The Gabal (G.) El-Niteishat area lies in the Central Eastern Desert of Egypt which is known for various mineral resources and geological structures. Umm Gheig, Umm Naggat, Umm Shaddad, Wadi (W.) Zeidun and Sigdit represent some important regions that contain mineral deposits in the study area. Various filters such as first vertical derivative (FVD), horizontal gradient magnitude (HGM), tilt derivative (TDR) and near-surface were applied to the airborne magnetic data for the study area to deduce the structural lineaments and magnetic source edges which were controlled by the presence of mineral deposits. Processed Landsat ETM+ images are used for delineating the rock unit boundaries that are exposed in the study area such as serpentinite, metagabbro, metavolcanics and metasediments. Also, band ratios, principal component analysis (PCA) and false-color composite image (Crosta alteration image) were applied to get specific results about the alteration zones. The structural lineaments analysis illustrated that the common trends that affected the study area were NW-SE, NE-SW, E-W and N-S. Integration of remote sensing and airborne magnetic data exhibited the relation between mineralization and structural lineaments.
Remote Sensing Airborne Magnetic Mineral Exploration Umm Naggat-Umm Gheig Central Eastern Desert of Egypt1. Introduction
The study area lies in the Central Eastern Desert of Egypt, between latitudes 25˚22' and 25˚42'N and longitudes 33˚53' and 34˚27'E (Figure 1). The study area reveals a special importance, as it comprises rock units, which show some indication of the presence of various mineralization (Au, Cr, Ta, Nb, Sn, Pb, Zn, Cu, Fe and others) as detected by the previous geological, geochemical and geophysical studies.
Ghieth (1995 and 1998), studied G. El Sebai and G. Abu Iteila areas using airborne spectrometric and magnetic data. He concluded that the WNW-ESE, NW-SE, NNW-SSE, N-S, NE-SW and ENE-WSW faults represented the major structures. Also, the study revealed the enrichment of uranium and thorium were related to the occurrence of Nb, Ta and Sn minerals, especially at the contact of granitic pluton in G. Atawi [1] [2].
Gaafar (2015), studied Umm Naggat area, he found that four regional structural trends NNW-SSE, NW-SE, ENE-WSW and E-W played the main important role in Nb, Ta [3], U mineralization. Alteration processes are associated with NW-SE and N-S trends in Umm Naggat [4].
Aboelkhair et al. (2014 and 2020) studied Kadabora granite through the integration of airborne spectrometric data remote sensing data. The study concluded that the concentrations of uranium mineralization were controlled by faults trending in the N-S direction [5] [6].
Mineral exploration depends on a complete integration of works, where it starts from searching for new mineral deposits then evaluates the economic importance. It also includes the augmentation of additional ore reserves and resources in the mine and total mining district [7]. Geophysical survey supplements the quick and cost-effective paths to identify the subsurface objects and prioritizing the drill targets [7].
Magnetic method can be useful in detecting magnetic anomalies which may represent ore. Also, it is used in different applications such as locating faults, folds, shear zones, contact and determining geological structures that may play a role in mineral exploration [8] [9] [10] [11].
Multi-resource geospatial data such as geophysical and geochemical information and analysis of satellite images were applied for lithological and mineral mapping, exploiting the development of remote sensing that provided the type of minerals of the different rock units [12] [13].
The current study aims to exploit remote sensing and airborne magnetic data to determine alteration zones of mineralization and structural lineaments that may have a role in the mineral exploration in the study area.
2. Geologic Setting
The geologic setting of the study area is mainly based on the geology of Hamata, Egypt of scale 1:500,000 (Conoco Coral and EGPC, 1987) [14] and metallogenic map of Aswan quadrangle, Egypt [15] (Figure 1). The exposed rock units in this area are mostly serpentinite, metagabbro, metavolcanics, metasediments, Hammamat clastics, gabbroic, older granites, younger granites, Post-Hammamat felsite, trachyte plugs and sheets (Figure 1). The outcrops of the different rock units are traversed by many valleys filled with Quaternary sediments. A digital elevation model (DEM) map was used for representing the different elevations in the study area (Figure 2).
The study area is characterized by groups of geological structures related in the concentration deposit mineralizations as gold (Au), chromium (Cr), lead (Pb), zinc (Zn), iron (Fe), copper (Cu) and many other economic minerals. Some of the most important regions in this area, which must be studied carefully because they contain gatherings of economic ore deposits are Umm Gheig, Umm Naggat, Umm Shaddad, Wadi (W.) Sitra, W. Zeidun, Sigdit and Umm Ghamis and many other important regions [3] [16] [17] [18] [19].
