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Siliceous concretions in terrigeneous deposits of Lower Jurassic Age in Eastern Caucasus
Concretions range in size from 1 to 10 cm; they occur exclusively in argillite and are entirely absent in sandstones; formation of concretions is explained as result of polymerization of colloidal solution in silt.
Siliceous concretions in terrigeneous deposits of Lower Jurassic Age in Eastern Caucasus
Concretions range in size from 1 to 10 cm; they occur exclusively in argillite and are entirely absent in sandstones; formation of concretions is explained as result of polymerization of colloidal solution in silt.
Siliceous concretions in terrigeneous deposits of Lower Jurassic Age in Eastern Caucasus
O kremnistykh konkretsiyakh v terrigennykh otlozheniyakh nizhnei yury vostochnogo Kavkaza
Nyrkov, A.A. (author)
1964
3 pages
Article (Journal)
Russian
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