Thermal stresses in subducting lithosphere can explain double seismic zones
- 1 February 1982
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 295 (5850) , 587-589
- https://doi.org/10.1038/295587a0
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Fine structure of the dipping seismic zone and subduction mechanics in the Shumagin Islands, AlaskaJournal of Geophysical Research, 1982
- Double seismic zone beneath the Mariana Island ArcJournal of Geophysical Research, 1981
- Double seismic zones and stresses of intermediate depth earthquakesGeophysical Journal International, 1981
- Observations of flexure and the rheology of the oceanic lithosphereJournal of Geophysical Research, 1981
- Double-planed structure of the deep seismic zone in the northeastern Japan arcTectonophysics, 1978
- The mechanisms of creep in olivinePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1978
- A double Benioff Zone beneath the central Aleutians: An unbending of the lithosphereGeophysical Research Letters, 1977
- Geometry of Benioff Zones: Lateral segmentation and downwards bending of the subducted lithospherePublished by Wiley ,1977
- Temperature field and geophysical effects of a downgoing slabJournal of Geophysical Research, 1971
- The seismicity and deep structure of Island arcsJournal of Geophysical Research, 1966