SEQUENCE STRATIGRAPHIC ANALYSIS OF THE OLIGO-MIOCENE SILICICLASTIC RESERVOIR IN MOGHAN AREA, NW IRAN

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AMINI A.A.H.

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Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2009 | Volume:34 | Issue:4 (SECTION: GEOLOGY) Page(s): 1-16

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Title

SEQUENCE STRATIGRAPHIC ANALYSIS OF THE OLIGO-MIOCENE SILICICLASTIC RESERVOIR IN MOGHAN AREA, NW IRAN

Author(s)

AMINI A.A.H. | Issue Writer Certificate

Keywords

SEQUENCE STRATIGRAPHYQ3

OLIGO-MIOCENEQ3

ZIVAH FORMATIONQ3

MOGHAN AREAQ3

IRANQ3

Abstract

Themost important reservoir unit in NW IRAN, known as ZIVAH FORMATION, is well described and its characteristics/are accomplished in the sequence stratigraphic framework. Using both field studies and laboratory measurements the constituent facies/facies associations are di6stinguished. The facies are grouped in to parasequences, system tracts and sequences based on their sedimentological characteristics, stratigraphic position, fining-up or coarsening-up trend, and the nature of their stratal surfaces. Discontinuous and thin coal seams, development of carbonate and Fe-oxide cements, distribution of turbidites, and establishment of incised valleys were used for detection of major strata surfaces. Sequence boundaries and maximum flooding surfaces have received greater attention due to their higher utility in sequence stratigraphic studies. The distinguished sequences are classified in to 2nd to 6th order sequences based on their sedimentological characteristics, thickness, stratigraphic position, and the age of whole formation.Correlating with available sea-level curves from other parts of the world, the 2ndorder cycles are related to worldwide sea-level changes (Eustacy). The 3rd to 4th order cycles are related to structural deformation of the source region and surrounding mountains, affected from regional tectonic. Local environmental conditions (bounding faults activities, waves, and currents, erosion rate) are found responsible for development of 5th to 6th order sequences. The facies/facies associations of LST and FRST are found more susceptible for hydrocarbon reservoir.

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APA: Copy

AMINI, A.A.H.. (2009). SEQUENCE STRATIGRAPHIC ANALYSIS OF THE OLIGO-MIOCENE SILICICLASTIC RESERVOIR IN MOGHAN AREA, NW IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 34(4 (SECTION: GEOLOGY)), 1-16. SID. https://sid.ir/paper/2275/en

Vancouver: Copy

AMINI A.A.H.. SEQUENCE STRATIGRAPHIC ANALYSIS OF THE OLIGO-MIOCENE SILICICLASTIC RESERVOIR IN MOGHAN AREA, NW IRAN. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2009;34(4 (SECTION: GEOLOGY)):1-16. Available from: https://sid.ir/paper/2275/en

IEEE: Copy

A.A.H. AMINI, “SEQUENCE STRATIGRAPHIC ANALYSIS OF THE OLIGO-MIOCENE SILICICLASTIC RESERVOIR IN MOGHAN AREA, NW IRAN,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 34, no. 4 (SECTION: GEOLOGY), pp. 1–16, 2009, [Online]. Available: https://sid.ir/paper/2275/en

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