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Geophysical-Geochemical Modeling of Deep Crustal Compositions: Examples of Continental Crust in Typical Tectonic Settings and North China Craton
Cui, Shinevar, Guo, Xu, Zhang, & Jin
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WISTFUL: Whole-Rock Interpretative Seismic Toolbox for Ultramafic Lithologies
WJ Shinevar, O Jagoutz, MD Behn
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WISTFUL: Whole-Rock Interpretative Seismic Toolbox for Ultramafic Lithologies
Gore Mountain Garnet Amphibolite Records UHT Conditions: Implications for the Rheology of the Lower Continental Crust during Orogenesis
Our results on peak metamorphic P–T conditions based on thermobarometry, diffusion models, and thermodynamic modelling indicate that the Gore Mountain Megacrystic Amphibolite (GMGA) formed at ultrahigh-temperature (>900 °C) conditions (P = 9–10 kbar, T = 950 ± 40 °C), significantly hotter than previously estimated. Diffusion models pinned by nearby cooling ages require the GMGA to initially cool quickly (9·1 °C Ma–1), followed by slower cooling (2·6 °C Ma–1).
WJ Shinevar, O Jagoutz, JA VanTongeren
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Gore Mountain Garnet Amphibolite Records UHT Conditions: Implications for the Rheology of the Lower Continental Crust during Orogenesis
Formation and composition of the Late Cretaceous Gangdese arc lower crust in southern Tibet
L Guo, O Jagoutz, WJ Shinevar, HF Zhang
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Causes of oceanic crustal thickness oscillations along a 74‐M mid‐atlantic ridge flow line
WJ Shinevar, HF Mark, F Clerc, EA Codillo, JGong, JA Olive, SM Brown, PT Smalls, Y Liao, VLe Roux, MD Behn
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Inferring crustal viscosity from seismic velocity: Application to the lower crust of Southern California
WJ Shinevar, MD Behn, G Hirth, O Jagoutz
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Compositional dependence of lower crustal viscosity
WJ Shinevar, MD Behn, G Hirth
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