Secondary faulting and transcurrent splay-faulting at transcurrent fault intersections
- 1 November 1959
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 2 (4) , 729-734
- https://doi.org/10.1080/00288306.1959.10422766
Abstract
Two principles are put forward to explain secondary faulting and transcurrent splay faulting at the intersections of clockwise with anti-clockwise transcurrent faults. The first is based on the convergence and divergence of material respectively in the compressional and tensional sectors, between the intersecting transcurrent faults. The second principle is based on the opposed sense of lateral displacement at the intersection of transcurrent faults. Either or both can be used to explain given examples.Keywords
This publication has 2 references indexed in Scilit:
- A Method of Graben and Horst FormationThe Journal of Geology, 1958
- SAN ANDREAS, GARLOCK, AND BIG PINE FAULTS, CALIFORNIAGSA Bulletin, 1953