Hypogenic karst development in a hydrogeological context, Buda Thermal Karst, Budapest, Hungary

2012 ◽  
pp. 137-152
2015 ◽  
pp. 90 ◽  
Author(s):  
E. D. Shavrina ◽  
V. N. Malkov ◽  
E. I. Gurkalo

2021 ◽  
Vol 36 (3) ◽  
Author(s):  
Mohammad Mohammadian ◽  
Gholam Reza Lashkaripour ◽  
Nasser Hafezi Moghaddas ◽  
Mohammad Ghafoori

2019 ◽  
Vol 201 ◽  
pp. 32-42 ◽  
Author(s):  
Petra Kovács-Bodor ◽  
Katalin Csondor ◽  
Anita Erőss ◽  
Dénes Szieberth ◽  
Ágnes Freiler-Nagy ◽  
...  

2020 ◽  
pp. 1-14
Author(s):  
Eduardo Mayoral ◽  
María Eugenia Dies Álvarez ◽  
José Antonio Gámez Vintaned ◽  
Rodolfo Gozalo ◽  
Eladio Liñán ◽  
...  

Abstract We study the largest exposed example of an early Cambrian palaeokarst, associated with laterites and developed during rifting of the Ossa–Morena Zone. The lithostratigraphy, biostratigraphy, facies and the genesis reflect episodes of sea-level fall (Cerro del Hierro Regression) related to tectonic events and palaeoclimate. This palaeokarst can be primarily considered as the result of early Cambrian polyphase karstification in an extensional tectonic regime, later modified by Neogene–Quaternary geomorphological processes. The event may correlate with other regressive events of a similar age in Spain, Italy, United Kingdom, South America and Australia. This episode also has local names (e.g. Cerro del Hierro Regression in the Mediterranean region; Woodlands Regression in the UK). It is sometimes accompanied by additional karst development outside of Spain that is compared and interpreted in a global context.


1960 ◽  
Vol S7-II (7) ◽  
pp. 824-830
Author(s):  
Reynold Barbier

Abstract Geologic investigations showed that in spite of the degree of karst development, construction of an underground tunnel for a hydroelectric installation was possible in the vicinity of the Sassenage falls near Grenoble (France), in the area of the Sassenage fold-fault. Only two small cavities were encountered over a distance of some 3.5 kilometers. The results of the geologic studies that prepared the way for construction of the installation (which began operation in 1958) are summarized.


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