By David Okaya, Tim Stern, Fred Davey
Released via the yankee Geophysical Union as a part of the Geophysical Monograph sequence, quantity 175.
A Continental Plate Boundary deals in a single position the main accomplished, updated wisdom for researchers and scholars to benefit concerning the tectonics and plate dynamics of the Pacific-Australian continental plate boundary in South Island and concerning the program of contemporary geological and geophysical equipment. It examines what occurs whilst convergence and translation take place at a plate boundary by means of
- Describing the geological and geophysical signature of a continental rework fault;
- Identifying the various vertical and lateral styles of deformation on the plate boundary;
- Assessing an obvious seismicity hole at the plate boundary fault and fast-moving plate motions;
- Comparing this plate boundary to different international convergent continental strike-slip plate boundaries;
- Documenting the software of the double-sided, onshore-offshore seismic approach for exploration of a slim continental island; and
- Providing extra papers providing formerly unpublished results.
This quantity will end up important for seismologists, tectonophysicists, geodesists and potential-field geophysicists, geologists, geodynamicists, and scholars of the deformation of tectonic plates.
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Additional resources for A Continental Plate Boundary: Tectonics at South Island, New Zealand
Periglacial conditions prevailed during the Pleistocene in eastern and northern South Island, and central and southern North Island, where loess accumulation, glacial-climate river aggradation, and interglacial degradation were widespread. Glacio-eustatic sea level fluctuation combined with tectonic uplift to leave a flight of marine terraces around the coast of New Zealand that have been used to constrain uplift rates [Kim and Sutherland, 2004; Suggate, 1965; Pillans, 1990]. By the Late Pleistocene, the topographic setting and landscape of South Island were broadly similar to that of the present day.
Elsewhere, evidence is lacking in the Southern Alps for differential fault throws that have significance greater than the uncertainty (around ± 2 km) of fission track methods [Tippett and Kamp, 1993a]. , 2005]. , 2000]. , 2005]. , 2007]. , 1999 and references therein]. Sequences typically begin with Cretaceous non-marine and marginal marine rocks, changing up section through marine clastics to carbonates by the end of the Paleogene. The Neogene sequence typically comprises marine clastics passing up into non-marine coarse lithic sediments.
3 mm/yr to have produced offset features that are preserved or are easily identifiable in the landscape. Although displacement rates are not precisely known, the total deformation distributed on these structures is insufficient to account for the 20-50% of plate motion that is not accommodated on the Alpine Fault. , 2006]. , 2007], but how, where and when this energy might be released is not known. , 2001] provide indirect, yet compelling, evidence that the “missing” component of plate boundary displacement probably occurs in the Southern Alps.
A Continental Plate Boundary: Tectonics at South Island, New Zealand by David Okaya, Tim Stern, Fred Davey
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