From the Late Carboniferous until the Middle Jurassic, continents were assembled in a quasi-rigid supercontinent called Pangea. The first palaeomagnetic data of South America indicated that the continent remained stationary in similar present-day latitudes during most of the Mesozoic and even the Palaeozoic. However, new palaeomagnetic data suggest that such a scenario is not likely, at least for the Jurassic. In order to test the stationary versus the dynamic-continent model, we studied the Jurassic apparent polar wander paths of the major continents, that is, Eurasia, Africa and North America that all in all show the same shape and chronology of the tracks with respect to those from South America. We thus present a master path that could ...
As a continuation of a systematic paleomagnetic research in the northern part of stable Adria, which...
Modern generations of apparent polar wander paths (APWPs) show the occurrence in North American and ...
True polar wander (TPW) is the reorientation of the crust-mantle system driven by the redistribution...
The apparent polar wander paths (= APWPs) for the northern and southern continents have been redeter...
A paleomagnetic pole and a new Ar-Ar date of 156.08 ± 0.05 Ma are reported for the Chon Aike Formati...
Many of the controversies that arise in global reconstructions for Permian-Triassic time could be re...
Several recent analyses of paleomagnetic data support the concept of Pangea, an assemblage of most o...
El estudio paleomagnético se llevó a cabo en cinco secciones del Jurásico Inferior de la Cuenca Neuq...
A long-standing debate regarding the configuration of Pangea during the Late Paleozoic has been goin...
A palaeomagnetic study has been carried out in five sections of Lower Jurassic age from the Neuquén ...
Paleomagnetic poles were obtained from the Chinle, Kayenta, Summerville, and Morrison Formations. Co...
Jurassic paleomagnetic data from North America have long been contentious, generating ambiguities in...
Eight paleomagnetic poles are considered to be reliable Jurassic reference poles for cratonic North ...
Modern generations of apparent polar wander paths (APWPs) show the occurrence in North American and...
The drift history of the Lhasa terrane from Gondwana to Asia plays a crucial role in understanding t...
As a continuation of a systematic paleomagnetic research in the northern part of stable Adria, which...
Modern generations of apparent polar wander paths (APWPs) show the occurrence in North American and ...
True polar wander (TPW) is the reorientation of the crust-mantle system driven by the redistribution...
The apparent polar wander paths (= APWPs) for the northern and southern continents have been redeter...
A paleomagnetic pole and a new Ar-Ar date of 156.08 ± 0.05 Ma are reported for the Chon Aike Formati...
Many of the controversies that arise in global reconstructions for Permian-Triassic time could be re...
Several recent analyses of paleomagnetic data support the concept of Pangea, an assemblage of most o...
El estudio paleomagnético se llevó a cabo en cinco secciones del Jurásico Inferior de la Cuenca Neuq...
A long-standing debate regarding the configuration of Pangea during the Late Paleozoic has been goin...
A palaeomagnetic study has been carried out in five sections of Lower Jurassic age from the Neuquén ...
Paleomagnetic poles were obtained from the Chinle, Kayenta, Summerville, and Morrison Formations. Co...
Jurassic paleomagnetic data from North America have long been contentious, generating ambiguities in...
Eight paleomagnetic poles are considered to be reliable Jurassic reference poles for cratonic North ...
Modern generations of apparent polar wander paths (APWPs) show the occurrence in North American and...
The drift history of the Lhasa terrane from Gondwana to Asia plays a crucial role in understanding t...
As a continuation of a systematic paleomagnetic research in the northern part of stable Adria, which...
Modern generations of apparent polar wander paths (APWPs) show the occurrence in North American and ...
True polar wander (TPW) is the reorientation of the crust-mantle system driven by the redistribution...