GEOLOGY AND STRATIGRAPHY OF PART OF SOUTH CHAHARMAHAL VA BAKHTIARI (FROM DEH-RASHID TO BIDLEH) ALONG WITH MAP AND GEOLOGICAL MAP INTERPRETATION OF THE REGION

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HALABIAN A.H.

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Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2003 | Volume:13 | Issue:49 Page(s): 4017-4032

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Title

GEOLOGY AND STRATIGRAPHY OF PART OF SOUTH CHAHARMAHAL VA BAKHTIARI (FROM DEH-RASHID TO BIDLEH) ALONG WITH MAP AND GEOLOGICAL MAP INTERPRETATION OF THE REGION

Author(s)

HALABIAN A.H. | Issue Writer Certificate

Keywords

GEOLOGYQ3

BAGH HEY RAN FAULTQ3

BAROTE STRUCTUREQ4

LALON STRUCTUREQ4

FARSGROUPQ4

BAKHTIARI FORMATIONS ASMARI FORMATIONQ4

Abstract

The studies area is situated in the south of Chaharmahal Va Bakhtiari between the eastern longtitude of 50°, 28° to 51°, 13° and north lattiude of 31°, 20° and 31°, 38°.The only existing geological map of the region is the map of Boroujen with a scale of 1:250,000, prepared by Ministry of Oil that with regard to the scale of the map, the studied region with brief geological information is observable on it. Therefore preparing the map of the above said region with geological interpretations and stratigraphic details seemed necessary. This region is divided by Bagh Heyran fault into two eastern and western zones. The eastern part is situated on high Zagross zone and its sediments date back to Paleozoic and Mesozoic eras. The significant characteristic of this zone is plenitude of faults and shattered structures. Sediments of this zone equals structure of Barote, Zygone, Lalone and Milia. In addition, carbonate sediments dating back to Jurassic and cretaceous periods are also discernible. The faults of this zone, in the south of Bagh Heyran village have a N-340 direction and in the north and north-west of the ahove mentioned village they show an east-west direction. The western zone that includes the main part of the studied zone contains sediments from the third and fourth eras. Main structures constituting this zone include: 1.Eocene sediments which are mainly calcareous and are sometimes converted to dolomite lime and dolomite. 2. Oligocene sediments which are mainly calcareous, Marne lime and occasionally chille. 3. Formation asmari inducing limestones and marne limestones. 4. Fars group that in the inferior section includes conglomera and in the upper part comprises chalk contatining marnes. silts tone and sandstone.5. Bakhtiari formations including conglomera and sandstone. 6. Sediments of the fourth era that in this zone are observable in the form of terraces, young alluviums and alluvial fans. The faults of this zone have north-west-south-east, north-east-south-west and north-south directions. At the end the geological map of the region with all details and guides was prepared that it is hoped to be used in development projects.

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APA: Copy

HALABIAN, A.H.. (2003). GEOLOGY AND STRATIGRAPHY OF PART OF SOUTH CHAHARMAHAL VA BAKHTIARI (FROM DEH-RASHID TO BIDLEH) ALONG WITH MAP AND GEOLOGICAL MAP INTERPRETATION OF THE REGION. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 13(49), 4017-4032. SID. https://sid.ir/paper/70560/en

Vancouver: Copy

HALABIAN A.H.. GEOLOGY AND STRATIGRAPHY OF PART OF SOUTH CHAHARMAHAL VA BAKHTIARI (FROM DEH-RASHID TO BIDLEH) ALONG WITH MAP AND GEOLOGICAL MAP INTERPRETATION OF THE REGION. JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2003;13(49):4017-4032. Available from: https://sid.ir/paper/70560/en

IEEE: Copy

A.H. HALABIAN, “GEOLOGY AND STRATIGRAPHY OF PART OF SOUTH CHAHARMAHAL VA BAKHTIARI (FROM DEH-RASHID TO BIDLEH) ALONG WITH MAP AND GEOLOGICAL MAP INTERPRETATION OF THE REGION,” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 13, no. 49, pp. 4017–4032, 2003, [Online]. Available: https://sid.ir/paper/70560/en

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