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
- 31 May 1985
- journal article
- Published by Elsevier BV in Marine and Petroleum Geology
- Vol. 2 (2), 131-141
- https://doi.org/10.1016/0264-8172(85)90003-0
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- Structure of the frontal part of the Andean Convergent MarginJournal of Geophysical Research, 1985
- Landward-dipping reflectors in accretionary wedges: Active dewatering conduits?Geology, 1984
- Varied responses to subduction in Nankai Trough and Japan Trench forearcsNature, 1983
- Mechanics of fold‐and‐thrust belts and accretionary wedgesJournal of Geophysical Research, 1983
- Hangingwall strain: A function of duplex shape and footwall topographyTectonophysics, 1982
- Fate of sediments on the descending plate at convergent marginsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1981
- ON THE THEORY OF GROWTH FAULTING*: A GEOMECHANICAL DELTA MODEL BASED ON GRAVITY SLIDINGJournal of Petroleum Geology, 1980
- MAGNETIC ANOMALIES AND TECTONIC EVOLUTION OF THE SHIKOKU INTER-ARC BASINJournal of Physics of the Earth, 1978
- The instantaneous rotation vector of the Philippine sea plate relative to the Eurasian plateTectonophysics, 1977
- Sedimentology, structural geology, and tectonics of the Shikoku subduction zone, southwestern JapanGSA Bulletin, 1976