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2018
The Karst topography describes the dissolution of underlying soluble rocks by surface water or ground water. This is commonly found in carbonate terrain (limestone and dolomite) in mountainous regions. The rain water infiltrates through the cracks of the rocks in the vertical manner until it reaches the water table and thereafter, it moves horizontally
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The Karst topography describes the dissolution of underlying soluble rocks by surface water or ground water. This is commonly found in carbonate terrain (limestone and dolomite) in mountainous regions. The rain water infiltrates through the cracks of the rocks in the vertical manner until it reaches the water table and thereafter, it moves horizontally
openaire +1 more source
Causes of colour and fluorescence in speleothems
Chemical Geology, 2001Philip Van Beynen +2 more
exaly
Holocene ENSO-related cyclic storms recorded by magnetic minerals in speleothems of central China
Proceedings of the National Academy of Sciences of the United States of America, 2017Mark D Bourne, Chaoyong Hu, Hai Cheng
exaly
Elevated and variable values of 13C in speleothems in a British cave system
Chemical Geology, 1997Emi Itô, Andy Baker, Peter L Smart
exaly