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22619

GEOLOGY, PETROGRAPHY, GEOCHEMISTRY ANDSUITABILITY OF ABU SHEIH PEGMATITE FOR CERAMIC INDUSTRY

Article

Last updated: 03 Jan 2025

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Tags

Geology

Abstract

The geological, petrographical and geochemical studies as well as physical properties of Abu Sheih pegmatites and its effects on various types of fired ceramic bodies.The rock units in the study area are classified as follow: Wadi deposits (youngest), Post granitic dikes, pegmatite pockets and veins, syenogranites andgranodiorites (oldest).Thegranodiorites are light grey in colour and medium to coarse grained equigranular rocks, composed of plagioclases, quartz, perthites, hornblendebiotite, and muscovite as essential minerals. Zircon, iron oxides, apatite and titanite are accessory minerals whereas epidote as secondary minerals. But syenogranites show distinct pink to red colours. They are medium to coarse grained, hypidiomorphic, possessing subhedral to euhedral crystal faces, they are composed mainly of perthites, quartz, plagioclase, biotite and muscovite as essential minerals, while zircon, titanite, iron oxides and apatite are the accessory minerals. Epidote and chlorite are present as secondary minerals.The geochemical studies revealed that, the studied Granodiorites were originated from metaluminouscalc-alkaline magma intruded in a crust of a thickness less than 30 km at water pressure less than 2 kb. They could be considered as volcanic arc or continental arc granitoides. The Syenogranites were derived from sialic crust and considered as I-type granites, that originated from peraluminous, calc-alkaline, highly fractionated magma. They could be considered as late orogenic granites, intruded in a crust ranging in thickness from 20 km to 30 km.
Pegmatites are relatively enriched in Al2O3and K2O than their granitic host. This is consistent with the mineral composition of pegmatites where they are more enriched in K-feldspar and quartz. Also the depletion of Sr in pegmatites than their granite host is related to less abundant plagioclase in pegmatites.The geochemical studies revealed thatthe studied pegmatite samples classified as granite,subalkaline nature field, intruded in a crust ranging in thickness from 20 to 30 km.

DOI

10.21608/absb.2015.22619

Keywords

Granodiorites, Syenogranites, Pegmatites, Ceramic Industry

Authors

First Name

AHMED

Last Name

EL-MEZAIN

MiddleName

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Affiliation

Al-Azhar University

Email

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City

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Orcid

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First Name

SAYEDAHMED

Last Name

MOHAMED OMAR

MiddleName

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Affiliation

nuclear Materials Authority

Email

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City

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Orcid

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First Name

MOHEY EL-DIENABD

Last Name

EL-HAMED

MiddleName

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Affiliation

Ceramica Cleopatra Company

Email

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City

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Orcid

-

First Name

ABD EL-FATTAHABD

Last Name

EL-MONEEMKABEL

MiddleName

-

Affiliation

Ceramica Cleopatra Company

Email

-

City

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Orcid

-

Volume

26

Article Issue

Issue 1-D

Related Issue

4292

Issue Date

2015-06-01

Receive Date

2018-02-04

Publish Date

2015-06-01

Page Start

91

Page End

108

Print ISSN

1110-2535

Online ISSN

2636-3305

Link

https://absb.journals.ekb.eg/article_22619.html

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https://absb.journals.ekb.eg/service?article_code=22619

Order

7

Type

Original Article

Type Code

520

Publication Type

Journal

Publication Title

Al-Azhar Bulletin of Science

Publication Link

https://absb.journals.ekb.eg/

MainTitle

GEOLOGY, PETROGRAPHY, GEOCHEMISTRY ANDSUITABILITY OF ABU SHEIH PEGMATITE FOR CERAMIC INDUSTRY

Details

Type

Article

Created At

22 Jan 2023