Clays and zeolite authigenesis in sediments from the flank of the Juan de Fuca Ridge

Clay Minerals

Volumn 37, Issue 1, 2002, Pages 143-155

  Buatier, M D ^a   Karpoff, A M ^a   Charpentier, D ^a  

^a UNIVERSITÉ DE FRANCHE COMTÉ   (France)

Author keywords

AEM; Alteration; Clays; Hydrothermalism; Juan de Fuca; Montmorillonite; Ridge flank; Saponite; TEM; Zeolite

Indexed keywords

CHEMICAL ANALYSIS; ENERGY DISPERSIVE SPECTROSCOPY; HYDROTHERMAL SYNTHESIS; MINERALOGY; SCANNING ELECTRON MICROSCOPY; SEAWATER; SEDIMENTS; TRANSMISSION ELECTRON MICROSCOPY; ZEOLITES;

HYDROTHERMAL PHASES;

CLAY MINERALS;

AUTHIGENESIS; CLAY MINERAL; HYDROTHERMAL ALTERATION; MARINE SEDIMENT; SEDIMENT CHEMISTRY; SMECTITE; ZEOLITE;

PACIFIC OCEAN;

EID: 0036502238     PISSN: 00098558     EISSN: None     Source Type: Journal    
DOI: 10.1180/0009855023710024     Document Type: Article

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13. The quantitative analysis of thin specimens
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40. Plate tectonic controls on diagenesis
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42. Chemical plumes from low-temperature hydrothermal venting on the Eastern flank of the Juan de Fuca Ridge
43. Experiments on the hydrothermal formation of calcium zeolites