Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions

Shigekazu Kusumoto; Yasuto Itoh; Keiji Takemura; Tomotaka Iwata

doi:doi:10.11648/j.earth.20150403.11

| Peer-Reviewed

Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions

Shigekazu Kusumoto, Yasuto Itoh, Keiji Takemura, Tomotaka Iwata

Published in Earth Sciences (Volume 4, Issue 3)

Received: 15 April 2015 Accepted: 26 April 2015 Published: 8 May 2015

Views: Downloads:

Download PDF

Share This Article

Twitter
Linked In
Facebook

Abstract

In the two-dimensional discrete element modeling of displacement of sedimentary layers caused by faulting within the basement, we attempted to move a rigid basement as if it were an elastic basement by controlling its motion through application of dislocation solutions. An advantage of our modeling procedure is that we can discuss displacement fields of sedimentary layers in connection with fault parameters. We simulated displacement fields of the sedimentary layers by means of our modeling procedure and found that our simulated fields are different from the fields obtained in rigid basement models and are dependent on the selected fault parameters.

Published in	Earth Sciences (Volume 4, Issue 3)
DOI	10.11648/j.earth.20150403.11
Page(s)	89-94
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2015. Published by Science Publishing Group

Keywords

Displacement Fields of Sedimentary Layers, Two-Dimensional Discrete Element Modeling, Dislocation Solutions, Fault Parameters, Rigid Basement, Elastic Basement

References

[1]	P. A., Cundall, “A computer model for simulating progressive large scale movements in blocky rock systems,” in Proceedings of the Symposium of the International Society of Rock Mechanics, Nancy, vol. 1, Paper No. II-8, October 1971, pp. 129-136.
[2]	P. A., Cundall, and O. D. L., Strack, “A discrete numerical model for granular assemblies,” Géotechnique, vol. 29, 1979, pp. 47-65.
[3]	M., Cai, P. K., Kaiser, H., Morioka, M., Minami, T., Maejim, Y., Tasak, and H., Kurose, “FLAC/PFC coupled numerical simulation of AE in large-scale underground excavations,” Int. J. Rock Mech. Min. Sci., vol. 44, 2007, pp. 550–564. doi:10.1016/j.ijrmms.2006.09.013.
[4]	J., Hadjigeorgiou, K., Esmaieli, and M., “Grenon, Stability analysis of vertical excavations in hard rock by integrating a fracture system into a PFC model,” Tunnel. Undergr. Space Technol., vol. 24, 2009, pp. 296–308. doi:10.1016/j.tust.2008.10.002.
[5]	M. A., Antonellini, and D. D., Pollard, “Distinct element modelling of deformation bands in sandstone,” J. Struct. Geol., vol. 17, 1995, pp. 1165-1182.
[6]	L. M., Strayer, and P. J., Huddleston, “Numerical modelling of fold initiation at thrust ramps,” J. Struct. Geol., vol. 19, 1997, pp. 551-566.
[7]	J., Imbera, G. W., Tuckwell, C., Childs, J. J., Walsh, T., Manzocchi, A. E., Heath, C. G., Bonson, and J., Strand, “Three-dimensional distinct element modelling of relay growth and breaching along normal faults,” J. Struct. Geol., vol. 26, 2004, pp. 1897–1911. doi:10.1016/j.jsg.2004.02.010.
[8]	T., Vietor, and O., Oncken, “Controls on the shape and kinematics of the Central Andean plateau flanks: Insights from numerical modeling,” Earth Planet. Sci. Let., vol. 236, 2005, pp. 814–827. doi:10.1016/j.epsl.2005.06.004.
[9]	S., Hardy, and E., Finch, “Discrete-element modelling of detachment folding,” Basin Res., vol. 17, 2005, pp. 507–520. doi: 10.1111/j.1365-2117.2005.00280.x.
[10]	S., Hardy, “Structural evolution of calderas: Insights from two-dimensional discrete element simulations,” Geology, vol. 36, 2008, pp. 927-930. doi:10.1130/G25133A.1.
[11]	D. Y., Wyrick, and K. J., Smart, “Dike-induced deformation and Martian graben systems,” J. Volcanol. Geotherm. Res., vol. 185, 2009, pp. 1–11. doi:10.1016/j.jvolgeores.2008.11.022.
[12]	S., Hardy, K., McClayc, and J. A., Muñoz, “Deformation and fault activity in space and time in high-resolution numerical models of doubly vergent thrust wedges,” Mar. Petrol. Geol., vol. 26, 2009, pp. 232–248. doi:10.1016/j.marpetgeo.2007.12.003.
[13]	E. P., Holohan, M. P. J., Schöpfer, J. J., Walsh, “Mechanical and geometric controls on the structural evolution of pit crater and caldera subsidence,” J. Geophys. Res., vol. 116, 2011, B07202. doi:10.1029/2010JB008032.
[14]	N., Sakai, S., Kusumoto, and Y., Shimizu, “Numerical simulations of middle-high viscous magma extrusion by means of discrete element modeling,” Bull. Volcanol. Soc. Jpn., vol. 58, 2013, pp. 551-555. (in Japanese with English abstract)
[15]	Y., Yamada, K., Baba, A., Miyakawa, and T., Matsuoka, “Granular experiments of thrust wedges: Insights relevant to methane hydrate exploration at the Nankai accretionary prism,” Mar. Petrol. Geol., vol. 51, 2014, pp. 34-48. doi: 10.1016/j.marpetgeo.2013.11.008.
[16]	E., Finch, S., Hardy, and R., Gawthorpe, “Discrete element modelling of contractional fault-propagation folding above rigid basement blocks,” J. Struct. Geol., vol. 25, 2003, pp. 515–528.
[17]	E., Finch, S., Hardy, and R., Gawthorpe, “Discrete element modelling of extensional fault-propagation folding above rigid basement fault blocks,” Basin Res., vol. 16, 2004, pp. 489–506. doi: 10.1111/j.1365-2117.2004.00241.x.
[18]	S., Hardy, “Cover deformation above steep, basement normal faults: Insights from 2D discrete element modeling,” Mar. Petrol. Geol., vol. 28, 2011, pp. 966-972. doi:10.1016/j.marpetgeo.2010.11.005.
[19]	S., Hardy, and E., Finch, “Mechanical stratigraphy and the transition from trishear to kink-band fault-propagation fold forms above blind basement thrust faults: A discrete-element study,” Mar. Petrol. Geol., vol. 24, 2007, pp. 75–90. doi:10.1016/j.marpetgeo.2006.09.001.
[20]	Y., Okada, “Surface deformation due to shear and tensile faults in a half-space,” Bull. Seismol. Soc. Am., vol. 75, 1985, pp. 1135–1154.
[21]	Itasca, 2008, “PFC2D - Particle Flow Code in 2 Dimensions,” ver.4.0, Minneapolis, Minnesota.
[22]	J. R., Rice, and M. P., Cleary, “Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents,” Rev. Geophys. Space Phys., vol. 14, 1976, pp. 227-241.
[23]	Rundle, J. B., 1978, Viscoelastic crustal deformation by finite quasi-static sources: Journal of Geophysical Research, v. 83, p. 5937–5945.
[24]	J. B., Rundle, “Viscoelastic-gravitational deformation by a rectangular thrust fault in a layered earth,” J. Geophys. Res., vol. 87, 1982, pp. 7787–7796.
[25]	M., Matsu’ura, T., Tanimoto, and T., Iwasaki, “Quasi-static displacements due to faulting in a layered half-space with an intervenient viscoelastic layer,” J. Phys. Earth, vol. 29, 1981, pp. 23-54.

