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Paper Information

Journal:   JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)   SUMMER 2009 , Volume 5 , Number 2; Page(s) 111 To 120.
 
Paper: 

SEDIMENTARY ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF FAHLIYAN FORMATION IN CENTER OF FARS

 
 
Author(s):  RASTEGAR LARI A.R.*
 
* GEOLOGICAL DEPARTMENT, FACULTY OF BASIC SCIENCES, ISLAMIC AZAD UNIVERSITY, SHIRAZ BRANCH, SHIRAZ I. R. IRAN
 
Abstract: 

Fahliyan Formation (Volgian - Neocomian) (Early Cretaceous) is a part of Khami Group. This formation has been studied in two sections in center of Fars (southwest of Arsenjan city and west of Sivand city) to determine its facies, sedimentary environments and sequence Stratigraphy. The deposits of Fahlyian Formation consist of carbonate facies which are deposited in a Carbonate Rimmed Shelf. Two sequences with both type 1 and type 2 sequence boundaries are recognized within these deposits which are in accordance with a part of Zuni mega sequence (Lower Zuni III). The age of this formation is referred toTithonian- Vallanginian (Early Cretaceous).

 
Keyword(s): KHAMI GROUP, ARSENJAN, SIVAND, TITHONIAN, VALLANGINIAN
 
References: 
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