PETROGENESIS OF GRANITOID MASSIF OF MOLATALEB (NORTH ALIGUDARZ)

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.

KHAKZAD A.; BAGHERIAN S.

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

Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY) Year:2002 | Volume:11 | Issue:42 Page(s): 3275-3281

Download Full-Text

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

Persian Verion

View:

1,101

Download:

Cites:

Information Journal Paper

Title

PETROGENESIS OF GRANITOID MASSIF OF MOLATALEB (NORTH ALIGUDARZ)

Author(s)

KHAKZAD A. | BAGHERIAN S. | Issue Writer Certificate

Keywords

PETROGENESISQ4

GRANITOIDQ4

Abstract

Molataleh region is Situated north of aligudarz and juxtaposed to The Zagros Thrust. The activities reverse Faults and the main zagros fault, induced The exposures of precambrian, Upper precambrian- Lower cambrian, triassic and jurassic Metamorphic complex. The effects of various metamorphic eposides at times can be Observed on these rocks. Following The Laramian Orogeny, The intrusive GRANITOID mass, affected the metamorphic rocks of the region. The lithological composition is mainly composed of granite, granodiorite and Monzogranite. The Mineralogical, Lithogical, and geochemical Studies along With field observation indicate the molataleb granitodic mass is "s Type" and palingenetic GRANITOIDes. The tectonic discrimination diagrams Showed that the GRANITOID mass is of post-Orogenic Type. Additionally, regarding the geochemical affinities With other granitioids of adjacent (Borujerd, Hamadan, Buin-Mianadasht and others), They have been injected after the Laramian orogeny.

Cites

No record.

References

پتروژنز توده گرانیتوییدی بویین- میاندشت

Cite

APA: Copy

KHAKZAD, A., & BAGHERIAN, S.. (2002). PETROGENESIS OF GRANITOID MASSIF OF MOLATALEB (NORTH ALIGUDARZ). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), 11(42), 3275-3281. SID. https://sid.ir/paper/70423/en

Vancouver: Copy

KHAKZAD A., BAGHERIAN S.. PETROGENESIS OF GRANITOID MASSIF OF MOLATALEB (NORTH ALIGUDARZ). JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY)[Internet]. 2002;11(42):3275-3281. Available from: https://sid.ir/paper/70423/en

IEEE: Copy

A. KHAKZAD, and S. BAGHERIAN, “PETROGENESIS OF GRANITOID MASSIF OF MOLATALEB (NORTH ALIGUDARZ),” JOURNAL OF SCIENCES (ISLAMIC AZAD UNIVERSITY), vol. 11, no. 42, pp. 3275–3281, 2002, [Online]. Available: https://sid.ir/paper/70423/en

Related Journal Papers