Detailed explanation of hydrogeological characteristics of gypsum aquifers is given in various situations: deep-seated karst-confined conditions, subjacent, entrenched and denuded karst types-semi-confined, phreatic and vadose conditions. The hydrogeological evolution of barren exposed gypsum karst and flow velocities in gypsum karst aquifers is also discussed
Karst aquifers have complex and original characteristics which make them very different from other a...
A Messinian succession containing gypsum beds crops out in northern Italy, mainly in Piedmont and al...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
Detailed explanation of hydrogeological characteristics of gypsum aquifers is given in various situa...
Definition of karst in gypsum and explanation of different types of karst in gypsum: intrastratal, e...
Gypsum is one of the most soluble of common rocks; it is dissolved readily to form caves, sinkholes,...
Gypsum is one of the most soluble of common rocks; it is dissolved readily to form caves, sinkholes,...
This article reviews the state of the art of speleogenetic investigations in gypsum karsts from nume...
Proper knowledge of an aquifer system is prerequisite for its utilization, protection from pollution...
This article reviews the state of the art of speleogenetic investigations in gypsum karsts from nume...
Intrastratal karst is by far the predominant gypsum karst type. Its development may begin in deep-se...
Karst aquifers have complex and original characteristics which make them very different from other a...
A Messinian succession containing gypsum beds crops out in northern Italy, mainly in Piedmont and al...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...
Detailed explanation of hydrogeological characteristics of gypsum aquifers is given in various situa...
Definition of karst in gypsum and explanation of different types of karst in gypsum: intrastratal, e...
Gypsum is one of the most soluble of common rocks; it is dissolved readily to form caves, sinkholes,...
Gypsum is one of the most soluble of common rocks; it is dissolved readily to form caves, sinkholes,...
This article reviews the state of the art of speleogenetic investigations in gypsum karsts from nume...
Proper knowledge of an aquifer system is prerequisite for its utilization, protection from pollution...
This article reviews the state of the art of speleogenetic investigations in gypsum karsts from nume...
Intrastratal karst is by far the predominant gypsum karst type. Its development may begin in deep-se...
Karst aquifers have complex and original characteristics which make them very different from other a...
A Messinian succession containing gypsum beds crops out in northern Italy, mainly in Piedmont and al...
Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of...