Structural evolution along the inner forearc of the obliquely convergent Hikurangi margin, New Zealand
- 1 February 1995
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 14 (1) , 1-18
- https://doi.org/10.1029/94tc01506
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Possible source models for the 1855 Wairarapa Earthquake, New ZealandJournal of Geophysical Research, 1992
- Pliocene and Pleistocene stratigraphy and tectonics, Ohara Depression and Wakarara Range, North Island, New ZealandNew Zealand Journal of Geology and Geophysics, 1992
- Strain Partitioning between structural domains in the forearc of the Hikurangi Subduction Zone, New ZealandTectonics, 1992
- Current plate motionsGeophysical Journal International, 1990
- Forearc uplift and extension, southern Hawke's Bay, New Zealand: Mid‐Pleistocene to presentTectonics, 1990
- Model for Late Mesozoic‐Early Tertiary tectonics of coastal California and western Mexico and speculations on the origin of the San Andreas FaultTectonics, 1986
- Structure of a growing accretionary prism, Hikurangi margin, New ZealandGeology, 1986
- Terrane motion by strike-slip faulting of forearc sliversGeology, 1986
- Mechanics of fold‐and‐thrust belts and accretionary wedgesJournal of Geophysical Research, 1983
- Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia and the western PacificJournal of Geophysical Research, 1972