TY - JOUR
T1 - Reverse and normal drag along a fault
AU - Grasemann, Bernhard
AU - Martel, Stephen J.
AU - Passchier, Cees W
N1 - DOI: 10.1016/j.jsg.2005.04.006
Affiliations: Department of Geological Sciences, University of Vienna, Althanstr. 14, 1090 Vienna, Austria; Department of Geology and Geophysics, University of Hawaii, Honolulu, HI, United States; Department of Geosciences, University of Mainz, Mainz, Germany
Adressen: Grasemann, B.; Department of Geological Sciences; University of Vienna; Althanstr. 14 1090 Vienna, Austria; email: [email protected]
Source-File: EarthScienceScopus_iso.csv
Import aus Scopus: 2-s2.0-22144471881
Importdatum: 27.11.2006 19:23:09
30.10.2007: Datenanforderung 1951 (Import Sachbearbeiter)
PY - 2005
Y1 - 2005
N2 - An analysis of the theoretical displacement field around a single dip-slip fault at depth reveals that normal and reverse fault drag develop by perturbation flow induced by fault slip. We analytically model the heterogeneous part of the instantaneous displacement field of an isolated two-dimensional mode II fault in an infinite, homogeneous elastic body in response to fault slip. Material on both sides of the fault is displaced and 'opposing circulation cells' arise on opposite sides of the fault, with displacement magnitudes increasing towards the center of the fault. Both normal and reverse drag can develop at the fault center depending on the angle between the markers and the fault; normal drag develops there for low angles (
AB - An analysis of the theoretical displacement field around a single dip-slip fault at depth reveals that normal and reverse fault drag develop by perturbation flow induced by fault slip. We analytically model the heterogeneous part of the instantaneous displacement field of an isolated two-dimensional mode II fault in an infinite, homogeneous elastic body in response to fault slip. Material on both sides of the fault is displaced and 'opposing circulation cells' arise on opposite sides of the fault, with displacement magnitudes increasing towards the center of the fault. Both normal and reverse drag can develop at the fault center depending on the angle between the markers and the fault; normal drag develops there for low angles (
M3 - Article
SN - 0191-8141
VL - 27
SP - 999
EP - 1010
JO - Journal of Structural Geology
JF - Journal of Structural Geology
IS - 6
ER -