MAGMATIC EVOLUTION IN QUATERNARY BASALTIC ROCKS IN GHORVEH – TAKAB AXIS

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MALAKOUTIAN S.; HAGHNAZAR SH.; GHORBANI MOSTAFA; EMAMI MOHAMMAD HASHEM

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Journal: GEOSCIENCES Year:2007 | Volume:16 | Issue:64 Page(s): 166-178

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Title

MAGMATIC EVOLUTION IN QUATERNARY BASALTIC ROCKS IN GHORVEH – TAKAB AXIS

Author(s)

MALAKOUTIAN S. | HAGHNAZAR SH. | GHORBANI MOSTAFA | EMAMI MOHAMMAD HASHEM | Issue Writer Certificate

Keywords

SR ISOTOPEQ2

ND ISOTOPEQ3

CRUSTAL CONTAMINATIONQ2

Abstract

Petrological,geochemical and isotropic evidence of CRUSTAL CONTAMINATION of the Quaternary basic rocks of Ghorveh-Takab axis is presented in this paper. These rocks are olivine basalt and basalt and they are plotted in the field of alkaline suites in geochemical diagrams.Some evidence, such as the presence of gneissic xenoliths, quartz xenocrysts with reaction rims and biotite phenoblasts in the basic rocks of the study area and high amount of potassium and high values of K2O/P2O5 ratios, high concentration of LREE in comparison with HREE, high values of 87Sr/86Sr ratios and low values of 143Nd/144Nd ratios all indicate the CRUSTAL CONTAMINATION of basic magma during its ascent.

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APA: Copy

MALAKOUTIAN, S., HAGHNAZAR, SH., GHORBANI, MOSTAFA, & EMAMI, MOHAMMAD HASHEM. (2007). MAGMATIC EVOLUTION IN QUATERNARY BASALTIC ROCKS IN GHORVEH – TAKAB AXIS. GEOSCIENCES, 16(64), 166-178. SID. https://sid.ir/paper/31856/en

Vancouver: Copy

MALAKOUTIAN S., HAGHNAZAR SH., GHORBANI MOSTAFA, EMAMI MOHAMMAD HASHEM. MAGMATIC EVOLUTION IN QUATERNARY BASALTIC ROCKS IN GHORVEH – TAKAB AXIS. GEOSCIENCES[Internet]. 2007;16(64):166-178. Available from: https://sid.ir/paper/31856/en

IEEE: Copy

S. MALAKOUTIAN, SH. HAGHNAZAR, MOSTAFA GHORBANI, and MOHAMMAD HASHEM EMAMI, “MAGMATIC EVOLUTION IN QUATERNARY BASALTIC ROCKS IN GHORVEH – TAKAB AXIS,” GEOSCIENCES, vol. 16, no. 64, pp. 166–178, 2007, [Online]. Available: https://sid.ir/paper/31856/en

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