GEOCHEMISTRY AND PETROGENESIS OF BASALTIC FLOWS IN THE NAIN-DEHSHIR OPHIOLITES

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SHAFAEI MOGHADAM H.; RAHGOSHAI MOHAMMAD; BANITABA A.

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Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2009 | Volume:16 | Issue:4 Page(s): 602-611

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Information Journal Paper

Title

GEOCHEMISTRY AND PETROGENESIS OF BASALTIC FLOWS IN THE NAIN-DEHSHIR OPHIOLITES

Author(s)

SHAFAEI MOGHADAM H. | RAHGOSHAI MOHAMMAD | BANITABA A. | Issue Writer Certificate

Keywords

BASALTSQ3

DIABASESQ3

FLAT REE PATTERNQ3

HFSE DEPLETIONQ3

BACK-ARC BASINQ2

Abstract

Diabases, pillow lavas and basaltic flows in the Nain-Dehshir ophiolites are marked with flat to slightly depleted pattern in REE chondrite-normalized diagram and are characterized by depletion in HFSE and enrichment in LILE. This geochemical behavior can be considered for lavas erupted in arc-related environments. Clinopyroxene in these rocks shows low content of TiO2 and resemble those found in island-arc tholeiites. These characteristics are consistent with back-arc formation during middle to upper Cretaceous, due to the oblique subduction of Neotethyan Ocean along the active continental margin of the central Iranian block.

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APA: Copy

SHAFAEI MOGHADAM, H., RAHGOSHAI, MOHAMMAD, & BANITABA, A.. (2009). GEOCHEMISTRY AND PETROGENESIS OF BASALTIC FLOWS IN THE NAIN-DEHSHIR OPHIOLITES. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 16(4), 602-611. SID. https://sid.ir/paper/3887/en

Vancouver: Copy

SHAFAEI MOGHADAM H., RAHGOSHAI MOHAMMAD, BANITABA A.. GEOCHEMISTRY AND PETROGENESIS OF BASALTIC FLOWS IN THE NAIN-DEHSHIR OPHIOLITES. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2009;16(4):602-611. Available from: https://sid.ir/paper/3887/en

IEEE: Copy

H. SHAFAEI MOGHADAM, MOHAMMAD RAHGOSHAI, and A. BANITABA, “GEOCHEMISTRY AND PETROGENESIS OF BASALTIC FLOWS IN THE NAIN-DEHSHIR OPHIOLITES,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 16, no. 4, pp. 602–611, 2009, [Online]. Available: https://sid.ir/paper/3887/en

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