Forearc
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- The Nature of the Banda Arc–Continent Collision in the Timor Region
- 22.2 the CASCADIA SUBDUCTION WEDGE: the ROLE of ACCRETION, UPLIFT, and EROSION—An Essay by Mark T. Brandon1
- Palaeozoic Accretionary and Convergent Tectonics of The
- Parallel Stretching and Folding of Forearc Basins and Lateral Migration
- Precambrian Plate Tectonics: Criteria and Evidence
- Forearc Peridotites from Tonga Record Heterogeneous Oxidation of the Mantle Following Subduction Initiation Suzanne K
- How Do Subduction Processes Contribute to Forearc Andean Uplift?
- Accretionary Orogens Through Earth History
- The Coast Range/Great Valley Ophiolite, Californ
- Isua Supracrustal Belt (Greenland)—A Vestige of a 3.8 Ga Suprasubduction Zone Ophiolite, and the Implications for Archean Geology
- Controls on Forearc Basin Formation and Evolution Insights From
- Plumes, Plateaux, and the Significance of Subduction-Related Accretionary Complexes in Early Earth Processes
- The Forearc Basin Earthquakes and Benioff Zones
- Accretionary Orogens Through Earth History
- The Transition from an Active to a Passive Margin (SW End of the South Shetland Trench, Antarctic Peninsula)
- Subduction Zones, Island Arcs and Active Continental Margins
- Structural Complexity in the Boundary of Forearc Basin
- Controls on Tectonic Accretion Versus Erosion in Subduction Zones: Implications for the Origin and Recycling of the Continental Crust