Article ID Journal Published Year Pages File Type
9536615 Journal of Structural Geology 2005 14 Pages PDF
Abstract
Based on the arrangement of solid inclusions within the vein we suggest that our veins grew continuously during syntectonic vein formation. Solid inclusions formed by a fluctuation of adhesion at the vein wall interface rather than by crack-sealing, and vein growth was at least partly driven by the force of crystallisation.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
On the arrangement of solid inclusions in fibrous veins and the role of the crack-seal mechanism
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