Add to ORKGA method for constructing maps of the positions of the continents in the past, using palaeomagnetic results, is described. It is illustrate
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Palaeomagnetic poles for a stable continental block are typically defined from a combination of decl...
All available Carboniferous and younger paleomagnetic data (some 220 individual observations) have ...
In theory it is possible now to reconstruct the ancient continental configurations, both in latitud...
Rocks have the ability to preserve magnetic information used in determining past geographic formatio...
The presentation of a revised set of maps for the Mesozoic and Cenozoic, together with a new set for...
The ability of certain rocks to become magnetised parallel to the earth’s magnetic field has been re...
A century ago geologists first began to consider the possibility of large lateral shifts of the cont...
ec to ni cs an d ge o dy na m ic s Apparent polar wander paths for the major continents (200 Ma to t...
This list incorporates the results available to the author up to April 1960. Cases are now arising w...
Palaeomagnetism and archaeomagnetism are fascinating specialized studies because they are applicable...
Abstract: Neoproterozoic to Late Palaeozoic times saw the break-up of the supercontinent Rodinia, an...
Summary. The information available for determining palaeopoles for oceanic plates includes data of f...
The enclosed figures illustrate continental geography and continental position for fourteen differen...
Over fifty years ago, the new Department of Geophysics of the Australian National University in Canb...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Palaeomagnetic poles for a stable continental block are typically defined from a combination of decl...
All available Carboniferous and younger paleomagnetic data (some 220 individual observations) have ...
In theory it is possible now to reconstruct the ancient continental configurations, both in latitud...
Rocks have the ability to preserve magnetic information used in determining past geographic formatio...
The presentation of a revised set of maps for the Mesozoic and Cenozoic, together with a new set for...
The ability of certain rocks to become magnetised parallel to the earth’s magnetic field has been re...
A century ago geologists first began to consider the possibility of large lateral shifts of the cont...
ec to ni cs an d ge o dy na m ic s Apparent polar wander paths for the major continents (200 Ma to t...
This list incorporates the results available to the author up to April 1960. Cases are now arising w...
Palaeomagnetism and archaeomagnetism are fascinating specialized studies because they are applicable...
Abstract: Neoproterozoic to Late Palaeozoic times saw the break-up of the supercontinent Rodinia, an...
Summary. The information available for determining palaeopoles for oceanic plates includes data of f...
The enclosed figures illustrate continental geography and continental position for fourteen differen...
Over fifty years ago, the new Department of Geophysics of the Australian National University in Canb...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Palaeomagnetic poles for a stable continental block are typically defined from a combination of decl...
All available Carboniferous and younger paleomagnetic data (some 220 individual observations) have ...