PETROGRAPHY, ORIGIN AND MAGMATIC EVOLUTION OF KHUNRANG INTRUSIVE COMPLEX, NORTHWEST OF JIROFT, KERMAN

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.

SEDIGHIAN S.; DARGAHI S.; ARVIN M.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2017 | Volume:26 | Issue:102 Page(s): 207-220

Download Full-Text

Persian Verion

View:

671

Download:

Cites:

Information Journal Paper

Title

PETROGRAPHY, ORIGIN AND MAGMATIC EVOLUTION OF KHUNRANG INTRUSIVE COMPLEX, NORTHWEST OF JIROFT, KERMAN

Author(s)

SEDIGHIAN S. | DARGAHI S. | ARVIN M. | Issue Writer Certificate

Keywords

INTRUSIVE COMPLEXQ2

SANANDAJ-SIRJAN ZONEQ2

VOLCANIC ARCQ2

NEOTETHYSQ2

KERMANQ2

Abstract

Khunrang INTRUSIVE COMPLEX, as a one of the largest complexes in the southern part of the SANANDAJ-SIRJAN ZONE, is located at northwest of Jiroft, in KERMAN province. The complex mainly consists of acidic-intermediate rocks such as diorite, quartzdiorite, tonalite, granodiorite, and granite with subordinate amounts of mafic members such as hornblende gabbro and microgabbro. Field studies together with mineralogical and geochemical evidence show that the Khunrang INTRUSIVE COMPLEX belongs to calc-alkaline series and its felsic members are metaluminous to weakly peraluminous which display features typical of I-type granites. On the primitive mantle-normalized spider diagrams, all mafic and felsic samples are enriched in LILE (such as Rb, Cs and K) and depleted in Ti, Ta and Nb which is a main characteristic of subduction-related magmas. Based on geochemical data, the mafic rocks seems to be formed by melting of metasomatised mantle wedge; whereas felsic rocks are formed by melting of lower crust metabasic rocks as a result of the injection of mantle derived mafic magmas. It can be concluded that the Khunrang INTRUSIVE COMPLEX was formed in a VOLCANIC ARC setting due to subduction of the NEOTETHYS oceanic crust beneath the Central Iranian Micro-continent in the Middle-Jurassic time.

Cites

No record.

References

No record.

Cite

APA: Copy

SEDIGHIAN, S., DARGAHI, S., & ARVIN, M.. (2017). PETROGRAPHY, ORIGIN AND MAGMATIC EVOLUTION OF KHUNRANG INTRUSIVE COMPLEX, NORTHWEST OF JIROFT, KERMAN. GEOSCIENCES, 26(102), 207-220. SID. https://sid.ir/paper/31481/en

Vancouver: Copy

SEDIGHIAN S., DARGAHI S., ARVIN M.. PETROGRAPHY, ORIGIN AND MAGMATIC EVOLUTION OF KHUNRANG INTRUSIVE COMPLEX, NORTHWEST OF JIROFT, KERMAN. GEOSCIENCES[Internet]. 2017;26(102):207-220. Available from: https://sid.ir/paper/31481/en

IEEE: Copy

S. SEDIGHIAN, S. DARGAHI, and M. ARVIN, “PETROGRAPHY, ORIGIN AND MAGMATIC EVOLUTION OF KHUNRANG INTRUSIVE COMPLEX, NORTHWEST OF JIROFT, KERMAN,” GEOSCIENCES, vol. 26, no. 102, pp. 207–220, 2017, [Online]. Available: https://sid.ir/paper/31481/en

Related Journal Papers