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Flat slab subduction

  • Uplift, Rupture, and Rollback of the Farallon Slab Reflected in Volcanic

    Uplift, Rupture, and Rollback of the Farallon Slab Reflected in Volcanic

  • 0 Master's Thesis the Department of Geosciences And

    0 Master's Thesis the Department of Geosciences And

  • Thermal Modelling of the Laramide Orogeny: Testing the £At-Slab Subduction Hypothesis

    Thermal Modelling of the Laramide Orogeny: Testing the £At-Slab Subduction Hypothesis

  • Andean Flat-Slab Subduction Through Time

    Andean Flat-Slab Subduction Through Time

  • Plate Tectonic Setting of the Andean Cordillera

    Plate Tectonic Setting of the Andean Cordillera

  • Foreland Uplift During Flat Subduction Insights from the Peruvian Andes

    Foreland Uplift During Flat Subduction Insights from the Peruvian Andes

  • Geological Framework of the Mineral Deposits of the Collahuasi District

    Geological Framework of the Mineral Deposits of the Collahuasi District

  • Modeling, Visualizing, and Understanding Complex Tectonic Structures on the Surface and in the Sub-Surface Steven Wild Old Dominion University

    Modeling, Visualizing, and Understanding Complex Tectonic Structures on the Surface and in the Sub-Surface Steven Wild Old Dominion University

  • PDF (Chapter 3)

    PDF (Chapter 3)

  • Economic Geology

    Economic Geology

  • Mamani Et Al., 2008A)

    Mamani Et Al., 2008A)

  • Causes and Consequences of Flat Slab Subduction in Southern Peru

    Causes and Consequences of Flat Slab Subduction in Southern Peru

  • A Grand Tour of the Ocean Basins by Declan G

    A Grand Tour of the Ocean Basins by Declan G

  • Distribution of Porphyry Copper Deposits Along the Western Tethyan

    Distribution of Porphyry Copper Deposits Along the Western Tethyan

  • Farallon Plate Subduction and the Laramide Orogeny by Sibiao

    Farallon Plate Subduction and the Laramide Orogeny by Sibiao

  • Igneous Rock Associations 7. Arc Magmatism I: Relationship Between Subduction and Magma Genesis J

    Igneous Rock Associations 7. Arc Magmatism I: Relationship Between Subduction and Magma Genesis J

  • (2.1 to 1.77 Ga) Continental Magmatic Arcs at the Tapajós and Juruena

    (2.1 to 1.77 Ga) Continental Magmatic Arcs at the Tapajós and Juruena

  • Field and Petrographic Analysis of the Indian Peak-Caliente Caldera Complex at Condor and English Canyons in Eastern Nevada

    Field and Petrographic Analysis of the Indian Peak-Caliente Caldera Complex at Condor and English Canyons in Eastern Nevada

Top View
  • Rock Uplift at the Transition from Flat-Slab to Normal Subduction
  • Influence of Peruvian Flat-Subduction Dynamics on the Evolution Of
  • Horizontal Subduction Zones, Convergence Velocity and the Building of the Andes
  • Chapter 14 Cenozoic Tectonics and Porphyry Copper Systems of the Chilean Andes
  • Recognition of a Middle–Late Jurassic Arc-Related Porphyry Copper Belt
  • Continental-Scale Geographic Change Across Zealandia During Paleogene Subduction Initiation R
  • Effect of Threedimensional Slab Geometry on Deformation in The
  • Spatial and Temporal Variations in Magma Geochemistry Along a NW
  • 1 Horizontal Subduction Zones, Convergence Velocity And
  • Central Andean Ore Deposits Linked to Evolving Shallow Subduction
  • An Interplay Between Subduction Dynamics and Crustal Wedge Tectonics Joseph Martinod, Mélanie Gérault, Laurent Husson, Vincent Regard
  • Subduction Duration and Slab
  • The Laramide Orogeny: What Were the Driving Forces?
  • Raising the Resurrection Plate from an Unfolded-Slab Plate Tectonic Reconstruction of Northwestern North America Since Early Cenozoic Time
  • A Review of the Geodynamic Evolution of Flat Slab Subduction in Mexico, Peru and Chile
  • Flat-Slab Subduction, Topography, and Mantle Dynamics in Southwestern
  • Subduction Consequences Along the Andean Margin: Thermal and Topographic Signature of an Ancient Ridge Subduction in the Marañón Basin of Perú
  • Subduction of Aseismic Ridges and Associated Deformation As Important Controls on Porphyry Copper Formation


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