scholarly journals Physical weathering of carbonate host-rock by precipitation of soluble salts in caves: A case study in El Orón-Arco Cave (Region of Murcia, SE Spain)

2019 ◽  
Vol 521 ◽  
pp. 1-11 ◽  
Author(s):  
Fernando Gázquez ◽  
José-María Calaforra ◽  
Nicholas P. Evans ◽  
Alexandra V. Turchyn ◽  
Fernando Rull ◽  
...  
2012 ◽  
Vol 518-523 ◽  
pp. 5754-5759
Author(s):  
Dong Jian Xue ◽  
Zheng Wei He ◽  
Xiang Dong Zheng

Derong County is located in Ganzi Tibetan Autonomous Prefecture in southern part of Sichuan Province, in the upper of the Jinsha River, where there is a subtropical plateau monsoon climate, abundant sunshine, and large amount of evaporation, so it is a typical dry-hot valleys region. Derong County is the area of more ups and downs in the terrain, deep valleys, steep mountains, complex geological conditions, intense tectonic activity, various climate types, and has obvious vertical zone effect by temperature, serious physical weathering of rock, and landslide, debris flow, collapse and other geohazards are easily induced under the influence of rainfall and human engineering activities. These geohazards have brought serious harm to the people's lives and property, and have a great impact on the socio-economic development. Through the analysis of geohazards in the study area to investigate its distribution and development trends, this paper provide a basis for geohazard prevention and economic development.


1999 ◽  
Vol 22 (1) ◽  
pp. 97-114 ◽  
Author(s):  
A. M. Poisson ◽  
J. L. Morel ◽  
J. Andrieux ◽  
M. Coulon ◽  
R. Wernli ◽  
...  
Keyword(s):  

2016 ◽  
Vol 22 (1) ◽  
pp. 27-36
Author(s):  
Tarek Nazel

Abstract The polychrome mosque of Sharaf Al-Din in the historic center of Cairo dates back to (717–738ah) (1317–1337ad). It consists of different layers of red brick and yellow limestone, characteristic of Mamluk architecture; the building is currently below the street level. The study concentrated on the mineralogical and physicochemical composition of these two construction materials, as well as identifying the Mokattam quarry as the source for the limestone. Furthermore, the presence of efflorescence in specific locations of the building was noted, and their composition was analyzed to identify the main soluble salts; these were found to be halite, gypsum and ettringite, the former two on limestone ashlars, and the latter on brick boundaries. Their formation and their possible different origins are discussed.


2000 ◽  
Vol 40 (1-2) ◽  
pp. 163-168 ◽  
Author(s):  
A. Pulido-Bosch ◽  
P. Pulido-Leboeuf ◽  
L. Molina-Sánchez ◽  
A. Vallejos ◽  
W. Martin-Rosales

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