Elements for a model of the geothermal field of Milos from seismological data
- 1 January 1989
- journal article
- Published by Elsevier in Geothermics
- Vol. 18 (4) , 579-595
- https://doi.org/10.1016/0375-6505(89)90058-8
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- The critical point and two-phase boundary of seawater, 200–500°CPublished by Elsevier ,2002
- Response of two‐phase fluids to fracture configurations within submarine hydrothermal systemsJournal of Geophysical Research, 1988
- Geological and industrial implications of extensive-dilatancy anisotropyNature, 1987
- Volcanology and petrology of volcanic products from the island of Milos and neighbouring isletsJournal of Volcanology and Geothermal Research, 1986
- Differential attenuation of seismic waves at a dense array: A marker of the travale field from sources at regional distanceGeothermics, 1985
- Anomalous focal mechanisms: tensile crack formation on an accreting plate boundaryNature, 1984
- Effects of the free surface on shear wavetrainsGeophysical Journal International, 1984
- Earthquake prediction: a new physical basisGeophysical Journal International, 1984
- The variation of delays in stress-induced anisotropic polarization anomaliesGeophysical Journal International, 1981
- Seismic-wave propagation through a cracked solid: polarization as a possible dilatancy diagnosticGeophysical Journal International, 1978