The study area includes many minor structural features associated with ore deposits and mineralization, these minor structures are related to the major structures in the area such as the Arabian Nubian Shield (ANS) and Najd faults zone. Hamimi et al. (2015b) concluded that the rifting of the Red Sea from
Oligocene and younger times led to uplifting and exhibition of the Neoproterozoic ANS. In the Central Eastern Desert, the fold-related faults are common and associated with pull-apart connected to the Najd system [20].
The Central Eastern Desert (CED) is the most known for its low topography, good roads and mineral resources. The CED consists mainly of Late Tonian-Cryo-genian superstructures (~700 - 750 Ma). Particular attention is paid to the sub-horizontal shear zone so-called the Eastern Desert Decollement (EDD), which was active during Najd strike-slip deformation (~600 Ma). Fluid infiltration accompanying superstructure deformation and infrastructure magmatism were responsible for generating most of ED gold deposits [21].
3. Data Acquisition and Methodology
Airborne magnetic data of the area under study was included in the segment of area II, which was measured by Aero-Service Division, Western Geophysical Company of America (1984). This survey was conducted over Sothern, Central and Northern Eastern Desert of Egypt to recognize and estimate the groundwater, mineral, petroleum resources (Aero-Service, 1984). The flight lines oriented in northeast-southwest direction, with spacing 1 km and azimuth of 45˚ and 225˚ from the north. The Tie lines were oriented in a northwest-southeast direction, with the azimuth of 135˚ and 315˚, and spacing of 10 km [22].
The airborne magnetic survey data of the study area were subjected to various methods of processing and analysis through the application of some integrated magnetic techniques to map the structural lineaments as evidence for mineral exploration, these techniques include first vertical derivative (FVD), horizontal gradient magnitude (HGM), tilt derivative (TDR) and near-surface. These techniques are considered good tools to delineate near-surface magnetic lineament features such as shear zones, contacts, dykes and faults, which may associate with mineral deposits.
· The algorithm of the vertical derivative is given by [23] as follows:
M ( x , y ) = M ( x , y ) ( ( x 2 + y 2 ) / n ) n (1)
where n is the order of the derivative.
· The horizontal gradient magnitude HGM(x, y) for the magnetic field M(x, y) is given by [24] [25].
HGM ( x , y ) = ( ∂ M / ∂ x ) 2 + ( ∂ M / ∂ y ) 2 (2)
· The tilt derivative (TDR) technique was described by [26],
T D R = t a n − 1 ( V D R H G M ) (3)
where the vertical derivative is VDR and total horizontal derivatives are HGM.
The main objectives for using the remote sensing images Landsat Enhanced Thematic Mapper (ETM+) are mapping the rock units and to identify the alteration zones in the study area. The Envi and Arc GIS software packages are used to enhance and analyze these data.
4. Results and Discussions4.1. Interpretation of Airborne Magnetic Data
The reduced to north magnetic pole (RTP) map (Figure 3) is characterized in general by magnetic values ranging from 41,930 nT to 43,625 nT. It displays three zones of magnetic anomalies (high, intermediate and low). High magnetic anomalies are located at the eastern, western, northern and southern parts of the study area. These anomalies have circular or semi-circular, linear and elongated shapes (Figure 3). The circular or semi-circular high magnetic anomalies are located at the western part (south W. Zeidun, at G. El-Gindi and southwest G. El-Hidilawie) and also observed at the eastern part (south G. Kadabora and north G. Umm Lasaf). While, the linear and elongated shape high magnetic anomalies are spread out over the study area and follow NW-SE, NNW-SSE, NE-SW and E-W directions (Figure 3). The high magnetic anomalies are related to surface or subsurface intrusions of basic rocks as serpentinite and metagabbro.
Intermediate magnetic anomalies (yellow to green colour) appeared all over the investigated area (Figure 3). The surface geology refers to that these anomalies are related to metasediments, metavolcanics, post-Hammamat felsite and granite.
Low magnetic anomalies (light and dark blue colour) are ellipsoid and elongated shapes. These anomalies occurred at the southern, east-central, northern and northeastern parts of the study area (Figure 3). They are belonging to metavolcanics, metasediments, post-Hammamat felsite and some parts of granitic rocks.
4.1.1. Radially Averaged Power Spectrum
A separation filter was applied on the RTP airborne magnetic map where the regional and residual magnetic-component maps are obtained at 0.12 cycle/K-unit. The estimated average depths for the shallow and deep magnetic sources as calculated from the power spectrum curve are 700 m and 1800 m respectively (Figure 4).
