DEPOSITIONAL AND POST DEPOSITIONAL HISTORY OF THE SARCHESHNIEH FORMATION (LOWER APTIAN) IN SOUTH OF AGH-DARBAND AREA, EASTERN KOPET-DAGH BASIN- NE IRAN

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AKHLAGHI M.A.S.; MAHBOUBI ASAD ELAH; MOUSAVI HARAMI SEYED REZA; NAJAFI MAHDI

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Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2006 | Volume:23 | Issue:1 Page(s): 175-192

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Information Journal Paper

Title

DEPOSITIONAL AND POST DEPOSITIONAL HISTORY OF THE SARCHESHNIEH FORMATION (LOWER APTIAN) IN SOUTH OF AGH-DARBAND AREA, EASTERN KOPET-DAGH BASIN- NE IRAN

Author(s)

AKHLAGHI M.A.S. | MAHBOUBI ASAD ELAH | MOUSAVI HARAMI SEYED REZA | NAJAFI MAHDI | Issue Writer Certificate

Keywords

SARCHESHRNEHFORMATIONQ3

KOPET-DAGH BASINQ3

LOWER APTIANQ3

DIAGENESISQ3

Abstract

The Sarcheshmeh Formation (Lower Aptian) has an excellent exposure south of Agh-Darband in the easternmost part of the KOPET-DAGH BASIN. It consists mostly of oolithic and fossiliferous limestones with interbedded shale and calcareous shale. The lower and upper contacts with oolithic and biogenic limestone of Tirgan and gray shale of Sanganeh Formations are conformable. Eight stratigraphic sections were measured and about 235 samples collected from limestone and shale.190 thin sections have been studied by petrographic as well as cathodoluminesce micemicroscopes to interpret the depositional and post depositional history of the Sarcheshmeh Formation. Lateral and vertical lithofacies variation in the study area shows that the Sarcheshmeh Formation, especially the limestones were deposited in tidal flat to open marine environments in a shallow marine carbonate ramp. After deposition, these limestones have been affected by different diagenetic processes including cementation, micritization, borrowing, neomorphism, compaction, dolomitization, silicification, hematitization, dissolution, fracturing and vein-fill. These processes have operated in different diagenetic environments including marine, meteoric, mixed marine-meteoric and burial during three euogenic, mesogenic and telogenic stages.

Cites

NANNOSTRATIGRAPHY OF BOUNDARY OF TIRGAN AND SARCHESHMEH FORMATIONS AT QALEZO SECTION IN THE WEST OF KOPET-DAGH BASIN

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APA: Copy

AKHLAGHI, M.A.S., MAHBOUBI, ASAD ELAH, MOUSAVI HARAMI, SEYED REZA, & NAJAFI, MAHDI. (2006). DEPOSITIONAL AND POST DEPOSITIONAL HISTORY OF THE SARCHESHNIEH FORMATION (LOWER APTIAN) IN SOUTH OF AGH-DARBAND AREA, EASTERN KOPET-DAGH BASIN- NE IRAN. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 23(1), 175-192. SID. https://sid.ir/paper/385946/en

Vancouver: Copy

AKHLAGHI M.A.S., MAHBOUBI ASAD ELAH, MOUSAVI HARAMI SEYED REZA, NAJAFI MAHDI. DEPOSITIONAL AND POST DEPOSITIONAL HISTORY OF THE SARCHESHNIEH FORMATION (LOWER APTIAN) IN SOUTH OF AGH-DARBAND AREA, EASTERN KOPET-DAGH BASIN- NE IRAN. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;23(1):175-192. Available from: https://sid.ir/paper/385946/en

IEEE: Copy

M.A.S. AKHLAGHI, ASAD ELAH MAHBOUBI, SEYED REZA MOUSAVI HARAMI, and MAHDI NAJAFI, “DEPOSITIONAL AND POST DEPOSITIONAL HISTORY OF THE SARCHESHNIEH FORMATION (LOWER APTIAN) IN SOUTH OF AGH-DARBAND AREA, EASTERN KOPET-DAGH BASIN- NE IRAN,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 23, no. 1, pp. 175–192, 2006, [Online]. Available: https://sid.ir/paper/385946/en

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