The pressure path of solid inclusions in minerals: the retention of coesite inclusions during uplift
- 1 October 1986
- Vol. 19 (3-4) , 317-324
- https://doi.org/10.1016/0024-4937(86)90030-7
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- The shift of the α-β transition temperature of quartz associated with the thermal expansion of granite at high pressurePublished by Elsevier ,2003
- Coesite in subducted continental crust: P-T history deduced from an elastic modelEarth and Planetary Science Letters, 1984
- Coesite in clinopyroxene in the Caledonides and its implications for geodynamicsNature, 1984
- Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequencesContributions to Mineralogy and Petrology, 1984
- Crack growth and the thermoelastic behavior of rocksJournal of Geophysical Research, 1979
- The origin of small cracks in igneous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1970
- Stress effects around quartz inclusions in almandine and the piezothermometry of coexisting aluminum silicatesAmerican Journal of Science, 1969
- Pressure and temperature of crystallization from elastic effects around solid inclusions in minerals?American Journal of Science, 1961