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139228

Re-Mapping the Neoproterozoic Basement Rocks of Um Gheig area, Central Eastern Desert, Egypt based on Remote Sensing, Petrography and Field Investigation

Article

Last updated: 23 Jan 2023

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Abstract

Landsat 8 (OLI) ETM+ satellite imagery data are evaluated for
improving and re-mapping the geologic map of Um Gheig area, Central
Eastern Desert of Egypt. Different remote sensing techniques including
FCC, band ratio, PCA, supervised classification and spectral
characteristic analysis were applied on satellite imagery to facilitate the
discrimination of the widely exposed Neoproterozoic basement rocks in
the study area. Best color composite 146 FCC, 762 FCC, band ratio 6/2,
4/3, 7/3 and 7/6, 6/5, 4/2 in RGB, as well as PCA 213 and 314 in RGB
were selected and used for detailed mapping of the different lithological
units. Spectral characteristic analysis was used to discriminate the rock
forming minerals through the different rock units in Umm Gheig area
(e.g. amphibole b7/b5, serpentine b5/b7, Quartz b7/b6, muscovite b6/b4
and PCA4). The rock units of Um Gheig area are divided four main
lithological units according to field and petrographical studies; ophiolitic
associations, foliated metavolcanics, post-granitoids and hammamat
sediments, as well as small parts of unmapple metavolcanics and
metgabbro. Ophiolitic associations are subdivided serpentinites,
metagabbro, volcanoclastic metasediments and hormblende schist.
Granitoids are subdivided El-Deilihimmi granite and Abu Shaddad
granite. Petrographically, serpentinites prevailing by antigurite
serpentinites, metagabrro includes quartz and hornblende gabbro, VCM
comprised different varieties range from biotite schist, biotite
hornblende schist, garnet biotite hornblende schist, intercalations of
actionolite schist and highly mylonitic schist, foliated metavolcanics
represented by schistose metatuffs and mylonitic schist, metavolcanics
represented by meta-andesite and fine metatuff, El-Deilihimmi granite
includes granodiorite and monzogranite while Abu shaddad granite
comprised alkali feldspar granite and syenogranite, hammamat
sediments represented by pebbles of dacite. A new modified geological
map is produced for Um Gheig area based on the remote sensing data,
field investigation and petrographical description.

DOI

10.21608/djs.2020.139228

Keywords

Um Gheig, Landsat8(OLI), CED, BasementRocks

Authors

First Name

Mohamed A.

Last Name

Abd El-Wahed

MiddleName

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Affiliation

Geology Department, Faculty of Science, Tanta University, 31527 Tanta, Egypt

Email

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City

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Orcid

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First Name

El Metwaly

Last Name

Lebda

MiddleName

-

Affiliation

Geology Department, Faculty of Science, Kafrelsheikh University, Kafrelsheikh, Egypt

Email

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City

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Orcid

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First Name

Samir

Last Name

Kamh

MiddleName

-

Affiliation

Geology Department, Faculty of Science, Tanta University, 31527 Tanta, Egypt

Email

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City

-

Orcid

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First Name

Mohamed

Last Name

Attia

MiddleName

-

Affiliation

Geology Department, Faculty of Science, Kafrelsheikh University, Kafrelsheikh, Egypt

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City

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Orcid

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Volume

41

Article Issue

1

Related Issue

20615

Issue Date

2019-06-01

Receive Date

2021-01-13

Publish Date

2019-06-01

Page Start

39

Page End

54

Print ISSN

1012-5965

Online ISSN

2735-5306

Link

https://djs.journals.ekb.eg/article_139228.html

Detail API

https://djs.journals.ekb.eg/service?article_code=139228

Order

5

Type

Research and Reference

Type Code

1,686

Publication Type

Journal

Publication Title

Delta Journal of Science

Publication Link

https://djs.journals.ekb.eg/

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Article

Created At

23 Jan 2023