| Autor: |
Mostafa, Mohamed S., Fayed, Laila A., Abdel-Meguid, Ahmed A., Mostafa, Mostafa E. |
| Předmět: |
|
| Zdroj: |
Natural Hazards; Jan1998, Vol. 17 Issue 1, p47, 0p |
| Abstrakt: |
The plateau east of the Nile Valley at El Minia, Egypt, has been chosen for the siting of El Minia El Gedida city. Problems of underground caves suggested the need for integral geological, geotechnical and environmental hazard studies to examine the suitability of the area as a building site. Geologically, the area is formed of a thick sequence of Middle Eocene fossiliferous limestones and chalk with some layers of sandy, cherty and marly limestones. These rocks have heterogeneous physical and mechanical properties and fall within the weak to very weak range of limestones. Their mode of failure is almost of the brittle type developing extension, wedge and single shear type fractures. The mechanical properties are controlled by their physical, geological and mineralogical properties. They increase with density and dolomite content and decrease with porosity and calcite content. Empirical equations for some of these relations as well as the relation between field measures of rebound index and compressive strength are presented. Both regional and detailed structural analyses revealed the presence of major and minor normal faults and fractures trending in NWand NE directions. The NW faults are dominant. They define the topographic escarpments in the area. Most of the caves are aligned along major faults of this trend. Faults, fracture distribution and structural hazard maps of the area are presented. Paleostress tectonic analysis of these fractures suggests that the NW and NE faults are extensional due to tectonic stress which changes from normal to parallel to the Red Sea at different geologic times starting in post Middle Eocene. The similarity of this paleotectonic setting to present Red Sea tectonics points out the possibility of future rejuvenation of these faults. Topographically, the area lies in shallow surface drainage basins. The topographical risk is increased by fracturing and it should beconsidered if the area is subjected to a long period of heavy rainfall [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
| Externí odkaz: |
|
Full text from SpringerLink