Abstract
As ostracods are excellent index in determining the paleoenvironment, age and paleoecology of sediments, the ostracods in marls units 1 and 3 of Tarbur Formation have been studied. Tarbur Formation with 712 m thickness is divided into 6 units. In this study, 60 samples of marls units 1 and 3 have been washed, and studied and totally 21 species identified. The ostracods indicate a Maestrichtian age and warm, oxygen-rich and shallow depositional environment for the studied units.
(2011). Introducing the ostracods in marls units 1 and 3 (K1 and K3) of Tarbur Formation in Chehel Cheshmeh Kherameh Mountain (Southeast of Shiraz). Journal of Stratigraphy and Sedimentology Researches, 27(3), 139-148.
MLA
. "Introducing the ostracods in marls units 1 and 3 (K1 and K3) of Tarbur Formation in Chehel Cheshmeh Kherameh Mountain (Southeast of Shiraz)", Journal of Stratigraphy and Sedimentology Researches, 27, 3, 2011, 139-148.
HARVARD
(2011). 'Introducing the ostracods in marls units 1 and 3 (K1 and K3) of Tarbur Formation in Chehel Cheshmeh Kherameh Mountain (Southeast of Shiraz)', Journal of Stratigraphy and Sedimentology Researches, 27(3), pp. 139-148.
CHICAGO
, "Introducing the ostracods in marls units 1 and 3 (K1 and K3) of Tarbur Formation in Chehel Cheshmeh Kherameh Mountain (Southeast of Shiraz)," Journal of Stratigraphy and Sedimentology Researches, 27 3 (2011): 139-148,
VANCOUVER
Introducing the ostracods in marls units 1 and 3 (K1 and K3) of Tarbur Formation in Chehel Cheshmeh Kherameh Mountain (Southeast of Shiraz). Journal of Stratigraphy and Sedimentology Researches, 2011; 27(3): 139-148.
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