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Indian Plate

  • India-Asia Collision and the Cenozoic Slowdown of the Indian Plate

    India-Asia Collision and the Cenozoic Slowdown of the Indian Plate

  • Greater India Basin Hypothesis and a Two-Stage Cenozoic Collision Between India and Asia

    Greater India Basin Hypothesis and a Two-Stage Cenozoic Collision Between India and Asia

  • Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen

    Himalaya - Southern-Tibet: the Typical Continent-Continent Collision Orogen

  • Late Paleozoic and Mesozoic Evolution of the Lhasa Terrane in the Xainza MARK Area of Southern Tibet

    Late Paleozoic and Mesozoic Evolution of the Lhasa Terrane in the Xainza MARK Area of Southern Tibet

  • The Plate Tectonics of Cenozoic SE Asia and the Distribution of Land and Sea

    The Plate Tectonics of Cenozoic SE Asia and the Distribution of Land and Sea

  • Lhasa Terrane in Southern Tibet Came from Australia

    Lhasa Terrane in Southern Tibet Came from Australia

  • Original Pdf Version

    Original Pdf Version

  • Plate Tectonics Passport

    Plate Tectonics Passport

  • The African Plate: a History of Oceanic Crust Accretion and Subduction Since the Jurassic

    The African Plate: a History of Oceanic Crust Accretion and Subduction Since the Jurassic

  • Earthquake Risk in Bangladesh

    Earthquake Risk in Bangladesh

  • Origin and Time Evolution of Subduction Polarity Reversal

    Origin and Time Evolution of Subduction Polarity Reversal

  • Insights on the Indian Ocean Tectonics and Geophysics Supported by GMT Polina Lemenkova

    Insights on the Indian Ocean Tectonics and Geophysics Supported by GMT Polina Lemenkova

  • Detailed Geometry of the Subducting Indian Plate Beneath the Burma Plate and Subcrustal Seismicity in the Burma Plate Derived from Joint Hypocenter Relocation

    Detailed Geometry of the Subducting Indian Plate Beneath the Burma Plate and Subcrustal Seismicity in the Burma Plate Derived from Joint Hypocenter Relocation

  • 38. Tectonic Constraints on the Hot-Spot Formation of Ninetyeast Ridge1

    38. Tectonic Constraints on the Hot-Spot Formation of Ninetyeast Ridge1

  • Deciphering Detailed Plate Kinematics of the Indian Ocean and Developing

    Deciphering Detailed Plate Kinematics of the Indian Ocean and Developing

  • India Plate Motion and Deformation

    India Plate Motion and Deformation

  • Initial Rifting of the Lhasa Terrane from Gondwana

    Initial Rifting of the Lhasa Terrane from Gondwana

  • Origin and Time Evolution of Subduction Polarity Reversal from Plate Kinematics of Southeast Asia

    Origin and Time Evolution of Subduction Polarity Reversal from Plate Kinematics of Southeast Asia

Top View
  • Flexure of the India Plate Underneath the Bhutan Himalaya
  • Seamounts in the Central Indian Ocean Basin: Indicators of the Indian Plate Movement
  • II. World Map - Label the Ocean Basins A
  • Plate Tectonics Puzzle
  • Localized Foundering of Indian Lower Crust in the India–Tibet Collision Zone
  • Interactions and Seismicity of Indian Tectonic Plate with Its Neighboring Plates: an Overview
  • Background Reading Earthquake Hazard and Emergency
  • Reconstructing the Total Shortening History of the NW Himalaya. Stéphane Guillot, Eduardo Garzanti, David Baratoux, Didier Marquer, Gweltaz Mahéo, Julia De Sigoyer
  • Reconstructing the Lost Eastern Tethys Ocean Basin: Convergence History of the SE Asian Margin and Marine Gateways
  • The Kerguelen Plateau and Broken Ridge, Southern Indian Ocean
  • Plate Tectonic Theory
  • Evidence from a Gabbro-Diorite Complex in the Gangdese Magmatic
  • The Development of Plate Tectonics, and His Importance at Cambridge While You Were There?
  • Plate Motions, Andean Orogeny, and Volcanism Above the South Atlantic Convection Cell Laurent Husson, Conrad Clinton P., Claudio Faccenna
  • Types of Plate Boundaries Map Identification Activity
  • Constructing Orogens in a Future Supercontinent As Thought Experiment
  • Understanding the Kerguelen Plateau and Broken Ridge
  • Anomalously Fast Convergence of India and Eurasia Caused by Double Subduction


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