Transition from frontal accretion to underplating in a part of the Nankai Trough Accretionary Complex off Shikoku (SW Japan) and extensional features on the lower trench slope
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- Type
- article
- Published
- 1985-05-01
- Cited by
- 51
- References
- 21
- OpenAlex
- https://openalex.org/W1984402782
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129088106
Keywords
Geology, Décollement, Accretionary wedge, Trench, Seismology
References
- Varied responses to subduction in Nankai Trough and Japan Trench forearcs
- Detailed Structure of the Nankai Trough from Migrated Seismic Sections: Convergent Margins: Field Investigations of Margin Structure and Stratigraphy
- The Possible Significance of Pore Fluid Pressures in Subduction Zones: Tectonic Processes: Model Investigations of Margin Environmental and Tectonic Processes
- Sedimentology, structural geology, and tectonics of the Shikoku subduction zone, southwestern Japan
- Hangingwall strain: A function of duplex shape and footwall topography
- Long decollements and mud volcanoes: Evidence from the Barbados Ridge Complex for the role of high pore-fluid pressure in the development of an accretionary complex
- THE INSTANTANEOUS ROTATION VECTOR OF THE PHILIPPINE SEA PLATE RELATIVE TO THE EURASIAN PLATE
- Structure of the frontal part of the Andean Convergent Margin
- Modes of extensional tectonics
- The Shimanto Belt of Japan: Cretaceous-lower Miocene active-margin sedimentation
- Fate of sediments on the descending plate at convergent margins
- MAGNETIC ANOMALIES AND TECTONIC EVOLUTION OF THE SHIKOKU INTER-ARC BASIN
- Mechanics of fold-and-thrust belts and accretionary wedges
- Landward-dipping reflectors in accretionary wedges: Active dewatering conduits?
- Structural geology in the eastern margin of the canadian rocky mountains
- ON THE THEORY OF GROWTH FAULTING*: A GEOMECHANICAL DELTA MODEL BASED ON GRAVITY SLIDING
- Accretion, Underplating, Subduction and Tectonic Evolution, Middle America Trench, Southern Mexico: Results From DSDP Leg 66
- Structural diversity along modern convergent margins and the role of overpressured pore fluids in subduction zones
- Sedimentary Evolution of Shikoku Subduction Zone: The Shimanto Belt and Nankai Trough
- In the Framework of Deformation in the Nankai Trough
Cited by
- Foldback reflectors near methane hydrate bottom‐simulating reflectors: Indicators of gas distribution from 3D seismic images in the eastern Nankai Trough
- In situ stress state from walkaround VSP anisotropy in the Kumano basin southeast of the Kii Peninsula, Japan
- Structural restoration of thrusts at the toe of the Nankai Trough accretionary prism off Shikoku Island, Japan: Implications for dewatering processes
- Distribution of methane hydrate BSRs and its implication for the prism growth in the Nankai Trough
- Subducting seamounts and deformation of overriding forearc wedges around Japan
- Melange and related structures in Torlesse accretionary wedge, Wairarapa, New Zealand
- Nankai Trough and the fossil Shikoku Ridge: results of Box 6 Kaiko survey
- Petrography of trench sands from the Nankai Trough, southwest Japan: implications for long-distance turbidite transportation
- Transitions among Mariana-, Japan-, Cordillera- and Alaska-type arc systems and their final juxtapositions leading to accretionary and collisional orogenesis
- Deformation processes in an accretionary prism : a study from the Torlesse terrane of New Zealand.
- A deep strong reflector in the Nankai accretionary wedge from multichannel seismic data: Implications for underplating and interseismic shear stress release
- Geomorphological study on a clastic accretionary prism : The Nankai Trough
- Exhumation of high-pressure rocks: a review of concepts and processes
- Deepwater high-resolution expanding spread and split spread seismic profiles in the Nankai Trough
- Structure of the Nankai Trough Accretionary Zone from multichannel seismic reflection data
- Structure of melange and associated units in the Torlesse accretionary wedge, Tararua Range, New Zealand
- Continental margin tectonics: Submarine accretionary prisms
- Evidence and mechanisms for forearc extension at the accretionary Costa Rica Convergent Margin
- Structure of the Nankai accretionary prism as revealed from IZANAGI sidescan imagery and multichannel seismic reflection profiling
- Normal faults in an accretionary complex formed at trench‐trench‐ridge triple junction, as an indicator of angle between the trench and subducted ridge
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