Mathew Domeier

TL;DR: A significant number of new palaeomagnetic poles have become available since the last time a compilation was made (assembled in 2005, published in 2008) to indicate to us that a new and significantly expanded set of tables with palaeOMagnetic results would be valuable, with results coming from the Gondwana cratonic elements, Laurentia, Baltica/Europe, and Siberia as mentioned in this paper.

TL;DR: In this article, a model for the late Paleozoic (410-250 million years ago) is presented, together with a review of the underlying data, which can be used for numerical mantle modeling, and serve as a general framework for understanding late paleozoic tectonics.

TL;DR: In this paper, a model for the late Paleozoic (410-250 million years ago) is presented, together with a review of the underlying data, which can be used for numerical mantle modeling, and serve as a general framework for understanding late paleozoic tectonics.

TL;DR: Van der Voo et al. as discussed by the authors considered that the Triassic MongolOkhotsk Ocean existed east of an initially meridian-parallel, but later progressively progressively decreasing trend.

TL;DR: In this article, a plate tectonic model for the Iapetus and Rheic oceans is presented, which is defined by explicit and rigorously managed plate boundaries, the nature and kinematics of which are derived from geological evidence and plate-tectonic principles, and an extensive review of the underlying geological and paleogeographic data is also presented.