Using multispectral and radar remote sensing data for geological investigation, Qena-Safaga Shear Zone, Eastern Desert, Egypt-Reference-Cited by-同舟云学术

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Using multispectral and radar remote sensing data for geological investigation, Qena-Safaga Shear Zone, Eastern Desert, Egypt

Published:2021-05-27 Issue:11 Volume:14 Page:
ISSN:1866-7511
Container-title:Arabian Journal of Geosciences
language:en
Short-container-title:Arab J Geosci

Author:

Kamal El-Din Gamal M.,El-Noby Eman,Abdelkareem Mohamed,Hamimi Zakaria

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

https://link.springer.com/content/pdf/10.1007/s12517-021-07130-2.pdf

Reference59 articles.

1. Abd El-Wahed MA and Hamimi Z (2021a) The infracrustal rocks in the Egyptian Nubian Shield: an overview and synthesis, pp. 107-160. In: Hamimi, Z., Arai, S., Fowler, A., El-Bialy, M.Z. (Eds.); The geology of the Egyptian Nubian Shield, Regional Geology Reviews book series (RGR), Springer Nature Switzerland, 700p https://doi.org/10.1007/978-3-030-49771-2

2. Abd El-Wahed MA and Hamimi Z (2021b) The Egyptian Nubian Shield within the frame of the Arabian–Nubian sShield, pp. 15-51. In: Hamimi, Z., Arai, S., Fowler, A., El-Bialy, M.Z. (Eds.); The geology of the Egyptian Nubian Shield, Regional Geology Reviews book series (RGR), Springer Nature Switzerland, 700p https://doi.org/10.1007/978-3-030-49771-2

3. Abdelkareem M, El-Baz F (2015) Analyses of optical images and radar data reveal structural features and predict groundwater accumulations in the central Eastern Desert of Egypt. Arab J Geosci 8:2653–2666

4. Abdelkareem M, El-Baz F (2016a) Mapping hydrothermal alteration zone as a probable site of potential mineral resources in the Central Eastern Desert of Egypt using remotely-sensed data. Geol Soc Am Abstr Programs 48(7). https://doi.org/10.1130/abs/2016AM-282399

5. Abdelkareem M, El-Baz F (2016b) Mode of formation of the Nile Gorge in northern Egypt by DEM-SRTM data and GIS analysis. Geol J 51:760–778. https://doi.org/10.1002/gj.2687

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