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Showing 1 to 8 of 8 for “"Banda Arc"”.

  1. Understanding Arc-Continent Collision in the Banda Arc Through 3-D Seismic Imaging

    The active arc-continent collision in the Banda Arc is a result of convergence of the Indo-Australian plate with the Eurasian plate in SE Asia. From west to east along the Sunda-Banda arc, the subducting Indo-Australian plate changes from the Cretaceous to Jurassic age Indian Ocean lithosphere to …

    aus-cath Repository record for Understanding Arc-Continent Collision in the Banda Arc Through 3-D Seismic Imaging (opens in a new tab)

  2. Understanding Arc-Continent Collision in the Banda Arc Through 3-D Seismic Imaging

    The active arc-continent collision in the Banda Arc is a result of convergence of the Indo-Australian plate with the Eurasian plate in SE Asia. From west to east along the Sunda-Banda arc, the subducting Indo-Australian plate changes from the Cretaceous to Jurassic age Indian Ocean lithosphere to …

    anu Repository record for Understanding Arc-Continent Collision in the Banda Arc Through 3-D Seismic Imaging (opens in a new tab)

  3. Origin and Tectonic Evolution of Gondwana Sequence Units Accreted to the Banda Arc: A Structural Transect through Central East Timor

    … constrain the tectonic evolution of the active Banda Arc. Our field studies and U/Pb zircon age analysis helped assign most units to either Asian or Australian affinity. Detrital zircon from uplifted Banda forearc units (Asian affinity) have U/Pb ages as young as 80 Ma (Standley and Harris, in …

    byu Repository record for Origin and Tectonic Evolution of Gondwana Sequence Units Accreted to the Banda Arc: A Structural Transect through Central East Timor (opens in a new tab)

  4. Long-Term Surface Uplift History of the Active Banda Arc-Continent Collision: Depth and Age Analysis of Foraminifera from Rote and Savu Islands, Indonesia

    … uplift in the past 1.5 Ma of the incipient Banda arc-continent collision. Paleodepth estimates are derived from benthonic forams and ages from planktonic forams. But estimates are complicated, however, by abundant reworking; yet several distinctive species have been found. Synorogenic …

    byu Repository record for Long-Term Surface Uplift History of the Active Banda Arc-Continent Collision: Depth and Age Analysis of Foraminifera from Rote and Savu Islands, Indonesia (opens in a new tab)

  5. GPS Velocity Field In The Transition From Subduction To Collision Of The Eastern Sunda And Banda Arcs, Indonesia

    … between subduction and collision of the Banda arc reveal how strain is partitioned away from the trench and distributed to other parts of the arc-trench system. Genrich, et. al. (1996) conducted a GPS campaign (1992-1994) throughout the Eastern Sunda and Banda arcs that demonstrated …

    byu Repository record for GPS Velocity Field In The Transition From Subduction To Collision Of The Eastern Sunda And Banda Arcs, Indonesia (opens in a new tab)

  6. Banda Forearc Metamorphic Rocks Accreted to the Australian Continental Margin: Detailed Analysis of the Lolotoi Complex of East Timor

    … the region that were detached from the Banda forearc and accreted to the NW Australian continental margin during Late Miocene to Present arc-continent collision. Metamorphic rock types are dominated by (in order of greatest to least abundance), greenschist, graphitic phyllite, …

    byu Repository record for Banda Forearc Metamorphic Rocks Accreted to the Australian Continental Margin: Detailed Analysis of the Lolotoi Complex of East Timor (opens in a new tab)

  7. Seismic structure beneath Southeast Asia from adjoint waveform tomography

    … continuous slab along the 180 curvature of the Banda Arc. The tomography confirms the existence of a hole in the slab beneath Mount Tambora and locates a high S-wave velocity zone beneath northern Borneo that may be associated with subduction termination in the mid-late Miocene. A previously …

    cambridge Repository record for Seismic structure beneath Southeast Asia from adjoint waveform tomography (opens in a new tab)

  8. Catastrophic Tsunamis In the Indonesian Archipelago

    Tsunamis are not rare events for the Indonesian Archipelago as a consequence of four major plate boundaries that meet and collide, and producing highly active seismic zone that is mostly located under the sea. The ‘tsunami season’ within this region started in 1992 at Hading Bay, Flores Island, …

    waikato-masters Repository record for Catastrophic Tsunamis In the Indonesian Archipelago (opens in a new tab)