A re-assessment of focal depth distributions in southern Iran, the Tien Shan and northern India: do earthquakes really occur in the continental mantle?
Open Access
- 1 December 2000
- journal article
- research article
- Published by Oxford University Press (OUP) in Geophysical Journal International
- Vol. 143 (3) , 629-661
- https://doi.org/10.1046/j.1365-246x.2000.00254.x
Abstract
No abstract availableKeywords
This publication has 64 references indexed in Scilit:
- Normal faulting in the upper continental crust: observations from regions of active extensionPublished by Elsevier ,2003
- Source parameters of moderate‐sized earthquakes in the Tien Shan, central Asia from regional moment tensor inversionGeophysical Research Letters, 1998
- Crustal thickness variations across the northern Tien Shan from teleseismic receiver functionsGeophysical Research Letters, 1998
- High‐temperature deformation of dry diabase with application to tectonics on VenusJournal of Geophysical Research, 1998
- The Bilila‐Mtakataka fault in Malaŵi: An active, 100‐km long, normal fault segment in thick seismogenic crustTectonics, 1997
- Active tectonics of the Pamirs and KarakorumJournal of Geophysical Research, 1994
- Evidence for a seismogenic upper mantle and lower crust in the Baikal RiftGeophysical Research Letters, 1991
- A very broad band inversion method for the recovery of earthquake source parametersTectonophysics, 1989
- Estimation of earthquake source parameters by the inversion of waveform data: synthetic waveformsPhysics of the Earth and Planetary Interiors, 1982
- Basement faulting and the focal depths of the larger earthquakes in the Zagros mountains (Iran)Geophysical Journal of the Royal Astronomical Society, 1981