DIAGENETIC PROCESSES OF THE GHORBAN MEMBER OF THE SACHUN FORMATION IN TYPE SECTION- (TANG-E- MEHDI, SOUTHERN FLANK OF THE GHAREH ANTICLINE- SOUTH EAST SHIRAZ)

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.

BAVI OWEYDI ABDOLREZA; ADABI MOHAMMAD HOSSEIN; SADEGHI ABAS; AMIRI BAKHTIAR HASAN

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

Journal Paper

Paper Information

Journal: JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES Year:2016 | Volume:32 | Issue:2 (63) Page(s): 1-22

Download Full-Text

Persian Verion

View:

837

Download:

Cites:

Information Journal Paper

Title

DIAGENETIC PROCESSES OF THE GHORBAN MEMBER OF THE SACHUN FORMATION IN TYPE SECTION- (TANG-E- MEHDI, SOUTHERN FLANK OF THE GHAREH ANTICLINE- SOUTH EAST SHIRAZ)

Author(s)

BAVI OWEYDI ABDOLREZA | ADABI MOHAMMAD HOSSEIN | SADEGHI ABAS | AMIRI BAKHTIAR HASAN | Issue Writer Certificate

Keywords

SACHUN FORMATIONQ2

GHORBAN MEMBERQ1

PALEOCENEQ2

EOCENEQ2

GHAREH ANTICLINEQ1

DIAGENETIC PROCESSESQ2

Abstract

The GHORBAN MEMBER of the SACHUN FORMATION (Paleocene-early EOCENE) at type section in south east Shiraz composed of limestone, dolomitic limestone and dolomite.This carbonate member has been affected by various diagenesis processes in marine, meteoric and burial digenetic environment. Result of this study indicates that botryoidal aragonite and bladed calcite cements and micritic envelope are the product of marine phreatic diagenetic environment. Anhedral dolomicrite with fenestral porosity and absence of fossils has been formed in marine vadose diagenetic environment. Mixing zone of marine and phreatic water in the Jahrum and the SACHUN FORMATIONs boundary has provided favorable conditions for formation of porous dolosparite. Oxidation conditions of meteoric vadoze has played important role for oxidizing of outcropped sediment that subsequently have been transported to basin as oxidizing extra clast and bioclasts. Products of meteoric phreatic diagenetic environment include dissolution, neomorphism, silicification and dog tooth, blocky and drusy calcite cements. DIAGENETIC PROCESSES of burial environment include physical and chemical (stylolite) compaction, drusy calcite cement along with dolosparite and dolomicrosparit. Results of uplifting of succession and exposure to the surface had been accompanied with fracture and calcite veins development, dissolutionand iron oxide in iron bearing sediments.

Cites

No record.

References

No record.

Cite

APA: Copy

BAVI OWEYDI, ABDOLREZA, ADABI, MOHAMMAD HOSSEIN, SADEGHI, ABAS, & AMIRI BAKHTIAR, HASAN. (2016). DIAGENETIC PROCESSES OF THE GHORBAN MEMBER OF THE SACHUN FORMATION IN TYPE SECTION- (TANG-E- MEHDI, SOUTHERN FLANK OF THE GHAREH ANTICLINE- SOUTH EAST SHIRAZ). JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 32(2 (63)), 1-22. SID. https://sid.ir/paper/157063/en

Vancouver: Copy

BAVI OWEYDI ABDOLREZA, ADABI MOHAMMAD HOSSEIN, SADEGHI ABAS, AMIRI BAKHTIAR HASAN. DIAGENETIC PROCESSES OF THE GHORBAN MEMBER OF THE SACHUN FORMATION IN TYPE SECTION- (TANG-E- MEHDI, SOUTHERN FLANK OF THE GHAREH ANTICLINE- SOUTH EAST SHIRAZ). JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2016;32(2 (63)):1-22. Available from: https://sid.ir/paper/157063/en

IEEE: Copy

ABDOLREZA BAVI OWEYDI, MOHAMMAD HOSSEIN ADABI, ABAS SADEGHI, and HASAN AMIRI BAKHTIAR, “DIAGENETIC PROCESSES OF THE GHORBAN MEMBER OF THE SACHUN FORMATION IN TYPE SECTION- (TANG-E- MEHDI, SOUTHERN FLANK OF THE GHAREH ANTICLINE- SOUTH EAST SHIRAZ),” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 32, no. 2 (63), pp. 1–22, 2016, [Online]. Available: https://sid.ir/paper/157063/en

Related Journal Papers