Tilting of active folds and faults in the Manawatu region, New Zealand: Evidence from surface drainage patterns
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[1] J. Jackson,et al. Drainage systems and the development of normal faults: an example from Pleasant Valley, Nevada , 1994 .
[2] B. Pillans,et al. Vegetational and climatic history during oxygen isotope stage 9, Wanganui district, New Zealand, and correlation of the Fordell Ash , 1992 .
[3] P. Anderton. Structure and evolution of the South Wanganui Basin, New Zealand , 1981 .
[4] B. Pillans. Upper Quaternary marine terrace chronology and deformation, South Taranaki, New Zealand , 1983 .
[5] R. Dissen,et al. Mount Stewart‐Halcombe Anticline: A look inside a growing fold in the Manawatu region, New Zealand , 1996 .
[6] G. Berger,et al. Dating loess up to 800 ka by thermoluminescence , 1992 .
[7] T. Stern,et al. Basin formation behind an active subduction zone: three-dimensional flexural modelling of Wanganui Basin, New Zealand , 1992 .
[8] C. Vita-Finzi,et al. Active folding in the Algerian earthquake of 10 October 1980 , 1981, Nature.
[9] James Jackson,et al. The structural evolution of active fault and fold systems in central Otago, New Zealand: evidence revealed by drainage patterns , 1996 .
[10] G. King,et al. Seismic Potential Revealed by Surface Folding: 1983 Coalinga, California, Earthquake , 1984, Science.
[11] H. Philip,et al. The Armenian earthquake of 1988 December 7: faulting and folding, neotectonics and palaeoseismicity , 1992 .
[12] B. Pillans. Direct marine-terrestrial correlations, Wanganui Basin, New Zealand: The last 1 million years , 1994 .