ŠPAČEK, Petr, Petr HERZÁN and Veronika SMÉKALOVÁ. Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results. Online. In Clark K. 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. 2017, p. 366-369. ISBN 978-1-988530-36-9. Available from: https://dx.doi.org/10.21420/G2H061. |
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@inproceedings{1406838, author = {Špaček, Petr and Herzán, Petr and Smékalová, Veronika}, booktitle = {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}, doi = {http://dx.doi.org/10.21420/G2H061}, editor = {Clark K.}, howpublished = {elektronická verze "online"}, language = {eng}, isbn = {978-1-988530-36-9}, pages = {366-369}, title = {Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results}, year = {2017} }
TY - JOUR ID - 1406838 AU - Špaček, Petr - Herzán, Petr - Smékalová, Veronika PY - 2017 TI - Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results SN - 9781988530369 N2 - 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. ER -
ŠPAČEK, Petr, Petr HERZÁN and Veronika SMÉKALOVÁ. Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results. Online. In Clark K. \textit{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}. 2017, p.~366-369. ISBN~978-1-988530-36-9. Available from: https://dx.doi.org/10.21420/G2H061.
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