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Terra Australis Orogen

  • Two Contrasting Phanerozoic Orogenic Systems Revealed by Hafnium Isotope Data William J

    Two Contrasting Phanerozoic Orogenic Systems Revealed by Hafnium Isotope Data William J

  • (Ordovícico) En El Segmento Andino Central Del Orógeno Terra Australis

    (Ordovícico) En El Segmento Andino Central Del Orógeno Terra Australis

  • Billion Year Cyclicity Through Earth History: Causes and Consequences

    Billion Year Cyclicity Through Earth History: Causes and Consequences

  • Locating South China in Rodinia and Gondwana: a Fragment of Greater India Lithosphere?

    Locating South China in Rodinia and Gondwana: a Fragment of Greater India Lithosphere?

  • Early Palaeozoic Continental Growth in the Tasmanides of Northeast Gondwana and Its Implications for Rodinia Assembly and Rifting Chris L

    Early Palaeozoic Continental Growth in the Tasmanides of Northeast Gondwana and Its Implications for Rodinia Assembly and Rifting Chris L

  • Lagorio, Silvia Leonor2, Gallastegui, Gloria3, Orts, Darío1, Busteros, Alicia2, Poma Stella4 1 Universidad Nacional De Río Negro

    Lagorio, Silvia Leonor2, Gallastegui, Gloria3, Orts, Darío1, Busteros, Alicia2, Poma Stella4 1 Universidad Nacional De Río Negro

  • U-Pb Geochronologic Evidence for the Evolution of the Gondwanan Margin of the North-Central Andes

    U-Pb Geochronologic Evidence for the Evolution of the Gondwanan Margin of the North-Central Andes

  • From Rodinia to Gondwana

    From Rodinia to Gondwana

  • From Rodinia to Gondwana

    From Rodinia to Gondwana

  • Extent of the Ross Orogen in Antarctica: New Data from DSDP 270 and Iselin Bank N

    Extent of the Ross Orogen in Antarctica: New Data from DSDP 270 and Iselin Bank N

  • The Pangea Conundrum

    The Pangea Conundrum

  • Implications for the Supercontinent Cycle

    Implications for the Supercontinent Cycle

  • Supercontinent Reconstruction the Palaeomagnetically Viable, Long

    Supercontinent Reconstruction the Palaeomagnetically Viable, Long

  • Speculations on the Mechanisms for the Formation and Breakup of Supercontinents

    Speculations on the Mechanisms for the Formation and Breakup of Supercontinents

  • Terrane Processes at the Margins of Gondwana: Introduction

    Terrane Processes at the Margins of Gondwana: Introduction

  • Constraints from U-Pb and Hf Isotopic Data of Detrital Zi

    Constraints from U-Pb and Hf Isotopic Data of Detrital Zi

  • The Significance of the Transbrasiliano-Kandi Tectonic

    The Significance of the Transbrasiliano-Kandi Tectonic

  • Tectonothermal Evolution of the Sarandí Del Yí Shear Zone and Adjacent Blocks (Uruguay): Implications for the Assembly of Western Gondwana

    Tectonothermal Evolution of the Sarandí Del Yí Shear Zone and Adjacent Blocks (Uruguay): Implications for the Assembly of Western Gondwana

Top View
  • Terrane Processes at the Margins of Gondwana: Introduction
  • The Basement of the Central Andes: the Arequipa and Related Terranes
  • Is the Rate of Supercontinent Assembly Changing with Time?
  • The Brasiliano Collage in South America: a Review a Colagem Brasiliana Na América Do Sul: Uma Revisão
  • Linking Collisional and Accretionary Orogens During Rodinia Assembly and Breakup: Implications for Models of Supercontinent Cycles ∗ Peter A
  • [Klikk Her Og Skriv Tittel]
  • 1 the Tectonic Context of the Early Palaeozoic Southern Margin Of
  • The Origin and Petrologic Evolution of the Ordovician Famatinian-Puna Arc
  • About a Peri-Gondwanan-North African Enlarged Acceptance of The
  • Implications for the Supercontinent Cycle
  • Raga 63.4 Corregida.Qxp
  • Accretionary Orogens Through Earth History
  • Late Neoproterozoic and Early Cambrian Palaeogeography: Models and Problems
  • A Tectonic Reconstruction of Accreted Terranes Along
  • Turpin Et Al., 1988; Cordani Mafic and Ultramafic Rocks and Underlain by Tonalitee Et Al., 1992; Pimentel Et Al., 1994; Cruz Et Al., 2007)
  • Universidad Nacional De La Plata
  • Provenance and Tectonic Evolution of Ganderia: Constraints on the Evolution of the Iapetus and Rheic Oceans


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