In this paper we present nine reconstructions for the Mesozoic and Cenozoic, based on the sea-floor spreading isochrons published by Larson et al. (1985). The purpose of this study was: 1) to determine if the isochrons drawn by Larson et al. (1985) could be refitted to produce a self-consistent set of plate tectonic reconstructions, 2) to use the areas of apparent mismatch between magnetic isochrons as a focus for further investigations, and 3) to test the capabilities and accuracy of interactive computer graphic methods of plate tectonic reconstruction. In general, Tertiary and Late Cretaceous isochrons could be refitted reasonably well; however, closure errors were apparent in the vicinity of the Bouvet and Macquarie triple junctions. It ...
This dissertation involves interpretation of geophysical data and physical models of plume-ridge flu...
This paper describes the evolution of the former Tethys ocean in terms of successive positions of th...
This report presents a series of plate reconstructions for the Mesozoic and Cenozoic.UT Institute fo...
During the past 20 years, numerous oceanographic surveys have mapped the age of the ocean floor in g...
Contact plates@ig.utexas.edu for more information.During the winter of 1984 work was begun on the Pa...
A global model for Mesozoic and Cenozoic plate motions has been developed by the Paleoceanographic M...
Reconstructions of the relative positions of the Indian, African, and Antarctic plates and their unc...
We present reconstructions of the Pacific region south of the equator for the following times: Anom....
The persistent creation and destruction of ocean basins has a major influence on changes in palaeocl...
We have developed an internally consistent isochron chart and a tectonic history of the South Pacifi...
The determination of the motion of Antarctica relative to Africa is particularly important when cons...
A Cenozoic tectonic reconstruction is presented for the Southwest Pacific region located east of Aus...
Plate tectonic reconstructions for the late Mesozoic-Cenozoic evolution of the eastern Tethyan Ocean...
This report presents plate reconstructions of the Southwest Indian Ridge, Indian Ocean from the Late...
Divergence of the Australian and East Antarctic plates is well understood from the late Jurassic ons...
This dissertation involves interpretation of geophysical data and physical models of plume-ridge flu...
This paper describes the evolution of the former Tethys ocean in terms of successive positions of th...
This report presents a series of plate reconstructions for the Mesozoic and Cenozoic.UT Institute fo...
During the past 20 years, numerous oceanographic surveys have mapped the age of the ocean floor in g...
Contact plates@ig.utexas.edu for more information.During the winter of 1984 work was begun on the Pa...
A global model for Mesozoic and Cenozoic plate motions has been developed by the Paleoceanographic M...
Reconstructions of the relative positions of the Indian, African, and Antarctic plates and their unc...
We present reconstructions of the Pacific region south of the equator for the following times: Anom....
The persistent creation and destruction of ocean basins has a major influence on changes in palaeocl...
We have developed an internally consistent isochron chart and a tectonic history of the South Pacifi...
The determination of the motion of Antarctica relative to Africa is particularly important when cons...
A Cenozoic tectonic reconstruction is presented for the Southwest Pacific region located east of Aus...
Plate tectonic reconstructions for the late Mesozoic-Cenozoic evolution of the eastern Tethyan Ocean...
This report presents plate reconstructions of the Southwest Indian Ridge, Indian Ocean from the Late...
Divergence of the Australian and East Antarctic plates is well understood from the late Jurassic ons...
This dissertation involves interpretation of geophysical data and physical models of plume-ridge flu...
This paper describes the evolution of the former Tethys ocean in terms of successive positions of th...
This report presents a series of plate reconstructions for the Mesozoic and Cenozoic.UT Institute fo...