Inherited structural control from repeated Cretaceous to Recent extension in the North Mernoo Fault Zone, western Chatham Rise, New Zealand
- 1 October 1994
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 237 (1-2) , 27-46
- https://doi.org/10.1016/0040-1951(94)90157-0
Abstract
No abstract availableKeywords
This publication has 53 references indexed in Scilit:
- Relationships between deformation and basin evolution in the intracratonic Amadeus Basin, central AustraliaPublished by Elsevier ,2003
- A note on fault reactivationPublished by Elsevier ,2003
- Modes of extensional tectonicsPublished by Elsevier ,2003
- Normal faulting in the upper continental crust: observations from regions of active extensionPublished by Elsevier ,2003
- The south Celtic Sea/Bristol Channel Basin: origin, deformation and inversion historyPublished by Elsevier ,2003
- The geometrical evolution of normal fault systemsPublished by Elsevier ,2003
- Relations between normal-fault geometry, tilting and vertical motions in extensional terrains: an example from the southern Gulf of SuezPublished by Elsevier ,2003
- Plio-Quaternary geodynamic evolution of a segment of the Peruvian Andean Cordillera located above the change in the subduction geometry: the Cuzco regionTectonophysics, 1991
- Deformation processes in an accretionary prism: a study from the Torlesse terrane of New ZealandJournal of Structural Geology, 1990
- Successive post-Variscan stress fields in the French Massif Central and its borders (Western European plate): comparison with geodynamic dataTectonophysics, 1989