FORMATION OF PENCIL STRUCTURES AND ITS RELATIONSHIP TO MAIN STRUCTURES IN THE MAKRAN ZONE

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MORIDI FARIMANI A.A.; POURKERMANI M.

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ISSN: 2588-4824

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Paper Information

Journal: JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY) Year:2001 | Volume:1 | Issue:2 Page(s): 85-95

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Title

FORMATION OF PENCIL STRUCTURES AND ITS RELATIONSHIP TO MAIN STRUCTURES IN THE MAKRAN ZONE

Author(s)

MORIDI FARIMANI A.A. | POURKERMANI M. | Issue Writer Certificate

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Abstract

One kind of deformation that was found in special facies in the Makran zone is pencil structures. This type of structure mainly formed in shale, siltstone and sometimes in finegraind sandstone. It seems that its formation is a kind of tectonic which develops during a metamorphic process before forming schistosity. In the other word, it can be mentioned that the pencil structures can be formed in special facies, when they are in specific condition such as intersect bedding or two cleavages in the early stgages of slaty cleavage. In many cases there is a loose relationship between slaty cleavages and large geological structures such as foldings, and almost they are in the same direction with axial plane. Therefore, it can be said that pencil structures are occured parallel to b axis (axia of folding).

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APA: Copy

MORIDI FARIMANI, A.A., & POURKERMANI, M.. (2001). FORMATION OF PENCIL STRUCTURES AND ITS RELATIONSHIP TO MAIN STRUCTURES IN THE MAKRAN ZONE . JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), 1(2), 85-95. SID. https://sid.ir/paper/44024/en

Vancouver: Copy

MORIDI FARIMANI A.A., POURKERMANI M.. FORMATION OF PENCIL STRUCTURES AND ITS RELATIONSHIP TO MAIN STRUCTURES IN THE MAKRAN ZONE . JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY)[Internet]. 2001;1(2):85-95. Available from: https://sid.ir/paper/44024/en

IEEE: Copy

A.A. MORIDI FARIMANI, and M. POURKERMANI, “FORMATION OF PENCIL STRUCTURES AND ITS RELATIONSHIP TO MAIN STRUCTURES IN THE MAKRAN ZONE ,” JOURNAL OF SCIENCE (KHARAZMI UNIVERSITY), vol. 1, no. 2, pp. 85–95, 2001, [Online]. Available: https://sid.ir/paper/44024/en

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