Cite This Article

Plain Text BibTeX RIS

APA Style

Shigekazu Kusumoto, Yasuto Itoh, Keiji Takemura, Tomotaka Iwata. (2015). Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sciences, 4(3), 89-94. https://doi.org/10.11648/j.earth.20150403.11

Copy | Download

ACS Style

Shigekazu Kusumoto; Yasuto Itoh; Keiji Takemura; Tomotaka Iwata. Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sci. 2015, 4(3), 89-94. doi: 10.11648/j.earth.20150403.11

Copy | Download

AMA Style

Shigekazu Kusumoto, Yasuto Itoh, Keiji Takemura, Tomotaka Iwata. Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sci. 2015;4(3):89-94. doi: 10.11648/j.earth.20150403.11

Copy | Download

@article{10.11648/j.earth.20150403.11,
  author = {Shigekazu Kusumoto and Yasuto Itoh and Keiji Takemura and Tomotaka Iwata},
  title = {Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions},
  journal = {Earth Sciences},
  volume = {4},
  number = {3},
  pages = {89-94},
  doi = {10.11648/j.earth.20150403.11},
  url = {https://doi.org/10.11648/j.earth.20150403.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20150403.11},
  abstract = {In the two-dimensional discrete element modeling of displacement of sedimentary layers caused by faulting within the basement, we attempted to move a rigid basement as if it were an elastic basement by controlling its motion through application of dislocation solutions. An advantage of our modeling procedure is that we can discuss displacement fields of sedimentary layers in connection with fault parameters. We simulated displacement fields of the sedimentary layers by means of our modeling procedure and found that our simulated fields are different from the fields obtained in rigid basement models and are dependent on the selected fault parameters.},
 year = {2015}
}

