Webb1 feb. 2024 · Paleocoastline and continental margin reconstructions in Mollweide projection for the 185–255 Ma after incorporating fossil occurrence data from the PBDB. The paleopositions of present-day coastlines and administrative boundaries are shown with black lines. Webb1 feb. 2024 · We 2) also use the fossil occurrence data to update the continental margins and map paleocoastlines that represent maximum transgressive surfaces for each …
3D paleogeographic and plate tectonic …
Webbტექტონიკა (ბერძ. tektonikós – სამშენებლო) — გეოლოგიის დარგი, რომელიც ... WebbThe PALEOMAP Project publishes the results of its research in a variety of formats useful for teaching and research: Atlases & AnimationsAtlases & Animations showing the plate … The Pacific Ocean is the world's largest ocean, covering nearly one-half of the … This animation shows what the world of the Late Cretaceous might have looked like. … Seafloor Spreading in the North Atlantic Ocean (to run animation, drag mouse … Earliest Jurassic - Home Page [scotese.com] This animation shows the motions of the continents from the Late Precambrian to … The Assembly of "Pangea Ultima" (to run animation, drag mouse across image) Early Cretaceous - Home Page [scotese.com] Modern Globe - Home Page [scotese.com] fibel zebra
Scotese Animation: Paleogeography (750 Ma - Present-day)
Webb6 juni 2007 · Created and compiled by Christopher Scotese, from the University of Texas at Arlington, Paleomap Project is a site that uses maps and animation to illustrate earth … WebbThe summary of the 2024-2024 goals are: 1. Refine depositional-environment and volcanic-province Knowledge Trees to maximize capture of data and usability. 2. Work towards a universal Lexicon for all geologic formations around the world. 3. Develop interactive web service for interrogating regional/global geology. a. Webb1 apr. 2024 · CRS would like to thank the past industrial sponsors of the PALEOMAP Project. H.S. is supported by the National Natural Science Foundation of China (41821001). B.J.W.M. is supported by the UK Natural Environment Research Council (NE/S009663/1). hq mi angi 36-2806