CEPHALOPODS AND STRATIGRAPHICAL POSITION OF CEPHALOPOD BED OF SHISHTU FORMATION, IRAN

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.

ASHOURI ALI REZA; YAMINI A.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2006 | Volume:15 | Issue:60 Page(s): 187-178

Download Full-Text

Persian Verion

View:

1,053

Download:

516

Cites:

Information Journal Paper

Title

CEPHALOPODS AND STRATIGRAPHICAL POSITION OF CEPHALOPOD BED OF SHISHTU FORMATION, IRAN

Author(s)

ASHOURI ALI REZA | YAMINI A. | Issue Writer Certificate

Keywords

CEPHALOPOD BEDSQ3

CEPHALOPODQ3

SHISHTU FORMATIONQ3

SHOTORI RANGEQ3

IRANQ2

Abstract

This paper attempts to describe a CEPHALOPOD fauna from the "CEPHALOPOD BEDS" in the SHOTORI RANGE, Central IRAN. The fauna contains 5 genera of nautiloid CEPHALOPODs and 12 genera of ammonoids. Among these, 7 ammonoid genera (Tornoceras, Cheiloceras, Maeneceras, Gonioclymenia, Cyrtoclymenia, Staffites, and Falcitornoceras) and 5 nautiloid genera (Ormoceras, Mooreoceras, Sycoceras, Michelinoceras, and Macroloxoceras) are reported for the first time from IRAN. Ammonoid faunas indicate a Middle (?)/Late Frasnian to Late Famennian age for the "CEPHALOPOD BEDS", confirmed by conodont (Ashouri, 1990, 1995 & 1997) and brachiopod (Rastkar, 1996) studies. Microfacies analysis of the sections indicates that sedimentation occurred in a mostly shallow and high energy sedimentary environment. The distribution of goniatite fauna in eastern as well as northern IRAN suggests similar paleobiological condition and a marine connection of the two regions during the Famennian stage. A paleogeographical map of the Late Devonian and comparison of the goniatite fauna of the study area with Alborz, Kazakhstan, China, North Africa and Europe indicate that these areas were in low latitudes during this time.

Cites

No record.

References

No record.

Cite

APA: Copy

ASHOURI, ALI REZA, & YAMINI, A.. (2006). CEPHALOPODS AND STRATIGRAPHICAL POSITION OF CEPHALOPOD BED OF SHISHTU FORMATION, IRAN. GEOSCIENCES, 15(60), 187-178. SID. https://sid.ir/paper/404752/en

Vancouver: Copy

ASHOURI ALI REZA, YAMINI A.. CEPHALOPODS AND STRATIGRAPHICAL POSITION OF CEPHALOPOD BED OF SHISHTU FORMATION, IRAN. GEOSCIENCES[Internet]. 2006;15(60):187-178. Available from: https://sid.ir/paper/404752/en

IEEE: Copy

ALI REZA ASHOURI, and A. YAMINI, “CEPHALOPODS AND STRATIGRAPHICAL POSITION OF CEPHALOPOD BED OF SHISHTU FORMATION, IRAN,” GEOSCIENCES, vol. 15, no. 60, pp. 187–178, 2006, [Online]. Available: https://sid.ir/paper/404752/en

Related Journal Papers