Copy | Download

TY  - JOUR
T1  - Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions
AU  - Shigekazu Kusumoto
AU  - Yasuto Itoh
AU  - Keiji Takemura
AU  - Tomotaka Iwata
Y1  - 2015/05/08
PY  - 2015
N1  - https://doi.org/10.11648/j.earth.20150403.11
DO  - 10.11648/j.earth.20150403.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 89
EP  - 94
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20150403.11
AB  - In the two-dimensional discrete element modeling of displacement of sedimentary layers caused by faulting within the basement, we attempted to move a rigid basement as if it were an elastic basement by controlling its motion through application of dislocation solutions. An advantage of our modeling procedure is that we can discuss displacement fields of sedimentary layers in connection with fault parameters. We simulated displacement fields of the sedimentary layers by means of our modeling procedure and found that our simulated fields are different from the fields obtained in rigid basement models and are dependent on the selected fault parameters.
VL  - 4
IS  - 3
ER  -

Copy | Download

Author Information

Shigekazu Kusumoto

Graduate School of Science and Engineering for Research, University of Toyama, Gofuku, Toyama, Japan
Yasuto Itoh

Graduate School of Science, Osaka Prefecture University, 1-1 Gakuen-cho, Nakaku, Sakai, Osaka Japan
Keiji Takemura

Institute for Geothermal Sciences, Graduate School of Science, Kyoto University, Kitashirakawa oiwake-cho, Sakyo-ku, Kyoto, Japan
Tomotaka Iwata

Disaster Prevension Research Institute, Kyoto University, Gokasho, Uji, Kyoto, Japan

Download PDF

Sections

Plain Text BibTeX RIS

APA Style

Shigekazu Kusumoto, Yasuto Itoh, Keiji Takemura, Tomotaka Iwata. (2015). Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sciences, 4(3), 89-94. https://doi.org/10.11648/j.earth.20150403.11

Copy | Download

ACS Style

Shigekazu Kusumoto; Yasuto Itoh; Keiji Takemura; Tomotaka Iwata. Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sci. 2015, 4(3), 89-94. doi: 10.11648/j.earth.20150403.11

Copy | Download

AMA Style

Shigekazu Kusumoto, Yasuto Itoh, Keiji Takemura, Tomotaka Iwata. Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions. Earth Sci. 2015;4(3):89-94. doi: 10.11648/j.earth.20150403.11

Copy | Download

@article{10.11648/j.earth.20150403.11,
  author = {Shigekazu Kusumoto and Yasuto Itoh and Keiji Takemura and Tomotaka Iwata},
  title = {Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions},
  journal = {Earth Sciences},
  volume = {4},
  number = {3},
  pages = {89-94},
  doi = {10.11648/j.earth.20150403.11},
  url = {https://doi.org/10.11648/j.earth.20150403.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20150403.11},
  abstract = {In the two-dimensional discrete element modeling of displacement of sedimentary layers caused by faulting within the basement, we attempted to move a rigid basement as if it were an elastic basement by controlling its motion through application of dislocation solutions. An advantage of our modeling procedure is that we can discuss displacement fields of sedimentary layers in connection with fault parameters. We simulated displacement fields of the sedimentary layers by means of our modeling procedure and found that our simulated fields are different from the fields obtained in rigid basement models and are dependent on the selected fault parameters.},
 year = {2015}
}

Copy | Download

TY  - JOUR
T1  - Displacement Fields of Sedimentary Layers Controlled by Fault Parameters: The Discrete Element Method of Controlling Basement Motions by Dislocation Solutions
AU  - Shigekazu Kusumoto
AU  - Yasuto Itoh
AU  - Keiji Takemura
AU  - Tomotaka Iwata
Y1  - 2015/05/08
PY  - 2015
N1  - https://doi.org/10.11648/j.earth.20150403.11
DO  - 10.11648/j.earth.20150403.11
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 89
EP  - 94
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20150403.11
AB  - In the two-dimensional discrete element modeling of displacement of sedimentary layers caused by faulting within the basement, we attempted to move a rigid basement as if it were an elastic basement by controlling its motion through application of dislocation solutions. An advantage of our modeling procedure is that we can discuss displacement fields of sedimentary layers in connection with fault parameters. We simulated displacement fields of the sedimentary layers by means of our modeling procedure and found that our simulated fields are different from the fields obtained in rigid basement models and are dependent on the selected fault parameters.
VL  - 4
IS  - 3
ER  -

Copy | Download