غلاف الجمعية الجيولوجية -1
INSTRUCTIONS TO AUTHORS -1
All rights reserved -1
A Scientific International Journal Published By -1
EDITORIAL BOARD -1
Editor-in-Chief: -1
Prof. Dr. Selim Zeidan -1
Associate Editors: -1
Correspondence: -1
7 El – Obour Buildings, Flat 85 -1
Cairo, Egypt -1
Tel. (02) 2627061 , Email:egs@link.net -1
SELIM ZEIDAN1 -1
Note: -1
Family names are arranged in alphabetical order. -1
EGS Board 2010 -1
CONTENT1 -1
1 -1
2 -1
3 -1
Fig. (13): Interpreted structural lineament map, as deduced from magnetic and VLF-EM maps, with geologic background for Wadi Eishimbai area, South Eastern Desert, Egypt. -1
4 -1
Figure (8): Geoelectrical cross-section B-B'. -1
Figure (7): Geoelectrical cross-section A-A'. -1
Table (1): Resistivity and thickness ranges. -1
Figure (9): Geoelectrical cross-section C-C'. -1
Figure (13): Inferred area of permanent source of recharge. -1
5 -1
6 -1
Wadi Qena hydrographic basin lies in the Egyptian Central Eastern Desert (Fig. 1). It extends from north to south for about 270 km long. It locates between Lat. 26 05' and 28 05'N and Long. 32 10' and 33 35' E. It debouches into the Nile River at Qena... -1
GEOMORPHOLOGIC SETTING -1
Table (3): Geomorphological parameters of the hydrographic sub-basins in the study area using topographic maps of scale 1: 100,000. -1
SUMMARY AND CONCLUSION -1
7 -1
Intensity -1
Clay in Sandstone -1
Intensity -1
8 -1
9 -1
10 1
Legend: 2
Schlumberger/Baker Hughes Company, 2002, Case study: Prestack depth migration 11
11 -1
12 -1
13 -1
Table (1): Resistivity, thickness ranges and the corresponding lithologic composition of the detected geoelectrical layers. -1
14 -1
15 -1
16 -1
17 -1
18 -1
181 -1

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2026-01-28