PETROGRAPHY AND PETROLOGY OF THE DYKES IN KHOSHUMI AREA, SOUTHWEST OF SAGHAND

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RAZAVI S.M.H.

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ISSN: 2588-4824

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Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2003 | Volume:13 | Issue:49 Page(s): 3993-4004

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Title

PETROGRAPHY AND PETROLOGY OF THE DYKES IN KHOSHUMI AREA, SOUTHWEST OF SAGHAND

Author(s)

RAZAVI S.M.H. | Issue Writer Certificate

Keywords

PETROLOGYQ4

DYKEQ4

SAGHANDQ4

UPPER CRUSTQ4

Abstract

Through the median part of Khoshumi mountains, the Mesozoic granitic rocks have intruded the Precambrian metamorphics of Chapedony Complex. In this way, numerous DYKEs intruded the igneous and metamorphic rocks. Some of the DYKEs are metamorphic and belong to Precambrian age. And some of them have not been metamorphosed.The non-metamorphosed DYKEs are more abundant, their basic to intermediate types include dolerite, and andesitic basalt and trachyandesite. Acidic non-metamorphosed DYKEs are of rhyolite and dacite in composition. Acidic DYKEs indicate to cale-alkaline type composition, and hasic to intermediate DYKEs are associated with alkaline type in series. Basic to intermediate DYKEs are possibly generated from the mantle flow and localized through the local rifts, whereas acidic DYKEs sourced from the UPPER CRUST.

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APA: Copy

RAZAVI, S.M.H.. (2003). PETROGRAPHY AND PETROLOGY OF THE DYKES IN KHOSHUMI AREA, SOUTHWEST OF SAGHAND. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 13(49), 3993-4004. SID. https://sid.ir/paper/70559/en

Vancouver: Copy

RAZAVI S.M.H.. PETROGRAPHY AND PETROLOGY OF THE DYKES IN KHOSHUMI AREA, SOUTHWEST OF SAGHAND. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2003;13(49):3993-4004. Available from: https://sid.ir/paper/70559/en

IEEE: Copy

S.M.H. RAZAVI, “PETROGRAPHY AND PETROLOGY OF THE DYKES IN KHOSHUMI AREA, SOUTHWEST OF SAGHAND,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 13, no. 49, pp. 3993–4004, 2003, [Online]. Available: https://sid.ir/paper/70559/en

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