A seismological constraint on the depth of basalt–eclogite transition in a subducting oceanic crust
Authors:
- Yoshio FukaoYFYoshio Fukao
- Sadaki HoriSHSadaki Hori
- Motoo UkawaMUMotoo Ukawa
- 1 June 1983
- journal article
- Published by Springer Nature in Nature
- Vol. 303 (5916) , 413-415
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Subduction products according to experimental predictionGeological Society of America Bulletin, 1982
- Calculation of the thermodynamic consequences of dehydration in subducting oceanic crust to 100 kb and > 800 degrees CAmerican Journal of Science, 1978
- The instantaneous rotation vector of the Philippine sea plate relative to the Eurasian plateTectonophysics, 1977
- On the Relative Importance of the Driving Forces of Plate MotionGeophysical Journal International, 1975
- Gabbro‐eclogite reaction rate and its geophysical significanceReviews of Geophysics, 1975
- The geology of the oceanic crust: Compressional wave velocities of oceanic rocksJournal of Geophysical Research, 1973
- A Comparison of Recent Experimental Data on the Gabbro-Garnet Granulite-Eclogite TransitionThe Journal of Geology, 1972
- Phase transformations and mantle dynamicsEarth and Planetary Science Letters, 1972
- CRUSTAL STRUCTURE IN THE PROFILE ACROSS CENTRAL JAPAN AS DERIVED FROM EXPLOSION SEISMIC OBSERVATIONSJournal of Physics of the Earth, 1972
- Origin of Basalt Magmas: An Experimental Study of Natural and Synthetic Rock SystemsJournal of Petrology, 1962