JOINT PATTERN STUDY OF BADAMESTAN ANTICLINE ZAGROS MOUNTAINS

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NAVAB POUR P.

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Journal: GEOSCIENCES Year:2001 | Volume:10 | Issue:39-40 Page(s): 26-31

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Information Journal Paper

Title

JOINT PATTERN STUDY OF BADAMESTAN ANTICLINE ZAGROS MOUNTAINS

Author(s)

NAVAB POUR P. | Issue Writer Certificate

Keywords

JOINT STUDYQ4

BADAMESTAN ANTICLINEQ4

ZAGROSQ2

IRANQ2

Abstract

The BADAMESTAN ANTICLINE is stuated in the ZAGROS folded belt of IRAN. Formations outcropping within the anticline are Gurpi-Pabdeh, Asmari, Gachsaran, Aghajari, and Bakhtiari in ascending order. Study of joint patterns in the Asmari limestone suggests that joint formation is synchronous with folding, and the stress field is symmetrically oriented with respect to the fold axis. Gomieh anticline shows gravitational slip of the Bakhtiari conglomerate on the lower ductile layers. The joints within this formation indicate another younger stress field.

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APA: Copy

NAVAB POUR, P.. (2001). JOINT PATTERN STUDY OF BADAMESTAN ANTICLINE ZAGROS MOUNTAINS. GEOSCIENCES, 10(39-40), 26-31. SID. https://sid.ir/paper/31866/en

Vancouver: Copy

NAVAB POUR P.. JOINT PATTERN STUDY OF BADAMESTAN ANTICLINE ZAGROS MOUNTAINS. GEOSCIENCES[Internet]. 2001;10(39-40):26-31. Available from: https://sid.ir/paper/31866/en

IEEE: Copy

P. NAVAB POUR, “JOINT PATTERN STUDY OF BADAMESTAN ANTICLINE ZAGROS MOUNTAINS,” GEOSCIENCES, vol. 10, no. 39-40, pp. 26–31, 2001, [Online]. Available: https://sid.ir/paper/31866/en

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