Volume 14 Issue 4
Dec.  2008
Turn off MathJax
Article Contents
XU Shun-shan, Nieto-Samaniego AF, Alaniz-Álvarez SA, 2008. METHODS TO CALCULATE THE FAULT-RELATED STRAIN. Journal of Geomechanics, 14 (4): 320-327.
Citation: XU Shun-shan, Nieto-Samaniego AF, Alaniz-Álvarez SA, 2008. METHODS TO CALCULATE THE FAULT-RELATED STRAIN. Journal of Geomechanics, 14 (4): 320-327.

METHODS TO CALCULATE THE FAULT-RELATED STRAIN

More Information
  • Received: 2008-09-16
  • Published: 2008-12-01
  • This paper presents some methods for calculation of fault strain. The faulting can produce continuous and discontinuous strain. The continuous strain has positive relationship with the ratio of fault displacement vs fault length and with the effective stress on the fault plane. When calculating the discontinuous fault strain, we should consider three factors that affect the establishment of equations: fault geometry, fault rotation, and fault size or fault displacement. There have been three mechanisms of fault rotation: rigid-body, vertical shear, and oblique shear. For these models, the calculation equations are established, respectively. These equations are related to the rotation angle and displacement of fault. For the rigid-body model, the fault has no internal deformation, thus the bed remain its length after rotation. The discontinuous strain due to this mechanism is smallest. The vertical shear produces bed deformation, whereas the horizontal length of bed does not change.The established equation indicates that, using the same data, the discontinuous fault strain is larger than that for the rigid-body model. Similarly, the oblique shear also causes bed deformation, but the horizontal length of bed remains constant. The obtained equation implies that the discontinuous fault strain is larger than that for the vertical shear model in the same condition.

     

  • loading
  • [1]
    Jamison WR.Fault -fracture strain in Wingate Sandstone[J]. Journal of Structural Geology, 1989, 11 (8): 959~974. doi: 10.1016/0191-8141(89)90047-3
    [2]
    Wojtal S. Measuring displacement gradients and strains in faulted rocks[J]. Journal of Structural Geology, 1989, 11 (6): 669~678. doi: 10.1016/0191-8141(89)90003-5
    [3]
    Peacock DCP, Sanderson DJ. Estimating strain from fault slip using a line sample[J]. Journal of Structural Geology, 1993, 15 (12): 1513~ 1516. doi: 10.1016/0191-8141(93)90011-X
    [4]
    Gauthier B, Angelier J. Fault tectonics and deformation: A method of quantification using field data[J]. Earth Planet Science Letters, 1985, 74 (1):137~148. doi: 10.1016/0012-821X(85)90173-6
    [5]
    Schultz RA, Fossen H. Displacement-length scaling in three dimensions:the importance of aspect ratio and application to deformation bands[J]. Journal of Structural Geology, 2002, 24 (9):1389~1411. doi: 10.1016/S0191-8141(01)00146-8
    [6]
    Wernicke B, Burchfiel BC. Modes of extensional tectonics[J]. Journal of Structural Geology, 1982, 4: 105~ 115. doi: 10.1016/0191-8141(82)90021-9
    [7]
    Jackson JA. Active normal faulting and crustal extension[A]. In: Coward MP, Dewey JF, Hancock PL. Continental Extensional Tectonics[C]. London: Geological Society, 1987, 28: 3~ 17. https://www.mendeley.com/research-papers/active-normal-faulting-crustal-extension/
    [8]
    Gibbs AD. Balanced cross-section construction from seismic sections in areas of extensional tectonics[J]. Journal of Structural Geology, 1983, 5 (2):153~ 160. doi: 10.1016/0191-8141(83)90040-8
    [9]
    Gibbs AD. Structural evolution of extensional basin margins[J]. Journal of the Geological Society, 1984, 141 (4): 609~620. doi: 10.1144/gsjgs.141.4.0609
    [10]
    Westaway R, Kusznir N.Fault and bed " rotation" during continental extension: block rotation or vertical shear?[J]. Journal of Structural Geology, 1993, 15 (6):753~770. doi: 10.1016/0191-8141(93)90060-N
    [11]
    White NJ, Jackson JA, McKenzie DP. The relationship between the geometry of normal faults and that of the sedimentary layers in their hanging walls[J]. Journal of Structural Geology, 1986, 8 (8):897~909. doi: 10.1016/0191-8141(86)90035-0
    [12]
    Xu S, Nieto-Samaniego AF, Alaniz- Álvarez SA. Tilting mechanism in domino faults of the Sierra de San M iguelito, CentralM exico [J]. Geologica Acta, 2004, 2 (3): 189~ 202. http://www.redalyc.org/resumen.oa?id=50520301
  • 加载中

Catalog

    Figures(9)  / Tables(2)

    Article Metrics

    Article views (219) PDF downloads(14) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return