4.1.2. Residual and Regional Airborne Magnetic Maps
The high pass (residual) magnetic map of the study area shows high (positive) and low (negative) magnetic features (Figure 5). These features have different sizes, amplitudes, and frequencies with pattern trends taking NW-SW, NE-SW and NNE-SSW directions. A good correlation was found between RTP and residual maps (Figure 4 and Figure 5), which reflects that most of the magnetic source bodies are situated on the surface and/or at shallow depths. The locations of the high magnetic features in the residual map agree well with the effect of these features on the RTP map.
The low pass (regional) magnetic map (Figure 6) displays high and low magnetic features with different sizes, amplitudes and directions. The high magnetic features are recorded at the eastern, western and southern parts of the study area. Meanwhile, low magnetic features are situated in the central, southern and northeastern parts. The locations of the high magnetic features on the regional magnetic map agree well with their locations on RTP and residual maps, which suggest that the causative magnetic bodies of these features have shallow depths with deep roots (Figure 6).
4.1.3. First Vertical Derivative (FVD) Map
The first vertical derivative filter was applied for the reduced to the north magnetic pole (RTP) data to enhancement the near-surface lineament features such as shear zones, contacts, dykes and faults. The first vertical derivative map (Figure 7) shows gradient values varying between −1.057 nT/m and 2.040 nT/m. Three levels of the gradient are displayed as high positive values (pink), intermediate (green) and low negative values (blue). This map displays many semi-circular and linear magnetic features.
Three semi-circular features with high magnitude are observed at the western part of the area, that lie south W. Zeidun, southwest G. El-Hidilawie and G. El-Gindi (Figure 7). These features may be related to basic rocks (serpentinites). Also, these features appeared to be structurally controlled.
An intermediate semi-circular feature occurs in the study area between G. Kadabora and G. Umm Lasaf at the eastern part (Figure 7), which is corresponding geologically to calc-alkaline granite at the surface. The contact of this feature with other rocks is clearly defined.
A linear magnetic feature with narrow width and NNW-SSE direction occurs at the western part of the study area (Figure 7). It may represent a buried basic dyke. Other high positive values occur at northern, eastern, southern and central parts of the study area, they are related to surface and subsurface basic rocks. These high positive values take different trends such as NW-SE, NE-SW, E-W and N-S.
Structural features like contacts, faults and shear zones can be deduced from the first vertical derivative map (Figure 7). Therefore, this technique is useful for extracting the structural lineman features.
4.1.4. Horizontal Gradient Magnitude (HGM) Map
Horizontal gradient magnitude map (Figure 8) displays high gradient values (pink) with amplitude peak of 1.167 nT/m, which may represent the magnetic features. The high values have variable amplitudes and shapes. The main trends of these values are NW-SE, NNW-SSE, NE-SW and E-W.
Semi-circular and ellipsoidal anomalies with high amplitude are located at south W. Zeidun, southwest G. El-Hidilawie, G. El-Gindi, G. Umm Lasaf and south G. Kadabora (Figure 8). They may due to outcrops and/or subsurface magnetic structures. Also, these anomalies can be classified as structurally controlled by faults.
A semi-circular anomaly is found at the eastern part of the map, along the area between G. Kadabora and G. Umm Lasaf. This anomaly is bounded by high amplitude gradient values, which are corresponding to faults and contacts (Figure 8).
Linear high amplitude gradient anomalies are observed on the HGM map (Figure 8). These anomalies are related to different structural and lithological features such as shear zones, faults and dykes located at the surface and subsurface in the study area.
4.1.5. Tilt Derivative (TDR) Map
Tilt derivative (TDR) filter is used for delineating the geologic structures, which may be linked to shallow structural lineaments and/or mineral exploration (Figure 9). This is because of the TDR concern on the detection of horizontal edges of the magnetic bodies or structures. The zero-contour line shows the horizontal location of the lateral change in magnetic susceptibility between positive and negative magnetic bodies (Figure 9).
4.1.6. Near Surface Map
The residual map at level of 100 m (Figure 10) is constructed by subtracting the upward continuation map of 100 m from the RTP map. This map is useful in the emphasizing of magnetic source bodies and structural lineaments (Finn and Horton, 2015). This map is exploited to highlights the near-surface structural lineaments of the study area. It shows high similarity with the first vertical derivative map and confirms the same results.
4.2. Interpretation of Remote Sensing Data
The interpretation of spectral data for detecting the target from different satellite sensors as Landsat Thematic Mapper (TM), Enhanced Thematic Mapper (ETM+) and ASTER imagery was applied. Integration of different images ASTER, and Landsat ETM) were used for mapping the mineral characters zones [27] [28].
