CAPROCK EVOLUTION OF ASMARI RESERVOIR IN GACHSARAN

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.

POORMORAD SAEID; AMIRI BAKHTIAR HASAN; JAFARI ABOLGHASEM; PARSAEI AFSHIN

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

Journal Paper

Paper Information

Journal: JOURNAL OF THE EARTH Year:2010 | Volume:4 | Issue:4 Page(s): 1-12

Download Full-Text

Persian Verion

View:

3,436

Download:

Cites:

Information Journal Paper

Title

CAPROCK EVOLUTION OF ASMARI RESERVOIR IN GACHSARAN

Author(s)

POORMORAD SAEID | AMIRI BAKHTIAR HASAN | JAFARI ABOLGHASEM | PARSAEI AFSHIN | Issue Writer Certificate

Keywords

KEY BEDQ3

CAP ROCKQ2

GACHSARANQ3

FORMATIONQ3

SEMQ3

EDXQ3

Abstract

The mudstone is main Caprock in the GACHSARAN Field. This Field is located at 220 km south east of AhwazThis Caprock iuvistigated by Gamma, Sonic log, SEM whit EDX. This Caprock divided by 6 keybeds the thiknes in some area is decreased that is related to tectonic activity. The more thikness of Caprock is on the north limb of field and in some wells, This thickness get 60 meter. The more thicknes is related to C Keybed. The comparision of changes whith dip FORMATION shows that chang of thickness always is not submission dip FORMATION. Anhydrit crystals is effected diagenestic and replacement calcitization processes is best marks to show that. The petrophysical studies and lithological changes are cases studied at he sobkha –lagon that is suggested for GACHSARAN FORMATION litological changes can be a sign alternactiv climates of warm and dry in depositional urrent of Caprock.

Cites

No record.

References

Cite

APA: Copy

POORMORAD, SAEID, AMIRI BAKHTIAR, HASAN, JAFARI, ABOLGHASEM, & PARSAEI, AFSHIN. (2010). CAPROCK EVOLUTION OF ASMARI RESERVOIR IN GACHSARAN. JOURNAL OF THE EARTH, 4(4), 1-12. SID. https://sid.ir/paper/192916/en

Vancouver: Copy

POORMORAD SAEID, AMIRI BAKHTIAR HASAN, JAFARI ABOLGHASEM, PARSAEI AFSHIN. CAPROCK EVOLUTION OF ASMARI RESERVOIR IN GACHSARAN. JOURNAL OF THE EARTH[Internet]. 2010;4(4):1-12. Available from: https://sid.ir/paper/192916/en

IEEE: Copy

SAEID POORMORAD, HASAN AMIRI BAKHTIAR, ABOLGHASEM JAFARI, and AFSHIN PARSAEI, “CAPROCK EVOLUTION OF ASMARI RESERVOIR IN GACHSARAN,” JOURNAL OF THE EARTH, vol. 4, no. 4, pp. 1–12, 2010, [Online]. Available: https://sid.ir/paper/192916/en

Related Journal Papers