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Where Is (And Was) Pennsylvania?”

Where Is (And Was) Pennsylvania?”

Earth History

Earth History

Muttoni+Kent-2019 RIPS Copy

Muttoni+Kent-2019 RIPS Copy

What's in a Name? the Columbia (Paleopangaea/Nuna) Supercontinent

What's in a Name? the Columbia (Paleopangaea/Nuna) Supercontinent

Exhibition Overview

Exhibition Overview

Opening of the Neo-Tethys Ocean and the Pangea B to Pangea a Transformation During the Permian

Opening of the Neo-Tethys Ocean and the Pangea B to Pangea a Transformation During the Permian

Paleomagnetism of the Amazonian Craton and Its Role in Paleocontinents Paleomagnetismo Do Cráton Amazônico E Sua Participação Em Paleocontinentes

Paleomagnetism of the Amazonian Craton and Its Role in Paleocontinents Paleomagnetismo Do Cráton Amazônico E Sua Participação Em Paleocontinentes

RESEARCH Geochronology and Geochemistry Of

RESEARCH Geochronology and Geochemistry Of

Climate of the Supercontinent ~Angea'

Climate of the Supercontinent ~Angea'

Iberian-Appalachian Connection Is the Missing Link Between Gondwana and Laurasia That Confrms a Wegenerian Pangaea Confguration Pedro Correia 1* & J

Iberian-Appalachian Connection Is the Missing Link Between Gondwana and Laurasia That Confrms a Wegenerian Pangaea Confguration Pedro Correia 1* & J

Reconstructing Pre-Pangean Supercontinents 1888 2013

Reconstructing Pre-Pangean Supercontinents 1888 2013

Vertebrate Palaeodistributional Patterns and Continental Drift Author(S): C

Vertebrate Palaeodistributional Patterns and Continental Drift Author(S): C

The Scandinavian Caledonides and Their Relationship to the Variscan Belt

The Scandinavian Caledonides and Their Relationship to the Variscan Belt

Mobility of Pangea: Implications for Late Paleozoic and Early Mesozoic Paleoclimate

Mobility of Pangea: Implications for Late Paleozoic and Early Mesozoic Paleoclimate

Assembly and Breakup of Supercontinents a Story of the Changing Map Patterns of the Earth

Assembly and Breakup of Supercontinents a Story of the Changing Map Patterns of the Earth

The Formation of Pangea

The Formation of Pangea

From Rodinia to Pangea: an Extroversion Process Driven First by Plume Push Followed by Downwelling Pull, Absorption and Merging

From Rodinia to Pangea: an Extroversion Process Driven First by Plume Push Followed by Downwelling Pull, Absorption and Merging

Top View
  • Late Jurassic Margin of Laurasia—A Record of Faulting Accommodating
  • Opening of the Neo-Tethys Ocean and the Pangea B to Pangea a Transformation During the Permian
  • Palaeozoic and Mesozoic Geological
  • ZOOGEOGRAPHY of FOSSIL and LIVING TURTLES-Russe// A
  • The Cambrian Explosion: Plume-Driven Birth of the Second Ecosystem on Earth
  • Reconstructing Rodinia by Fitting Neoproterozoic Continental Margins
  • Four-Dimensional Context of Earth's Supercontinents
  • On the Nature of the Cimmerian Continent and the Opening of the Neo-Tethys
  • A Paleo-Mesoproterozoic Supercontinent: Assembly, Growth and Breakup
  • Supercontinents and Landforms Warm up 1/31
  • Jurassic Accretionary Complex and Ophiolite from Northeast Turkey: No Evidence for the Cimmerian Continental Ribbon
  • Supercontinent Symposium 2012
  • Geological Reconstructions of the East Asian Blocks from the Breakup of Rodinia to the Assembly of Pangea
  • About Turn for Supercontinents System
  • Supercontinents – Teacher Notes


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