By David Okaya, Tim Stern, Fred Davey

ISBN-10: 0875904408

ISBN-13: 9780875904405

ISBN-10: 1118666143

ISBN-13: 9781118666142

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  • Providing extra papers providing formerly unpublished results.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.

Show description

Read Online or Download A Continental Plate Boundary: Tectonics at South Island, New Zealand PDF

Similar geophysics books

Dynamics of Multiscale Earth Systems by Horst J. Neugebauer, Clemens Simmer PDF

At the present time, earth and lifestyles scientists are more and more faced with the perplexing complexity of phenomena enmeshed in a probably boundless net of interrelations. to house this complexity and to extra our skill to research and are expecting process habit, technological know-how is studying to go beyond reliance on averages and ?

Read e-book online Geophysik II / Geophysics II PDF

Forty five downwards simply because (j at the standard raises with peak; yet this end doesn't stick with from (18. three) whilst the dependency of Kc upon ~o is considered. s 2 ERTELl and PRIESTLEY and SWINBANK have proven that the upward eddy­ flux of brilliant warmth has to be better than indicated through (18.

Download e-book for kindle: Glaciers and Glaciology of Alaska: Anchorage to Juneau, by Robert M. Krimmel, Mark F. Meier

In regards to the ProductPublished via the yank Geophysical Union as a part of the sector journey Guidebooks sequence the sphere journey Glaciers and Glaciology of Alaska for the twenty eighth foreign Geological Congress will start in Anchorage on 21 July 1989 and lead to Juneau on 29 July 1989. commute might be through bus, constitution boat, and constitution plane, with stops at Portage Glacier, Whittier, Columbia Glacier, Valdez, Yakutat, Glacier Bay, and Juneau.

F.W. Taylor's Planetary Atmospheres PDF

The emphasis of Planetary Atmospheres is on comparative elements of planetary atmospheres, ordinarily that means comparability with the Earth, together with atmospheric composition, thermal constitution, cloud homes, dynamics, climate and weather, and aeronomy. The objective is to seem for universal methods at paintings lower than varied boundary stipulations so that it will succeed in a primary knowing of the physics of atmospheres.

Additional resources for A Continental Plate Boundary: Tectonics at South Island, New Zealand

Sample text

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.

Download PDF sample

A Continental Plate Boundary: Tectonics at South Island, New Zealand by David Okaya, Tim Stern, Fred Davey


by Christopher
4.4

Get A Continental Plate Boundary: Tectonics at South Island, New PDF
Rated 4.90 of 5 – based on 29 votes