MINERALOGY – PETROFABRIC OF GHORVEH METAMORPHIC COMPLEX (NW OF 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.

ZAKARIAEE J.; MONSEF I.

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

Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2010 | Volume:20 | Issue:77 (GEOLOGY ISSUE) Page(s): 203-220

Download Full-Text

Persian Verion

View:

1,101

Download:

Cites:

Information Journal Paper

Title

MINERALOGY – PETROFABRIC OF GHORVEH METAMORPHIC COMPLEX (NW OF IRAN)

Author(s)

ZAKARIAEE J. | MONSEF I. | Issue Writer Certificate

Keywords

GHORVEH METAMORPHIC COMPLEXQ3

DEFORMATIONQ3

LPOQ3

BASAL SLIP SYSTEMQ3

RHOMB SLIP SYSTEMQ3

Abstract

Introduction: The GHORVEH METAMORPHIC COMPLEX consists of regional and contact metamorphic rocks. The regional metamorphic rocks are including meta-sediments and metalimestone and are related to green schist to amphibolite facies.Aim: The contact metamorphic series are schist, marbls and quartzite and are inferred to result from hornblend to pyroxene hornfels facies.Methods: Studying of oriented thinsection using of universal stage.Results: The LPO Patterns of quartz in regional metamorphic schists show BASAL SLIP SYSTEM along a<a>direction that confirms the green schist facies condition. The pattern of c- axes distributions of quartz in the marbles reveals a basal and RHOMB SLIP SYSTEM along a<a>direction that are consistent with green schist to lower amphibolite facies.Conclusions: According to microstructural studies two discrete DEFORMATIONal events are recorded in Ghorveh metamorphic rocks. The first DEFORMATIONal phase (D1) forms a first schistosity (S1) and inter-tectonic staurolite and garnet porphyroblasts. The second phase of DEFORMATION (D2) as a S2 fabric followed by syn to post-tectonic andalusite, sillimanite and cordierite porphyroblasts. In the last stage, the retrograde metamorphic events are created from emplacement of metamorphic rocks. As result, the proposed P-T-t path indicates a clockwise path with maximum temperature 700oc and maximum pressure 4 Kbar for GHORVEH METAMORPHIC COMPLEX.

Cites

No record.

References

No record.

Cite

APA: Copy

ZAKARIAEE, J., & MONSEF, I.. (2010). MINERALOGY – PETROFABRIC OF GHORVEH METAMORPHIC COMPLEX (NW OF IRAN). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 20(77 (GEOLOGY ISSUE)), 203-220. SID. https://sid.ir/paper/70597/en

Vancouver: Copy

ZAKARIAEE J., MONSEF I.. MINERALOGY – PETROFABRIC OF GHORVEH METAMORPHIC COMPLEX (NW OF IRAN). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2010;20(77 (GEOLOGY ISSUE)):203-220. Available from: https://sid.ir/paper/70597/en

IEEE: Copy

J. ZAKARIAEE, and I. MONSEF, “MINERALOGY – PETROFABRIC OF GHORVEH METAMORPHIC COMPLEX (NW OF IRAN),” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 20, no. 77 (GEOLOGY ISSUE), pp. 203–220, 2010, [Online]. Available: https://sid.ir/paper/70597/en

Related Journal Papers