The Jurassic to Mid-Cretaceous apparent polar wander path of the Pacific plate irrespective of ages have been delineated. Two poles have been established: one pole, which is relatively older than the other, is at 75.01°N/287.5°E (α = 6.9°) and the other pole is at 61.0°N°/304.7°E (!95 = 4.5°). These results indicate that the Pacific plate drifted southward during the Jurassic to Early-Cretaceous period. Additionally, the results demonstrate that there is an apparent consistent correspondence between changes of plate motion and significant shifts of the Jurassic to Mid-Cretaceous apparent polar wander path
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...
To construct the Mesozoic apparent polar wander path (APWP) for the inner arc of the southwestern Ja...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
True polar wander, or TPW, is the rotation of the entire mantle–crust system about an equatorial axi...
Eight paleomagnetic poles are considered to be reliable Jurassic reference poles for cratonic North ...
Utilizing marine magnetic anomalies and paleomagnetic pole positions, paleogeographic maps were cons...
The North American apparent polar wander (APW) path indicates an episode of unusually rapid absolute...
The palaeoinagnetism of Cretaceous Pacific seamounts, as deduced from their magnetic anomalies, is r...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
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...
To construct the Mesozoic apparent polar wander path (APWP) for the inner arc of the southwestern Ja...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
Understanding of Pacific plate tectonics and geodynamics is aided by refinement of the plate's appar...
True polar wander, or TPW, is the rotation of the entire mantle–crust system about an equatorial axi...
Eight paleomagnetic poles are considered to be reliable Jurassic reference poles for cratonic North ...
Utilizing marine magnetic anomalies and paleomagnetic pole positions, paleogeographic maps were cons...
The North American apparent polar wander (APW) path indicates an episode of unusually rapid absolute...
The palaeoinagnetism of Cretaceous Pacific seamounts, as deduced from their magnetic anomalies, is r...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
Synthetic apparent polar wander (APW) paths for North America, South America, Eurasia, India, Centra...
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...
To construct the Mesozoic apparent polar wander path (APWP) for the inner arc of the southwestern Ja...