BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE QOM FORMATION IN TALENKUH SECTION IN SOUTHWEST OF SEMNAN

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.

HOSSEINI NEJAD S.M.; RAMEH H.; AHARIPOUR R.

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

Journal Paper

Paper Information

Journal: APPLIED SEDIMENTOLOGY Year:2016 | Volume:4 | Issue:7 Page(s): 101-116

Download Full-Text

Persian Verion

View:

710

Download:

Cites:

Information Journal Paper

Title

BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE QOM FORMATION IN TALENKUH SECTION IN SOUTHWEST OF SEMNAN

Author(s)

HOSSEINI NEJAD S.M. | RAMEH H. | AHARIPOUR R. | Issue Writer Certificate

Keywords

BIOSTRATIGRAPHYQ2

SEDIMENTARY ENVIRONMENTQ2

QOM FORMATIONQ2

BENTHIC FORAMINIFERAQ2

SOUTHWEST OF SEMNANQ1

Abstract

The QOM FORMATION in Talenkuh section with 605 meters thick is located 50 kilometers SOUTHWEST OF SEMNAN and includes six rock units which mainly consists of limestone, alternating of limestone and marl, marl, marly limestone, and gypsum. Lower boundary of the QOM FORMATION in this section with Lower red Formation is unconformable and its upper boundary is missing by faulting or erosion. By biostratigraphic studies, 34 genera and 18 species of BENTHIC FORAMINIFERA were identified. Three assemblages have been recognized by distribution of these BENTHIC FORAMINIFERA in the studied section that indicate Chattian? Burdigalian age. Field evidences and petrographic studies together with microfacies analysis, led to recognition 1 conglomerate lithofacies, 1 evaporite facies and 10 microfacies that deposited in 5 SEDIMENTARY ENVIRONMENTs consists of: supratidal, tidal flat, lagoon, shoal and shallow open marine. Therefore, for the Talenkuh section, a carbonate platform in the homoclinal ramp has been suggested.

Cites

No record.

References

No record.

Cite

APA: Copy

HOSSEINI NEJAD, S.M., RAMEH, H., & AHARIPOUR, R.. (2016). BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE QOM FORMATION IN TALENKUH SECTION IN SOUTHWEST OF SEMNAN. APPLIED SEDIMENTOLOGY, 4(7), 101-116. SID. https://sid.ir/paper/260630/en

Vancouver: Copy

HOSSEINI NEJAD S.M., RAMEH H., AHARIPOUR R.. BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE QOM FORMATION IN TALENKUH SECTION IN SOUTHWEST OF SEMNAN. APPLIED SEDIMENTOLOGY[Internet]. 2016;4(7):101-116. Available from: https://sid.ir/paper/260630/en

IEEE: Copy

S.M. HOSSEINI NEJAD, H. RAMEH, and R. AHARIPOUR, “BIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE QOM FORMATION IN TALENKUH SECTION IN SOUTHWEST OF SEMNAN,” APPLIED SEDIMENTOLOGY, vol. 4, no. 7, pp. 101–116, 2016, [Online]. Available: https://sid.ir/paper/260630/en

Related Journal Papers