MICROSTRUCTURAL OBSERVATIONS ON NATURAL SYNTECTONIC FIBROUS VEINS: IMPLICATIONS FOR THE GROWTH PROCESS

dc.contributor.author	Hilgers C.
dc.contributor.author	Urai J.L.
dc.date.accessioned	2021-04-20T03:35:24Z
dc.date.available	2021-04-20T03:35:24Z
dc.date.issued	2002
dc.identifier	https://www.elibrary.ru/item.asp?id=1233503
dc.identifier.citation	Tectonophysics, 2002, 352, 3-4, 257-274
dc.identifier.issn	0040-1951
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28192
dc.description.abstract	Syntectonic antitaxial and ataxial fibrous veins were investigated using SEM, microprobe, cathodoluminescence (CL) and optical microscopy. In antitaxial calcite veins, fibres and surrounding selvage grew simultaneously, with similar growth rates of crystallographically differently oriented grains. New material precipitated at the vein margin in antitaxial and bi-mineralic ataxial microstructures. Bridges of country rock material formed during vein growth in an initial en-echelon vein system. In our antitaxial and bi-mineralic ataxial samples, the spacing of solid inclusions does not reflect individual crack-seal openings.
dc.subject	CRACK-SEAL
dc.subject	FIBROUS VEIN
dc.subject	ANTITAXIAL
dc.subject	ATAXIAL
dc.subject	CATHODOLUMINESCENCE
dc.title	MICROSTRUCTURAL OBSERVATIONS ON NATURAL SYNTECTONIC FIBROUS VEINS: IMPLICATIONS FOR THE GROWTH PROCESS
dc.type	Статья

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