Shocked minerals at the K/T boundary: explosive volcanism as a source
- 30 September 1987
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 48 (1-2) , 167-174
- https://doi.org/10.1016/0031-9201(87)90120-8
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Dynamic deformation of volcanic ejecta from the Toba caldera: Possible relevance to Cretaceous/Tertiary boundary phenomenaGeology, 1986
- Micrometre-sized volcanic glasses in polar ices and snowsNature, 1985
- Terminal Cretaceous Environmental EventsScience, 1985
- The quartz-coesite-stishovite transformations: new calorimetric measurements and calculation of phase diagramsPhysics of the Earth and Planetary Interiors, 1984
- Mineralogic Evidence for an Impact Event at the Cretaceous-Tertiary BoundaryScience, 1984
- Analysis of seismic body waves excited by the Mount St. Helens eruption of May 18, 1980Journal of Geophysical Research, 1984
- Soret convection and rheology (viscous dissipation): arguments for whole-mantle convectionPhysics of the Earth and Planetary Interiors, 1982
- Convective fractionation: A mechanism to provide cryptic zoning (macrosegregation), layering, crescumulates, banded tuffs and explosive volcanism in igneous processesJournal of Geophysical Research, 1981
- Metastable growth of coesite in highly strained quartzJournal of Geophysical Research, 1972
- Some Benard convection experiments: Their relationship to viscous dissipation and possible periodicity in sea-floor spreadingJournal of Geophysical Research, 1972