| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9527084 | Tectonophysics | 2005 | 19 Pages |
Abstract
This result points out the predominance of the effects of the Permo-Carboniferous Neotethys episode, whereas the extension related to the Argo Abyssal Plain rifting that occurred later and closer to the studied area, had only limited effects on the subsidence of the proximal Dampier Sub-basin. Therefore, it supports a tectonic model with two distinct modes of extension for the Late Palaeozoic (widespread) and the Mesozoic (localised) rifting phases.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Laurent Langhi, Gilles D. Borel,