A laser-probe Ar-40/Ar-39 study of pseudotachylite from the Tambach Fault Zone, Kenya: direct isotopic dating of brittle faults

Understanding the tectonic evolution of orogenic belts and intracratonic ar eas depends on our ability to determine the age of tectonic features on a v ariety of scales. This study demonstrates the value of the laser-probe Ar-4 0/Ar-39 dating technique, which, if applied to fault-derived pseudotachylit es, may be used to directly determine the age of brittle faults. The laser- probe technique affords high spatial resolution, enabling a greater opportu nity for discriminating between pseudotachylite matrix. host-rock clasts an d alteration products that are often present in varying proportions within pseudotachylites. The laser-probe Ar-40/Ar-39 technique has been applied to pseudotachylite samples from the Tambach Fault Zone (TFZ). a major NW-SE t rending strike-slip fault within the Kenyan part of the Late Proterozoic/Ea rly Palaeozoic Mozambique Belt. The pseudotachylites of the TFZ were previo usly thought to have formed either (i) at about 530-430 Ma, or (ii) during the Cenozoic evolution of the Kenya Rift. In the latter case, seismic slip on the rift-bounding normal fault would have generated the pseudotachylites , due to the reactivation of old NW-SE trending structures in the basement. Based on our new data, we interpret the pseudotachylite formation age to b e 400 Ma. This rules out the possibility that the pseudotachylites are rela ted to the formation of the Kenya Rift. Although the inherited basement fau lts may have been locally reactivated as transfer faults, reactivation of t hese structures during rifting did not occur beyond the margins of the Keny a Rift. (C) 2001 Elsevier Science Ltd. All rights reserved.