Using the X-ray micro-computed tomography to reveal cryptic
strain fabric of faulted soft sediment: outlines of a pilot
study and preliminary results

D 2017

Using the X-ray micro-computed tomography to reveal cryptic strain fabric of faulted soft sediment: outlines of a pilot study and preliminary results

ŠPAČEK, Petr; Petr HERZÁN a Veronika SMÉKALOVÁ

Základní údaje

Originální název

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

ŠPAČEK, Petr; Petr HERZÁN a Veronika SMÉKALOVÁ

Vydání

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, od s. 366-369, 2017

Další údaje

Jazyk

angličtina

Typ výsledku

Stať ve sborníku

Obor

10505 Geology

Stát vydavatele

Nový Zéland

Utajení

není předmětem státního či obchodního tajemství

Forma vydání

elektronická verze "online"

Organizační jednotka

Přírodovědecká fakulta

ISBN

978-1-988530-36-9

DOI

http://dx.doi.org/10.21420/G2H061

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 6. 2. 2018 16:55, Mgr. Petr Špaček, Ph.D.

Anotace

V originále

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.

Citovat

ŠPAČEK, Petr; Petr HERZÁN a 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, s. 366-369. ISBN 978-1-988530-36-9. Dostupné z: https://dx.doi.org/10.21420/G2H061.

@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  - CONF
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 a 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, s.~366-369. ISBN~978-1-988530-36-9. Dostupné z: https://dx.doi.org/10.21420/G2H061.

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