One scene of Landsat-7 covering the selected area (p174) was used (30 m resolution). False-color composite image of band combination 7, 4, 2 in red (R), green (G) and blue (B) is used for representing the rock unit boundaries in the selected area. This combination shows the variation of felsic, mafic and wadi deposits. Felsic rocks reflect a reddish-brown to dark red color, the mafic rocks are dark and the wadi deposits are bright color (Figure 11).
For detecting the mineralization zones, band ratio is almost applied to represent the spectral characters of the alteration zones due to absorbing bands of their altered minerals. Applying of the enhanced satellite images of Landsat-7, the iron-bearing (ferrous and ferric oxides) minerals are detecting from applying band ratios 3/5, 5/4 and 3/1 [29] [30]. Moreover, the band ratio of 5/7 was used to pick up the high values of the hydroxyl-bearing minerals (epidotes, chlorites, kaolinite and muscovite) (e.g., [31] ). In the current study, the band ratio 5/4 was used for detecting the alteration zone of ferrous and ferric minerals in the study area as shown in Figure 12 in which these alteration areas are represented by the very clear white color surrounded by the grey color. For detecting the Alteration zone of the hydroxyl (OH)-bearing minerals, the band ratio 5/7 is used, as shown in Figure 13.
Another band ratio has been applied for representing the final alteration zone in the study area, this band ration displayed the OH-bearing menials (5/7 ratio) in R, the Fe-bearing menials (5/4 ratio) in B and OH + F (5/7 + 5/4) in G (Figure 14). The final image shows the alteration zones of ferric, ferrous and OH-bearing minerals, which appear in very light pink color (Figure 15). The clay minerals content in the sedimentary rocks and wadi deposits, both represented by the dark green color (Figure 15).
In addition to band ratios, principal component analysis (PCA) was applied to get specific results about the alteration zones. PCA is an important technique that provided simple information on multispectral datasets. This method was used to reduce the abundance of information between the different bands ( [32] [33] ). Crosta and Moore (1989) represented the advantage of oriented principal components selection, that used for evaluation of PCA to determine which of the principal component images allowed concentrating data immediately concerning with the theoretical spectral signatures of certain objectives [34]. Loughlin (1991) deduced that the analysis of these images showed the target zones in bright or dark pixels [32]. Based on the experiment results, the iron-bearing minerals and OH-bearing minerals showed absorption features in specific bands rather than another. This technique requires no atmospheric correction or detail information of the spectral characters of specific targets. It is an efficient tool for describing alteration zones from the obtained data.
Using the PCA method, the hydroxide minerals, ferric and ferrous minerals can be delineated from the selected bands with their principal components. For detecting the alteration zones of hydroxide minerals, the bands of 1, 4, 5, 7 were selected using PCA (Table 1) and iron-bearing minerals, bands 1, 3, 4, 5 (Table 2). To get good contrast for the alteration areas, suitable eigenvectors from different bands were selected.
False-color composite image (Crosta alteration image) was constructed after utilizing the OH-bearing minerals (H-image) in Red (Figure 13), the iron-bearing oxides (F-image) in Blue (Figure 12) and the H + F image in green (Figure 14). This map is used to delineate the alteration zones and detect the richer zones of the iron oxides and OH-bearing minerals. The alteration areas resulting from this technique can be shown in Figure 16. The Alteration zone of the iron bearing minerals and hydroxide-bearing minerals richer zones appear by brown color.
From the two Figure 12 and Figure 13, the alteration zones of the iron-bearing menials and the Hydroxides-bearing menials were represented by brown color in the Crosta image (Figure 16) and represented by very light pink color in the final alteration zone image (Figure 15) at exactly in the same locations in the study area. There is a good correlation between the two images about the locations of the alteration area in the study area.
The iron-bearing oxides and the OH-bearing minerals are commonly accompanied by ore economic deposits such as Au, Pb, Fe, Cr, Cu and many other economic minerals. So, using the analysis of the satellite image and applying some method of the enhancements of these images help to delineate the location of the ore deposits minerals in the study area.
