Abstract
The thicknesses of veins of a single generation from the Kodiak accretionary complex show a power-law distribution with an exponent of D = 1.33. This value indicates that a significant portion of the vein-related extension is accommodated by the thinnest veins. Thick vein segments are typically confined to southeast-dipping brittle-ductile shear zones. Model simulations of vein-thickness distributions show that a constant growth model results in a negative-exponential distribution and that it is neceesary to assume size-proportional growth to produce a power-law distribution. Textures and power-law thickness distributions for the Kodiak veins are thus consistent with an increasing time-averaged growth rate as vein thickness increased, comprising a positive feedback. -Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 975-978 |
| Number of pages | 4 |
| Journal | Geology |
| Volume | 23 |
| Issue number | 11 |
| DOIs | |
| State | Published - 1995 |
All Science Journal Classification (ASJC) codes
- Geology
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