development.

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    APA: Copy

    YOUSEFIRAD, M.. (2005). THE ROLE OF TECTONIC IN THE SHAZAND KARST GENESIS. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 15(57 (GEOLOGY ISSUE)), 302-317. SID. https://sid.ir/paper/70462/en

    Vancouver: Copy

    YOUSEFIRAD M.. THE ROLE OF TECTONIC IN THE SHAZAND KARST GENESIS. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2005;15(57 (GEOLOGY ISSUE)):302-317. Available from: https://sid.ir/paper/70462/en

    IEEE: Copy

    M. YOUSEFIRAD, “THE ROLE OF TECTONIC IN THE SHAZAND KARST GENESIS,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 15, no. 57 (GEOLOGY ISSUE), pp. 302–317, 2005, [Online]. Available: https://sid.ir/paper/70462/en

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