GEOCHEMISTRY AND ERUPTIVE ENVIRONMENT OF THE MAFIC ROCK SERIES IN THE BALVARD-BAFT OPHIOLITES

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.

SHAFAEI MOGHADAM H.; RAHGOSHAI MOHAMMAD; WHITECHURCH H.; MONSEF I.; SOLTAN MOHAMMADI A.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2009 | Volume:18 | Issue:72 Page(s): 155-160

Download Full-Text

Persian Verion

View:

834

Download:

Cites:

Information Journal Paper

Title

GEOCHEMISTRY AND ERUPTIVE ENVIRONMENT OF THE MAFIC ROCK SERIES IN THE BALVARD-BAFT OPHIOLITES

Author(s)

Keywords

ISLAND-ARC THOLEIITESQ3

CALC-ALKALINE AFFINITYQ3

MIDDLE CRETACEOUSQ2

BACK-ARC BASINQ3

Abstract

Basalts, gabbros, tuffs, diabasic dikes, agglomerates and breccias and the rock fragments of breccias are the main mafic constituents of the Balvard-Baft ophiolites. Geochemical signatures of these rocks reveal depletion in HFSE and enrichment in LILE and simultaneous occurrence of island-arc tholeiitic and calc-alkalic volcanisms. These geochemical behaviors are the evidences suggesting that these mafic rocks are of supra-subduction zone affinity. These special signatures associated with the position of the Nain-Baft ophiolitic belt behind the Mesozoic magmatic arc of the Sanandaj-Sirjan zone, suggest back-arc spreading (in the active margin of the Central Iranian block), during MIDDLE CRETACEOUS due to the oblique subduction of Neo-Tethys beneath the Central Iranian block.

Cites

No record.

References

No record.

Cite

APA: Copy

SHAFAEI MOGHADAM, H., RAHGOSHAI, MOHAMMAD, WHITECHURCH, H., MONSEF, I., & SOLTAN MOHAMMADI, A.. (2009). GEOCHEMISTRY AND ERUPTIVE ENVIRONMENT OF THE MAFIC ROCK SERIES IN THE BALVARD-BAFT OPHIOLITES. GEOSCIENCES, 18(72), 155-160. SID. https://sid.ir/paper/32318/en

Vancouver: Copy

SHAFAEI MOGHADAM H., RAHGOSHAI MOHAMMAD, WHITECHURCH H., MONSEF I., SOLTAN MOHAMMADI A.. GEOCHEMISTRY AND ERUPTIVE ENVIRONMENT OF THE MAFIC ROCK SERIES IN THE BALVARD-BAFT OPHIOLITES. GEOSCIENCES[Internet]. 2009;18(72):155-160. Available from: https://sid.ir/paper/32318/en

IEEE: Copy

H. SHAFAEI MOGHADAM, MOHAMMAD RAHGOSHAI, H. WHITECHURCH, I. MONSEF, and A. SOLTAN MOHAMMADI, “GEOCHEMISTRY AND ERUPTIVE ENVIRONMENT OF THE MAFIC ROCK SERIES IN THE BALVARD-BAFT OPHIOLITES,” GEOSCIENCES, vol. 18, no. 72, pp. 155–160, 2009, [Online]. Available: https://sid.ir/paper/32318/en

Related Journal Papers