GEOCHEMISTRY AND GENESIS OF INDUSTRIAL SOILS OF BID-AKHAVID FELDSPAR DEPOSIT (DEHSHIR FAULT ZONE), USING RARE EARTH ELEMENTS AND STABLE ISOTOPIC DATA

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TAGHIPOUR BATOUL; ETEMADI BIJAN; MACKIZADEH MOHAMMAD ALI; MAHDAVI AMIR

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Journal: GEOCHEMISTRY Year:2013 | Volume:1 | Issue:3 Page(s): 227-237

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Title

GEOCHEMISTRY AND GENESIS OF INDUSTRIAL SOILS OF BID-AKHAVID FELDSPAR DEPOSIT (DEHSHIR FAULT ZONE), USING RARE EARTH ELEMENTS AND STABLE ISOTOPIC DATA

Author(s)

TAGHIPOUR BATOUL | ETEMADI BIJAN | MACKIZADEH MOHAMMAD ALI | MAHDAVI AMIR | Issue Writer Certificate

Keywords

BID-AKHAVIDQ2

SHIR-KUH GRANITEQ2

FELDSPAR MINEQ2

INDUSTRIAL SOILQ2

TRACE AND REE ELEMENTSQ2

Abstract

dakhavid feldspar deposit soil is located at 70 km southwest of Yazd city. From the geological point of view, the area is a part of Central Iranian zone located in Urumieh-Dokhtar volcanic belt. The deposit is formed as Quaternary alluvial sands in the fault contact zone of SHIR-KUH GRANITE with Jamal Formation carbonates (Permian). This fault zone in now active and there are emanations of sulfur-bearing gases (fumarole) in parts of area. The succession of arens and loosely-consolidated sandstones are predominate lithology in the mining quarry. According to petrographic studies on unconsolidated sediments, the granitic composition of grains is determined. These sediments could be considered as litharenite and arkose according to the Folk classification. The following main mineral composition deduced from XRD analysis: Quartz + albite + muscovite + illite + orthoclase + jarosite + Poor sorting and roundness of grain components indicate that the host rocks of these terrigenous clastic sediments are near the deposit. According to field evidence, petrographic and comparative mineralogical studies of samples with Shirkuh granite, it is obvious that batholith has an important role as the source materials for Bidakhavid deposit. The sediments are of economic value and are known as INDUSTRIAL SOIL in mining literature. The deposit is formed in the subduction zone tectonic setting. REE normalized pattern in all samples is indicative of the intense enrichment of LREE and depletion of HREE. This pattern shows that Shir-kuh granitic rocks are the source of BID-AKHAVID sediments.d18 O and dD values of the BID-AKHAVID sediments range (-3.34‰ to -7.6‰) and (-48.34‰ to -75.4 ‰) respectively. These data indicate that connate water played essential role in the alteration of intrusive protolith and formation of the sediments.

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APA: Copy

TAGHIPOUR, BATOUL, ETEMADI, BIJAN, MACKIZADEH, MOHAMMAD ALI, & MAHDAVI, AMIR. (2013). GEOCHEMISTRY AND GENESIS OF INDUSTRIAL SOILS OF BID-AKHAVID FELDSPAR DEPOSIT (DEHSHIR FAULT ZONE), USING RARE EARTH ELEMENTS AND STABLE ISOTOPIC DATA. GEOCHEMISTRY, 1(3), 227-237. SID. https://sid.ir/paper/230863/en

Vancouver: Copy

TAGHIPOUR BATOUL, ETEMADI BIJAN, MACKIZADEH MOHAMMAD ALI, MAHDAVI AMIR. GEOCHEMISTRY AND GENESIS OF INDUSTRIAL SOILS OF BID-AKHAVID FELDSPAR DEPOSIT (DEHSHIR FAULT ZONE), USING RARE EARTH ELEMENTS AND STABLE ISOTOPIC DATA. GEOCHEMISTRY[Internet]. 2013;1(3):227-237. Available from: https://sid.ir/paper/230863/en

IEEE: Copy

BATOUL TAGHIPOUR, BIJAN ETEMADI, MOHAMMAD ALI MACKIZADEH, and AMIR MAHDAVI, “GEOCHEMISTRY AND GENESIS OF INDUSTRIAL SOILS OF BID-AKHAVID FELDSPAR DEPOSIT (DEHSHIR FAULT ZONE), USING RARE EARTH ELEMENTS AND STABLE ISOTOPIC DATA,” GEOCHEMISTRY, vol. 1, no. 3, pp. 227–237, 2013, [Online]. Available: https://sid.ir/paper/230863/en

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