FRACTURE SYSTEM OF KOPET-DAGH FOLD BELT, NE BOJNURD

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GHAEMI F.; GHAEMI F.

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Paper Information

Journal: GEOSCIENCES Year:2012 | Volume:21 | Issue:83 Page(s): 77-86

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Information Journal Paper

Title

FRACTURE SYSTEM OF KOPET-DAGH FOLD BELT, NE BOJNURD

Author(s)

GHAEMI F. | GHAEMI F. | Issue Writer Certificate

Keywords

STRIKE-SLIP FAULTQ3

THRUST FAULTQ2

BOJNURDQ2

SYMPATHETIC FAULTSQ2

ACTIVE FAULTQ2

JOINTQ3

FAULT ZONEQ2

Abstract

The Northern Khorasan is one of important active tectonics area. The main faults are strike slip (dextral and sinistral) and minor faults are THRUST FAULTs. Many of THRUST FAULTs are older than strike- slip faults and some of them are younger and are active now. It is because of bending of STRIKE-SLIP FAULTs that converts, them into THRUST FAULTs. We recognized ACTIVE FAULTs based on their characteristics. In this area we have two series of tensile JOINTs and two series of shear JOINTs. Principal stresses have the fallowing attitudes (d1=N9oE, 5o)-(d2=S1oW, 86o)-(d3=N81oW, 1o). Strikeslip faults can be sympathetic. For example the 1997 BOJNURD earthquake on the Yekke-shakh fault affects Baba- aman and Gharlegh faults.

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References

بررسی زمین لرزه های 16 بهمن 1375 بجنورد در شمال خاور ایران

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APA: Copy

GHAEMI, F., & GHAEMI, F.. (2012). FRACTURE SYSTEM OF KOPET-DAGH FOLD BELT, NE BOJNURD. GEOSCIENCES, 21(83), 77-86. SID. https://sid.ir/paper/31971/en

Vancouver: Copy

GHAEMI F., GHAEMI F.. FRACTURE SYSTEM OF KOPET-DAGH FOLD BELT, NE BOJNURD. GEOSCIENCES[Internet]. 2012;21(83):77-86. Available from: https://sid.ir/paper/31971/en

IEEE: Copy

F. GHAEMI, and F. GHAEMI, “FRACTURE SYSTEM OF KOPET-DAGH FOLD BELT, NE BOJNURD,” GEOSCIENCES, vol. 21, no. 83, pp. 77–86, 2012, [Online]. Available: https://sid.ir/paper/31971/en

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