Deformation history of tectonic melange and its relationship to the underplating process and relative plate motion: An example from the deeply buried Shimanto Belt, SW Japan

Tectonics

Volumn 20, Issue 3, 2001, Pages 376-393

  Onishi, C T ^a   Kimura, G ^b   Hashimoto, Y ^b   Ikehara Ohmori, K ^a   Watanabe, T ^a  

^a HOKKAIDO UNIVERSITY   (Japan)

^b UNIVERSITY OF TOKYO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

ACCRETION; DEFORMATION MECHANISM; MELANGE; SUBDUCTION ZONE; TECTONIC EVOLUTION; UNDERPLATING;

HONSHU; JAPAN; SHIMANTO BELT;

EID: 0034989397     PISSN: 02787407     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999TC001154     Document Type: Article

References (60)

1. The interaction of fluid process and progressive deformation during shallow level accretion: Examples from the Shimanto Belt of SW Japan
2. Detailed structure of the Nankai Trough from migrated seismic sections
3. Thermal structure and uplift of the Cretaceous Shimanto Belt, Kii Peninsula, southwest Japan: An illite crystalinity and illite bO lattice spacing study
4. The high pressure metamorphic belts in Japan: A review
5. Calculation of vitrinite reflectance from thermal histories and peak temperatures: A comparision of methods
6. Orthogneiss, mylonite and non-coaxial deformation of granites: The example of the South Armonian Shear Zone
7. Early deformation in melange terranes of the Ghost Rocks Formation, Kodiak Islands, Alaska
8. Evidence for changing plate motions in southwest Japan and reconstructions of the Philippine Sea Plate
9. Evidence for a weak and overpressured decollement beneath sediment-dominated accretionary prism
10. Structural synthesis: Correlation of structural fabrics, velocity anisotropy, and magnetic susceptibility data
11. Fixed hotspots gone with the wind
12. Flow melanges: Numerical modeling and geologic constraints to their origin in the Franciscan subduction complex. California
13. Structural styles in Mesozoic and Cenozoic melanges in the western Cordillera of North America
14. Relative motions between oceanic and continental plates in the Pacific basin
15. Structural evolution of underthrusted sediments, Kodiak Islands, Alaska
16. Plate convergence, transcurrent faults, and internal deformation adjacent to southeast Asia and western Pacific
17. Evolution of the Shimanto accretionary complex: A fission-track thermochronologic study
18. Underplating process from melange formation to duplexing: Example from the Cretaceous Shimanto Belt, Kii Peninsula, southwest Japan
19. Sheath-like folds and progressive fold deformation in Tertiary sedimentary rocks of the Shimanto accretionary complex
20. The principles of melanges and their bearing on the Franciscan-Knoxville paradox
21. The seismogenic zone of subduction thrust faults
22. Anatomy and genesis of a subduction-related orogen: A new view of geotectonic subdivision and evolution of the Japanese Island
23. Tectonic implications of the 1944 Tonankai and the 1946 Nankaido earthquakes
24. Asymmetrical melange fabric as possible indicators of the convergent direction of plates: A case study from the Shimanto Belt of the Akaishi Mountains, central Japan
25. Cretaceous episodic growth of the Japanese Island
26. Underplated units in an accretionary complex: Melange of the Shimanto Belt of eastern Shikoku, southwest Japan
27. A deep section of accretionary complex: Susunai Complex in Sakhalin Island, northwestern Pacific margin
28. Deformation mechanism path diagrams for sediments undergoing lithification
29. Shimanto Belt in the Kii Peninsula, southwest Jpn
30. Geology of the Kudoyama area in the western Kii Peninsula, southwest Japan, with reference to disappearance of the Chichibu terrane
31. Controls on accretion of flysch and melange belts at convergent margins: Evidence from the Chugach Bay thrust and Iceworm melange, Chugach accretionary wedge. Alaska
32. Macroscopic structural features in Deep Sea Drilling Project cores from forearc regions
33. Oblique plate convergence, slip vectors, and forearc deformation
34. Mechanims of subduction accretion along the central Aleutian Trench
35. Slump strain indicative of paleoslope in Cretaceous Izumi sedimentary basin among Median Tectonic Line, southwest Japan
36. Tectonics and hydrogeology of accretionary prism: Role of the decollement zone
37. Thickening of fault zones: A mechanism for melange formation in accreting sediments
38. Continental margin tectonics: Submarine accretionary prism
39. Asymmetric extensional structures and their implication for the generation of melanges
40. Plate motions in the North Pacific: The 43 Ma nonevent
41. Paleothermal structure of the Shimanto accretionary prism, Shikoku. Japan: Role of an out-of-sequence thrust
42. Change in fabric of melange in the Shimanto Belt, Japan: Change in relative convergence?
43. When was the Japan Sea opened?: Paleomagnetic evidence from southwest Japan
44. Nature of seismic coupling along simple plate boundaries of the subduction type
45. The uplift of high-pressure-low-temperature metamorphic rocks
46. Stratal extension in thrust footwalls. Makran accretionary prism: Implications for thrust tectonics
47. Duplex accretion and underplating in an ancient accretionary complex, Kodiak Island, Alaska
48. A model for the motion of the Philippine Sea plate consistent with NUVEI-1 and geological data
49. The relationship between regionally consistent stretching lineations and plate motions
50. Comments on the growth of accretionary wedges
51. Fundamental process of the construction of Japanese Island-Oblique subduction and strikeslip fault
52. Accretion tectonics and evolution of Japan
53. Paleomagnetic evidence for motion of the Hawaiian hotspot during formation of the Emperor seamounts
54. Large-scale motion between Pacific and Atlantic hotspots
55. Tectonometamorphism of the Shimanto Belt
56. Segmentation and Holocene surface faulting on the Median Tectonic Line, southwest Japan
57. On the mechanical role of smectite in subduction zone
58. The brittle-ductile transition in porous sedimentary rocks: Geological implications for accretionary wedge aseimicity