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The Anahita Temple,Low-porosity limestone,Deterioration,Physical weathering,Sparite,Clay veins,XRD,SEM–EDS
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https://doi.org/10.1186/s40494-020-00411-1
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Heritage Science, https://doi.org/10.1186/s40494-020-00411-1
The Anahita Temple
Low-porosity limestone
Deterioration
Physical weathering
Sparite
Clay veins
XRD
SEM–EDS
The deterioration process of limestone in the Anahita Temple of Kangavar (West Iran)
Vahid Barnoos
Omid Oudbashi
Atefeh Shekofteh
10.1186/s40494-020-00411-1
2010-04-23
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