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Information Journal Paper

Title

TECTONICS SETTING OF SEDIMENTARY FACIES IN THE KOPET-DAGH BASEMENT

Author(s)

GHAEMI F. | Issue Writer Certificate 

Pages

  61-79

Abstract

 Detrital sedimentary rocks of AGH-DARBAND area with Paleozoic to late Triassic age, which is the only outcrop of KOPET-DAGH basement, consist of three zones. 1- Paleozoic Metamorphic rocks that processed in deep marine of continental slope by turbidity flow. 2- QARA-GHEITAN FORMATION formed maximum outcrop in AGH-DARBAND area. According to sedimentary structures, this formation formed in debris flow and sheet flood by baraided stream in proximal environment with flowing from North to South. Qara-gheitan’s conglomerates have volcanic sources. Magmatic debris fragments are CALK-ALKALINE granodiorite to tonalite and volcanic debris fragments are high potassic CALK-ALKALINE rhyolite to dacite. Petrological studies show that these rocks are "I- type". These plutonic and volcanic fragments in Qara-gheitan’s conglomerates is due to existence of a magmatic arc in north of AGH-DARBAND which now buried under the young sediments. 3-Sina formation is sequence of shale and sandstone rocks that formed in continental slope basin by classic turbidites. All sandstone rocks of Qara-gheitan and SINA FORMATION are lithic arkose to feldspatic litharenite that originate from dissected to transitional arc. Detrital sedimentary rocks that created in Paleozoic to late Triassic in basement of KOPET-DAGH basin produce in FORELAND BASIN that formed in front of magmatic arc.

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    APA: Copy

    GHAEMI, F.. (2009). TECTONICS SETTING OF SEDIMENTARY FACIES IN THE KOPET-DAGH BASEMENT. SEDIMENTARY FACIES, 2(1), 61-79. SID. https://sid.ir/paper/199842/en

    Vancouver: Copy

    GHAEMI F.. TECTONICS SETTING OF SEDIMENTARY FACIES IN THE KOPET-DAGH BASEMENT. SEDIMENTARY FACIES[Internet]. 2009;2(1):61-79. Available from: https://sid.ir/paper/199842/en

    IEEE: Copy

    F. GHAEMI, “TECTONICS SETTING OF SEDIMENTARY FACIES IN THE KOPET-DAGH BASEMENT,” SEDIMENTARY FACIES, vol. 2, no. 1, pp. 61–79, 2009, [Online]. Available: https://sid.ir/paper/199842/en

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