Chemostratigraphic correlation of sediments containing expandable clay minerals based on ion exchange with cu(II) triethylenetetramine

Clays and Clay Minerals

Volumn 57, Issue 2, 2009, Pages 168-182

  Grygar, Tomáš ^a   Kadlec, Jaroslav ^b   Žigová, Anna ^b   Mihaljevič, Martin ^c   Nekutová, Tereza ^c   Lojka, Richard ^d   Světlík, Ivo ^e  

^a INSTITUTE OF INORGANIC CHEMISTRY   (Czech Republic)

^b INSTITUTE OF GEOLOGY   (Czech Republic)

^c CHARLES UNIVERSITY   (Czech Republic)

^d CZECH GEOLOGICAL SURVEY   (Czech Republic)

^e NUCLEAR PHYSICS INSTITUTE   (Czech Republic)

Author keywords

Chemostratigraphy; Expandable clay minerals; Flood sediments; Lacustrine sediments; Smectite

Indexed keywords

CHEMOSTRATIGRAPHY; EXPANDABLE CLAY MINERALS; FLOOD SEDIMENTS; LACUSTRINE SEDIMENTS; SMECTITE;

CALCITE; CALCIUM; CARBONATE MINERALS; GYPSUM; ION EXCHANGE; ION EXCHANGERS; METALLIC COMPOUNDS; MINERALS; ORGANIC MINERALS; OXIDE MINERALS; POSITIVE IONS; RIVERS; SEDIMENTOLOGY; SEDIMENTS; SILICATE MINERALS; SOILS; STRATIGRAPHY; SULFUR COMPOUNDS;

CLAY MINERALS;

CHEMOSTRATIGRAPHY; CLAY MINERAL; COPPER COMPOUND; ION EXCHANGE; IONIC COMPOSITION; LACUSTRINE DEPOSIT; SMECTITE; STRATIGRAPHIC CORRELATION;

CENTRAL EUROPE; CZECH REPUBLIC; EURASIA; EUROPE;

EID: 68749121463     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2009.0570204     Document Type: Article

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