| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445115 | Journal of Structural Geology | 2012 | 10 Pages |
Abstract
⸠We characterize the clay fabrics of three SAFOD samples. ⸠Randomly oriented matrix sheet silicates dominate the fault rocks. ⸠Well-oriented clay stacks occur only locally in small (<1 μm) domains. ⸠Locally aligned clay particles may act as barriers to fluid flow.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
C. Janssen, W. Kanitpanyacharoen, H.-R. Wenk, R. Wirth, L. Morales, E. Rybacki, M. Kienast, G. Dresen,