Informace o publikaci
Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results
| Autoři | |
|---|---|
| Rok publikování | 2017 |
| Druh | Článek ve sborníku |
| Konference | Clark K. et al. (eds.): 8th International INQUA Meeting on Paleoseismology, Active Tectonics and Archaeoseismology, 13-16 November 2017, Blenheim, New Zealand, Handbook and Programme |
| Fakulta / Pracoviště MU | |
| Citace | |
| Doi | http://dx.doi.org/10.21420/G2H061 |
| Popis | In many exposed faults we fail to determine the slip direction and sense due to the absence of clear macroscopic kinematic indicators. To improve this situation we have been working out a technique employing the X-ray imaging of narrow faults by micro-computed tomography to reveal their cryptic strain fabric. It is expected that a detailed knowledge of 3-D particle orientation will allow resolving the shear kinematics. Here, we give a methodical concept and preliminary results of a pilot study to validate this assumption. The approach tested is potentially suitable for coarser clastic sediments or clasts-in-matrix lithologies representing common examples of faulted rocks in which slickensides typically do not develop. |