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Information Journal Paper

Title

BASEMENT TECTONICS INVESTIGATION OF DEZFUL EMBAYMENT, BETWEEN KAZERON AND HENDIJAN FAULTS

Pages

  47-61

Abstract

 The area under investigation is, DEZFUL EMBAYMENT, between KAZERON and HENDIJAN faults and investigation of its tectonic position is the main aim of this study. In order to this, results of previous workers have compiled together. In the other hand, geologic and seismologic data have integrated with geophysical data and interpretations. Therefore, it appears that formation of southern DEZFUL EMBAYMENT is the result of BASEMENT configuration and its magnetic anomalies is adapted on structural boundaries. Thus, KHARK MISH-Hendijan uplift and Borazjan embayment have introduced as BASEMENT uplift and embayment.In the other hand, according to all evidence, HENDIJAN, KHARK MISH, KAZERON, Zagros Frontal Faults and Mountain Front faults are BASEMENT faults.

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    APA: Copy

    MANAFI, MOJTABA, & ARIAN, MEHRAN. (2008). BASEMENT TECTONICS INVESTIGATION OF DEZFUL EMBAYMENT, BETWEEN KAZERON AND HENDIJAN FAULTS. JOURNAL OF THE EARTH, 3(1), 47-61. SID. https://sid.ir/paper/193072/en

    Vancouver: Copy

    MANAFI MOJTABA, ARIAN MEHRAN. BASEMENT TECTONICS INVESTIGATION OF DEZFUL EMBAYMENT, BETWEEN KAZERON AND HENDIJAN FAULTS. JOURNAL OF THE EARTH[Internet]. 2008;3(1):47-61. Available from: https://sid.ir/paper/193072/en

    IEEE: Copy

    MOJTABA MANAFI, and MEHRAN ARIAN, “BASEMENT TECTONICS INVESTIGATION OF DEZFUL EMBAYMENT, BETWEEN KAZERON AND HENDIJAN FAULTS,” JOURNAL OF THE EARTH, vol. 3, no. 1, pp. 47–61, 2008, [Online]. Available: https://sid.ir/paper/193072/en

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