Thermal evolution of convergent plate margins: Thermal modeling and reevaluation of isotopic AR‐ages for Blueschists in the Franciscan Complex of California
- 1 August 1985
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 4 (5) , 421-433
- https://doi.org/10.1029/tc004i005p00421
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Comparative Study of Melange Matrix and Metashales from the Franciscan Subduction Complex With the Basal Great Valley Sequence, CaliforniaThe Journal of Geology, 1983
- Uranium‐lead isotopic ages from the Sierra Nevada Batholith, CaliforniaJournal of Geophysical Research, 1982
- Seismicity of the forearc marginal wedge (accretionary prism)Journal of Geophysical Research, 1982
- Petrologic, structural, and age relations of serpentinite, amphibolite, and blueschist in the Shuksan Suite of the Iron Mountain–Gee Point area, North Cascades, WashingtonGSA Bulletin, 1982
- Flow melanges: Numerical modeling and geologic constraints on their origin in the Franciscan subduction complex, CaliforniaGSA Bulletin, 1982
- Optical Determination of Topotactic Aragonite-Calcite Growth Kinetics: Metamorphic ImplicationsThe Journal of Geology, 1981
- Phase relations of pyroxene and amphibole in greenstone, blueschist and eclogite of the Franciscan Complex, CaliforniaContributions to Mineralogy and Petrology, 1979
- Stress and temperature in subduction shear zones: Tonga and MarianaGeophysical Journal International, 1978
- South Fork Mountain Schist at Black Butte and Cottonwood Creek, northern CaliforniaGeology, 1977
- Phytoclasts as Indicators of Thermal Metamorphism, Franciscan Assemblage and Great Valley Sequence (Upper Mesozoic), CaliforniaPublished by Geological Society of America ,1974