PETROGENSIS OF GRANITOID MASSIF OF MOLATALEB AREA (NORTH ALIGUDARZ)

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BAGHERIAN S.; KHAKZAD A.

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Journal: GEOSCIENCES Year:2001 | Volume:10 | Issue:41-42 Page(s): 80-83

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Information Journal Paper

Title

PETROGENSIS OF GRANITOID MASSIF OF MOLATALEB AREA (NORTH ALIGUDARZ)

Author(s)

BAGHERIAN S. | KHAKZAD A. | Issue Writer Certificate

Keywords

METAMORPHIC COMPLEXQ4

PRECAMBRIANQ2

LOWER CAMBRIANQ4

LARAMIDQ3

GRANITOIDQ4

PALINGENETICQ4

ALIGUDARZQ2

IRANQ2

Abstract

Molataleb region is situated in the nort of ALIGUDARZ and in the immediate vicinity of the Zagros Thrust Fault Becacome. of the activities of reverse faults and the Zagros Fault, PRECAMBRIAN, Upper PRECAMBRIAN - LOWER CAMBRIAN, Triassic and Jurassic METAMORPHIC COMPLEX have been exposed. The effects of various metamorphic phases of different episodes, can be observed on these rocks. Following the Laramian Orogeny, the intrusive GRANITOID mass, affected the metamorphic rocks of the region. Lithological composition is mainly composed of granite, granodiorite and monzogranite. Mineralogical, lithogical, and geochemical studies along with field observation indicate that the Molataleb Granitoic mass is of "S Type" and PALINGENETIC GRANITOIDes. The tectonic discrimination diagrams showed that the GRANITOID mass is of post Orogenic Type. Additionally, regarding the geochemical affinities With other granitioids of adjacent (Borujerd, Haramian Buin- Mianadasht and others), They have been injected after the Laramian orogeny.

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APA: Copy

BAGHERIAN, S., & KHAKZAD, A.. (2001). PETROGENSIS OF GRANITOID MASSIF OF MOLATALEB AREA (NORTH ALIGUDARZ). GEOSCIENCES, 10(41-42), 80-83. SID. https://sid.ir/paper/31456/en

Vancouver: Copy

BAGHERIAN S., KHAKZAD A.. PETROGENSIS OF GRANITOID MASSIF OF MOLATALEB AREA (NORTH ALIGUDARZ). GEOSCIENCES[Internet]. 2001;10(41-42):80-83. Available from: https://sid.ir/paper/31456/en

IEEE: Copy

S. BAGHERIAN, and A. KHAKZAD, “PETROGENSIS OF GRANITOID MASSIF OF MOLATALEB AREA (NORTH ALIGUDARZ),” GEOSCIENCES, vol. 10, no. 41-42, pp. 80–83, 2001, [Online]. Available: https://sid.ir/paper/31456/en

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