LITHOSTRATIGRAPHY, FACIES ANALYSIS AND SEDIMENTARY ENVIROMNENTS OF

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

LASEMI Y.; REZAIE P.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2002 | Volume:11 | Issue:43-44 Page(s): 68-79

Download Full-Text

Persian Verion

View:

1,113

Download:

Cites:

Information Journal Paper

Title

LITHOSTRATIGRAPHY, FACIES ANALYSIS AND SEDIMENTARY ENVIROMNENTS OF "BIDOU GROUP" IN FAYZABAD SECTION, NORTH KERMAN

Author(s)

LASEMI Y. | REZAIE P. | Issue Writer Certificate

Keywords

FACIESQ2

SEDIMENTARY ENVIRONMENTSQ4

FACIES ASSOCIATION AND SEQUENCESQ4

Abstract

The "Bidou group" crops out in the north of Kerman, have various thickness and lithology. About 590 meters of this group was studied in the Fayzabad section, 35Kilometers N.W. of Ravar to determin it's FACIES and paleoenvironments. The "Bidou group" consists mainly of conglomerate, sandstone, shale/mudstone and limestone. Three FACIES association are recognized. FACIES association 1 consists of interbedded conglomerate and sandstone. FACIES association 2 is composed of sandstone and shale/mudstone. FACIES association 2 is composed of sandstone and shale/mudstone. FACIES association 3 consists of limestone, sandstone, shale/mudstone. Field and laboratory studies indicate that FACIES association 1 and 2 were deposited in the braided and meandering river environments respectively. FACIES associations 3 represents a shallow marine mixed clastic and carbonate environment. The carbonates of FACIES association 3 include four microFACIES group and deposited in the tidal flat, lagoon, oolitic/bioclastic barrier and open marine subenvironments. The sandstone and shale/mudstone of the mixed carbonate- clastic associations are indication of beach to offshore environment.

Cites

PALAEOICHNOLOGY AND PALAEONTOLOGY OF DINOSAURS IN NORTH OF KERMAN, SOUTH EAST CENTRAL IRAN

References

Cite

APA: Copy

LASEMI, Y., & REZAIE, P.. (2002). LITHOSTRATIGRAPHY, FACIES ANALYSIS AND SEDIMENTARY ENVIROMNENTS OF "BIDOU GROUP" IN FAYZABAD SECTION, NORTH KERMAN. GEOSCIENCES, 11(43-44), 68-79. SID. https://sid.ir/paper/31332/en

Vancouver: Copy

LASEMI Y., REZAIE P.. LITHOSTRATIGRAPHY, FACIES ANALYSIS AND SEDIMENTARY ENVIROMNENTS OF "BIDOU GROUP" IN FAYZABAD SECTION, NORTH KERMAN. GEOSCIENCES[Internet]. 2002;11(43-44):68-79. Available from: https://sid.ir/paper/31332/en

IEEE: Copy

Y. LASEMI, and P. REZAIE, “LITHOSTRATIGRAPHY, FACIES ANALYSIS AND SEDIMENTARY ENVIROMNENTS OF "BIDOU GROUP" IN FAYZABAD SECTION, NORTH KERMAN,” GEOSCIENCES, vol. 11, no. 43-44, pp. 68–79, 2002, [Online]. Available: https://sid.ir/paper/31332/en

Related Journal Papers