SIAH-CHESHMEH OPHIOLITE, NW OF KHOY

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POORMOHSEN M.; RAHGOSHAY M.; AZADI I.; SHAFAII MOGHADAM H.

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Journal: GEOSCIENCES Year:2010 | Volume:20 | Issue:77 Page(s): 131-138

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Information Journal Paper

Title

SIAH-CHESHMEH OPHIOLITE, NW OF KHOY

Author(s)

POORMOHSEN M. | RAHGOSHAY M. | AZADI I. | SHAFAII MOGHADAM H. | Issue Writer Certificate

Keywords

SIAH-CHESHMEH OPHIOLITEQ3

ALKALINE BASALTSQ3

CALC-ALKALINE BASALTSQ3

MANTLE PLUMEQ3

SUBDUCTION ZONEQ2

Abstract

The SIAH-CHESHMEH OPHIOLITEs at the north-northwest part of the Khoy ophiolites show a dismembered pile of metamorphic units, mantle sequence, and basaltic-andesitic lavas associated with Late Cretaceous pelagic limestones and cherts. The basaltic-andesitic lavas can be divided into alkaline and calc-alkaline varieties. The presence of Ti-rich amphibole prisms and Ti-bearing clinopyroxenes is characteristic of these lavas. The calc-alkaline lavas are characterized by enrichment in LREE and depletion in HFSE while the alkaline lavas display positive LREE and HFSE anomalies. The interaction between MANTLE PLUMEs with a spreading center can be considered for generation of ALKALINE BASALTS while a SUBDUCTION ZONE is responsible for the genesis of CALC-ALKALINE BASALTS.

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APA: Copy

POORMOHSEN, M., RAHGOSHAY, M., AZADI, I., & SHAFAII MOGHADAM, H.. (2010). SIAH-CHESHMEH OPHIOLITE, NW OF KHOY. GEOSCIENCES, 20(77), 131-138. SID. https://sid.ir/paper/32306/en

Vancouver: Copy

POORMOHSEN M., RAHGOSHAY M., AZADI I., SHAFAII MOGHADAM H.. SIAH-CHESHMEH OPHIOLITE, NW OF KHOY. GEOSCIENCES[Internet]. 2010;20(77):131-138. Available from: https://sid.ir/paper/32306/en

IEEE: Copy

M. POORMOHSEN, M. RAHGOSHAY, I. AZADI, and H. SHAFAII MOGHADAM, “SIAH-CHESHMEH OPHIOLITE, NW OF KHOY,” GEOSCIENCES, vol. 20, no. 77, pp. 131–138, 2010, [Online]. Available: https://sid.ir/paper/32306/en

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