RESEARCH ON FRACTURES IN NORTH OF THE TORUD-MOALLEMAN AREA (CENTRAL IRAN, SOUTHEASTERN OF DAMGHAN) AND THEIR RELATION WITH MINERALIZATION

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KEYNEZHAD A.; POURKERMANI M.; ARIAN M.; SAEEDI A.; LOTFI M.

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Journal: JOURNAL OF THE EARTH Year:2010 | Volume:5 | Issue:2 Page(s): 81-97

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Title

RESEARCH ON FRACTURES IN NORTH OF THE TORUD-MOALLEMAN AREA (CENTRAL IRAN, SOUTHEASTERN OF DAMGHAN) AND THEIR RELATION WITH MINERALIZATION

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Keywords

DETERMINISTIC METHODQ2

POROSITYQ2

SATURATIONQ2

LITHOLOGYQ2

ILAMQ2

SARVAKQ2

Abstract

Study area is located in 130 km Southeaster of Damghan city and North of the Jandagh desert between Torud- Moalleman villages. This area situated in Central Iran zone and located between two major faults, Torud fault in South and Anjilu fault in North. This region belongs to Torud-Chahshirin volcano-plutonic band with metamorphic substructure. Volcanic rocks of this area consist of dacite, andesit, trachyandesit, tuff, rhyodacite, rhyolite and andesibasalt also the plutonic rocks consist of Granite and Granodiorite to Diorite. The Paleozoic and Mesozoic sedimentary rocks separated in west of this area. These rocks consist of so many fractures in this fault shear zone that with penetration of hydrothermal solution in fractures and fault system, without mineral veins and mineralized (Au, Ag, Cu, Pb, Zn and Para genes) veins are formed. Near of them different dykes penetrated in some fractures that altered the host rocks. General and detailed geological research (in 12 regions of this area) showed that this area contains of so much fracture and faults that formed relation of left lateral shear zone.Determinated of these small and huge fractures were classified them to D, P, X, T, R and R' fracture groups that each one have tectonic specifics. Another way research of dykes and fracture of them, showed tension regions that located in west and central of study area and agreement with T, R and D types of fracture. Notice to these fractures controlled mineralized veins, we studied all of fractures and the veins of them in 12 Mining areas that resulted mineralized veins located in R, R' and D types of fracture.

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APA: Copy

KEYNEZHAD, A., POURKERMANI, M., ARIAN, M., SAEEDI, A., & LOTFI, M.. (2010). RESEARCH ON FRACTURES IN NORTH OF THE TORUD-MOALLEMAN AREA (CENTRAL IRAN, SOUTHEASTERN OF DAMGHAN) AND THEIR RELATION WITH MINERALIZATION. JOURNAL OF THE EARTH, 5(2), 81-97. SID. https://sid.ir/paper/193019/en

Vancouver: Copy

KEYNEZHAD A., POURKERMANI M., ARIAN M., SAEEDI A., LOTFI M.. RESEARCH ON FRACTURES IN NORTH OF THE TORUD-MOALLEMAN AREA (CENTRAL IRAN, SOUTHEASTERN OF DAMGHAN) AND THEIR RELATION WITH MINERALIZATION. JOURNAL OF THE EARTH[Internet]. 2010;5(2):81-97. Available from: https://sid.ir/paper/193019/en

IEEE: Copy

A. KEYNEZHAD, M. POURKERMANI, M. ARIAN, A. SAEEDI, and M. LOTFI, “RESEARCH ON FRACTURES IN NORTH OF THE TORUD-MOALLEMAN AREA (CENTRAL IRAN, SOUTHEASTERN OF DAMGHAN) AND THEIR RELATION WITH MINERALIZATION,” JOURNAL OF THE EARTH, vol. 5, no. 2, pp. 81–97, 2010, [Online]. Available: https://sid.ir/paper/193019/en

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