MICROSTRUCTURAL OBSERVATIONS ON NATURAL SYNTECTONIC FIBROUS VEINS: IMPLICATIONS FOR THE GROWTH PROCESS
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
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 |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru