U-Pb Garnet, Sphene, Monazite, and Rutile Ages: Implications for the Duration of High-Grade Metamorphism and Cooling Histories, Adirondack Mts., New York
- 1 May 1991
- journal article
- Published by University of Chicago Press in The Journal of Geology
- Vol. 99 (3) , 415-428
- https://doi.org/10.1086/629503
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Age of Xenolith-Bearing Olivine Metagabbro, Eastern Adirondack Mountains, New YorkThe Journal of Geology, 1989
- Evidence for Multiple Metamorphic Events in the Adirondack Mountains, N.Y.The Journal of Geology, 1988
- U-Pb zircon geochronology of the Adirondack Mountains and implications for their geologic evolutionGeology, 1988
- Pressure-Temperature-Time Paths and a Tectonic Model for the Evolution of GranulitesThe Journal of Geology, 1987
- The Archaean geological evolution of Enderby Land, AntarcticaGeological Society, London, Special Publications, 1987
- Evidence for the stability of the potential nuclear waste host, sphene, over geological time, from uranium-lead ages and uranium-series measurementsApplied Geochemistry, 1986
- Pre-Grenvillian history of the Adirondacks as an anorogenic, bimodal caldera complex of mid-Proterozoic ageGeology, 1986
- Oxygen isotope evidence for shallow emplacement of Adirondack anorthositeNature, 1982
- Akermanite in the Cascade Slide xenolith and its significance for regional metamorphism in the AdirondacksContributions to Mineralogy and Petrology, 1980
- Isotopic lead ages of chondritic meteoritesEarth and Planetary Science Letters, 1973