FACIES AND DEPOSITIONAL ENVIRONMENTS OF DALICHAI FORMATION IN ANBARAN AREA (NORTH OF ARDABIL )

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KARIM DOUST SH.; MAHARI R.; VASIGH Y.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK Year:2009 | Volume:2 | Issue:6 Page(s): 53-62

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Title

FACIES AND DEPOSITIONAL ENVIRONMENTS OF DALICHAI FORMATION IN ANBARAN AREA (NORTH OF ARDABIL )

Author(s)

KARIM DOUST SH. | MAHARI R. | VASIGH Y. | Issue Writer Certificate

Keywords

DALICHAI FORMATIONQ2

ANBARANQ3

ARDABILQ2

FACIESQ3

DEPOSITIONAL ENVIRONMENTQ2

Abstract

Delichai Formation (Bajocian-Callovian) in ANBARAN region (North of Ardebil) comprises about 49 meters of Sandy–marl limestone with interbeded marly shale layers. Accurate field and laboratory studies upon limestone layer of Delichai Formation lead to the discovery of seven microfacies indicating sedimentary environments related to barrier, dam or open marine under open-sea environments. FACIES in deeper areas sometimes reveal turbidite FACIES which are attributed to slope currents. Sedimentary model offered for these FACIES suggests that a regression sequence comprising at least three smaller sequences has been deposited in the continental slope to barrier in the Jurassic Sea.

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APA: Copy

KARIM DOUST, SH., MAHARI, R., & VASIGH, Y.. (2009). FACIES AND DEPOSITIONAL ENVIRONMENTS OF DALICHAI FORMATION IN ANBARAN AREA (NORTH OF ARDABIL ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(6), 53-62. SID. https://sid.ir/paper/186838/en

Vancouver: Copy

KARIM DOUST SH., MAHARI R., VASIGH Y.. FACIES AND DEPOSITIONAL ENVIRONMENTS OF DALICHAI FORMATION IN ANBARAN AREA (NORTH OF ARDABIL ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(6):53-62. Available from: https://sid.ir/paper/186838/en

IEEE: Copy

SH. KARIM DOUST, R. MAHARI, and Y. VASIGH, “FACIES AND DEPOSITIONAL ENVIRONMENTS OF DALICHAI FORMATION IN ANBARAN AREA (NORTH OF ARDABIL ),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 6, pp. 53–62, 2009, [Online]. Available: https://sid.ir/paper/186838/en

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