PCA of the selected bands 1, 4, 5, and 7 of Landsat-7
Eigen vector
Band 1
Band 4
Band 5
Band 7
Eigen %
PC1
0.431
0.522
0.523
0.517
89.67
PC2
0.840
0.065
−0.373
−0.389
7.75
PC3
0.328
−0.844
0.200
0.375
1.88
PC4
−0.029
0.108
−0.740
0.664
0.70
PCA of the selected bands 1, 3, 4, and 5 of Landsat-7
Eigen vector
Band 1
Band 3
Band 4
Band 5
Eigen %
PC1
0.446
0.522
0.525
0.504
91.33
PC2
0.790
0.049
−0.153
−0.591
6.38
PC3
0.400
−0.442
−0.502
0.627
2.11
PC4
0.130
−0.728
0.670
−0.060
0.18
4.3. Structural Lineaments Analysis
Structural lineament analysis has an important role in mineral exploration where most of the mineral deposits are controlled by structures directly or indirectly. To study structural lineaments of the study area; surface, shallow and deep lineament structures were deduced from the geologic, remote sensing, RTP, near-surface, residual and regional maps. These lineaments were presented as rose diagrams (Figure 17).
The rose diagrams of surface lineament structures (Figure 17(a) and Figure 17(b)) illustrate that the common trends are NW-SE, NE-SW, E-W and N-S. These trends also appeared in the rose diagrams of the shallow and deep lineament structures (Figures 17(c)-(e) and Figure 17(f)). This confirms that these trends extended from the surface to deep depths.
The E-W trend is observed at the rose diagram of the regional map (Figure 17(f)) as a dominant structure which suggests that this trend is considered as the deepest structure in the study area. According to Meshref (1990), the NW-SE, NE-SW trends represent the favorable structures for mineral Exploration.
4.4. Data Results Integration
Through the results that are obtained from airborne magnetic and remote sensing data, it can be inferred the following:
1) The analysis of remote sensing data displays the alteration zones as red circles (Figure 18). These zones show the locations of concentrations of mineral deposits in the study area. Figure 18 shows that the known mineralization sites previously recorded on maps are located in or near alteration zones, indicating that the areas inferred from the current study are promising for mineralization exploration.
2) The integrated map (Figure 18) shows that the main structural trends in alteration zones are taking the NW-SE and NE-SW directions. Structural lineaments have the main effect on mineral exploration, as these lineaments act as channels for hydrothermal solutions that carry mineralization. The results of the present study show that there is an agreement between the structural lineaments and alteration zones, which is the main objective of this study.
5. Conclusions
The analyses of RTP, residual and regional maps show the magnetic features of rocks and the structural lineaments which may associate with mineralization zones. Also, the depths of the shallow and deep magnetic anomalies are estimated by the radially averaged power spectrum. The first vertical derivative (FVD), horizontal gradient magnitude (HGM), tilt derivative (TDR) and near-surface maps illustrated the locations of the magnetic anomalies and shallow structural lineaments. The remote sensing images revealed the boundaries of rock units, surface structural lineaments and alteration areas.
The results of the application of different magnetic and remote sensing techniques revealed the following:
1) The computed power spectrum of the RTP airborne magnetic data revealed that the estimated average depths for shallow and deep magnetic causative bodies were 700 m and 1800 m respectively.
2) Through the implementation of different processing and filter techniques such as the first vertical derivative (FVD), horizontal gradient magnitude (HGM), tilt derivative (TDR) and near-surface for the airborne magnetic data. The structural lineaments that affected the study area were extracted and represented as rose diagrams. These structural lineaments played an important role in the mineral distributions. Also, these lineaments were correlated with known mineralization that was found from the previous studies. Some of the known mineralization coincided with the extracted structural lineaments.
3) The processing of remote sensing data displayed the alteration zones of ferric, ferrous and hydroxyl-minerals, which appeared in a very light pink color. The clay minerals content in the sedimentary rocks and wadi deposits are represented by dark green color.
4) Crosta alteration image showed the alteration zones of the iron-bearing minerals and hydroxide-bearing mineral richer zones appeared by brown color.
5) The analysis of the structural lineaments as deduced from geologic, remote sensing, RTP, near surface, residual and regional maps for the study area are taking the NW-SE, NE-SW, E-W and N-S directions.
6) It is recommended to carry out geochemical and geophysical studies to test the type and degree of mineralization especially in the alteration zones obtained from the present study.
Acknowledgements
Firstly, we thank Allah who helps us to finish this study, we also thank our colleges in ground geophysics department who give us the requested information about the study area. Finally, many thanks to everyone supported us to finish the present paper in a good final form.
Conflicts of Interest
The authors declare no conflicts of interest regarding the publication of this paper.
Cite this paper
El-Qassas, R.A.Y., Ahmed, S.B., Abd-Elsalam, H.F. and Abu-Donia, A.M. (2021) Integrating of Remote Sensing and Airborne Magnetic Data to Outline the Geologic Structural Lineaments That Controlled Mineralization Deposits for the Area around Gabal El-Niteishat, Central Eastern Desert, Egypt. Geomaterials, 11, 1-21. https://doi.org/10.4236/gm.2021.111001
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