T215 Structure and Tectonic Studies, from Outcrop to Supercontinent II: In Honor of Ian Dalziel

Tuesday, 24 September 2019
1:30 PM - 5:30 PM
Room 229A, North Building


TWINNING STRAINS FROM SYN-FAULTING CALCITE GOUGE: SMALL-OFFSET STRIKE-SLIP, NORMAL AND THRUST FAULTS

Paper number: T215-2
Program: Technical Sessions
Time: 1:45 PM – 2:00 PM


Authors


Abstract

We have evaluated the stress-strain behavior of calcite precipitated and mechanically twinned in small-offset strike-slip (5 sites), normal (7 sites) and thrust faults (7 sites) of a variety of ages and from a variety of tectonic settings (n=3001 twinned grains) on 6 continents. For each strike-slip fault system the twinning shortening strain (e1) is horizontal and at an angle of 0°-60° to the respective fault plane (dextral or sinistral) although in the majority of cases the shortening axis is parallel to fault strike. In each normal fault example, dip-slip kinematic striations dominate the faulted surface yet the orientation of the maximum principal compressive stress (s1) and shortening strain axis (e1) are not 45° to the fault plane as predicted but are sub-horizontal and either strike-parallel or strike-normal. Thrust faults preserve shortening strain axes (e1) parallel to the dip-slip kinematic direction, within the fault plane (plane strain) and not at 45° to the principal plane. None of the fault stress-strain field results reported here support the Andersonian or Mohr-Coulomb criteria for stress-strain relations predicted along faults.

Geological Society of America Abstracts with Programs. Vol. 51, No. 5

doi: 10.1130/abs/2019AM-338487

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