Whittaker et al. (Reports, 5 October 2007, p. 83) presented reconstructions for Australia and Antarctica showing a change in relative plate motion ~53 million years ago, coincident with an inferred major global plate reorganization. This comment addresses problematic areas in their assumptions and the geological consequences of their reconstructions
Tectonic structures on the seafloor preserve a wealth of information on seafloor spreading and plate...
The subduction of oceanic plateaux, which contain extraordinarily thick basaltic crust and are the m...
The present work, derived from a full global geodynamic reconstruction model over 600 Ma and based o...
Whittaker et al. (Reports, 5 October 2007, p. 83) presented reconstructions for Australia and Antar...
Accurately locating boundaries between continental and oceanic crust is topical in view of locating ...
The clockwise bend at 99 Ma (mid-Cretaceous) in linear volcanic chains in the tropical Pacific coinc...
In recent years several tectonic reconstructions have been presented for Australia-Antarctica break-...
Divergence of the Australian and East Antarctic plates is well understood from the late Jurassic ons...
Highlights • New 40Ar/39Ar dates from SW Pacific and Zealandia igneous rocks form the basis of...
We use an absolute and relative plate motion model for the plates around Australia to identify majo...
Several aspects of the plate tectonic evolution of the ridge systems and structural development of o...
Reconstructions are presented documenting the relative motion of the Australia. Antarctic and Pacif...
Oceanic crust between 38°S and 65°S along the Pacific-Antarctic ridge records a complete history of ...
We use an absolute and relative plate motion model for the plates around Australia to identify major...
Stone and Stevens agree that apparent termination of large displacement on the Last Chance thrust n...
Tectonic structures on the seafloor preserve a wealth of information on seafloor spreading and plate...
The subduction of oceanic plateaux, which contain extraordinarily thick basaltic crust and are the m...
The present work, derived from a full global geodynamic reconstruction model over 600 Ma and based o...
Whittaker et al. (Reports, 5 October 2007, p. 83) presented reconstructions for Australia and Antar...
Accurately locating boundaries between continental and oceanic crust is topical in view of locating ...
The clockwise bend at 99 Ma (mid-Cretaceous) in linear volcanic chains in the tropical Pacific coinc...
In recent years several tectonic reconstructions have been presented for Australia-Antarctica break-...
Divergence of the Australian and East Antarctic plates is well understood from the late Jurassic ons...
Highlights • New 40Ar/39Ar dates from SW Pacific and Zealandia igneous rocks form the basis of...
We use an absolute and relative plate motion model for the plates around Australia to identify majo...
Several aspects of the plate tectonic evolution of the ridge systems and structural development of o...
Reconstructions are presented documenting the relative motion of the Australia. Antarctic and Pacif...
Oceanic crust between 38°S and 65°S along the Pacific-Antarctic ridge records a complete history of ...
We use an absolute and relative plate motion model for the plates around Australia to identify major...
Stone and Stevens agree that apparent termination of large displacement on the Last Chance thrust n...
Tectonic structures on the seafloor preserve a wealth of information on seafloor spreading and plate...
The subduction of oceanic plateaux, which contain extraordinarily thick basaltic crust and are the m...
The present work, derived from a full global geodynamic reconstruction model over 600 Ma and based o...