DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY MEMBERS3.4.5 OF MILLA FORMATION IN HASANAKDAR AREA, CENTRAL ALBORZ

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KARIMI HOSSEINI H.; LASEMI Y.; JAHANI D.

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Journal: JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK Year:2009 | Volume:2 | Issue:6 Page(s): 63-72

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Title

DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY MEMBERS3.4.5 OF MILLA FORMATION IN HASANAKDAR AREA, CENTRAL ALBORZ

Author(s)

KARIMI HOSSEINI H. | LASEMI Y. | JAHANI D. | Issue Writer Certificate

Keywords

FACIESQ2

DEPOSITIONAL ENVIRONMENTQ2

MILLA FORMATIONQ2

SEQUENCE STRATIGRAPHYQ2

CAMBRIAN AND ORDOVICIANQ3

Abstract

The 3rd, 4th and 5th stratigraphic members of the Mila Formation (Middle Cambrian - Lower Ordovician) are about 120 m thick in the Hasanakdar section and mainly are composed of carbonate and clastic successions. Field and microscopic investigations of this formation have shown that member 3 is mainly comprised of shallow marine mixed carbonate and clastic FACIES; member 4 is attributed by continental FACIES and member 5 is mainly marked by a set of deep sea clastic FACIES. Sequence stratigraphic analysis of the 3rd, 4th and 5th stratigraphic members led to recognition of 3 depositional sequences (third-order cycles).

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APA: Copy

KARIMI HOSSEINI, H., LASEMI, Y., & JAHANI, D.. (2009). DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY MEMBERS3.4.5 OF MILLA FORMATION IN HASANAKDAR AREA, CENTRAL ALBORZ. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(6), 63-72. SID. https://sid.ir/paper/186839/en

Vancouver: Copy

KARIMI HOSSEINI H., LASEMI Y., JAHANI D.. DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY MEMBERS3.4.5 OF MILLA FORMATION IN HASANAKDAR AREA, CENTRAL ALBORZ. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(6):63-72. Available from: https://sid.ir/paper/186839/en

IEEE: Copy

H. KARIMI HOSSEINI, Y. LASEMI, and D. JAHANI, “DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY MEMBERS3.4.5 OF MILLA FORMATION IN HASANAKDAR AREA, CENTRAL ALBORZ,” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 6, pp. 63–72, 2009, [Online]. Available: https://sid.ir/paper/186839/en

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