All abstracts by Sarah Penniston-Dorland in conference series: Goldschmidt
(2020) Archean Surface-Derived Contamination in the Plume Source of the Paleoproterozoic Bushveld Large Igneous ProvinceBybee G, Hayes B, Magalhães N, Zirakparvar A, Farquhar J, Wu N, Penniston-Dorland S, Feineman M & Leach T
(2019) Stopping Crystal Clocks: The Role of Electrons in Arresting Diffusion of Lithium in Subduction Zone Garnets
Penniston-Dorland S, Baumgartner L, Dragovic B & Bouvier A-S
(2019) Comparison of Single-Phase Thermobarometers and their Application to Reconstructing the Tectonometamorphic Evolution of the Rio San Juan Complex (Dominican Republic)
Harvey K, Dragovic B, Penniston-Dorland S, Piccoli P & Bodnar R
(2018) Anomalous Sulfur of the Waterberg Project of the Bushveld Complex is not Locally Derived
Magalhaes N, Penniston-Dorland S, Bybee G, Farquhar J & McCreesh M
(2018) Crustal-Lithospheric Processes Recorded at the 2.06 Ga Bushveld-Molopo Farms Igneous Complex
Feineman M, Magalhaes N, Penniston-Dorland S & Bybee G
(2018) Evidence from in situ Measurements of δ7Li in Garnets Suggests Control of Subduction Fluid Composition on Li Isotopic Fractionation within Garnet
Penniston-Dorland S, Baumgartner L, Dragovic B & Bouvier A-S
(2016) A Mélange of Subduction Temperatures: Zr-in-Rutile Thermometry of the Catalina Schist
Penniston-Dorland S, Kohn M & Piccoli P
(2015) The Global Range of Subduction Zone Thermal Structures from Exhumed Blueschists and Eclogites: Rocks are Hotter Than Models
Penniston-Dorland S, Kohn M & Manning C
(2014) A Mélange of Subduction Temperatures: Zr-in-Rutile Thermometry and the Nature of the Slab-Mantle Interface
Penniston-Dorland S, Kohn M & Piccoli P
(2013) Formation Mechanisms of Reaction Zones in Mélange Zones: Evidence for Mechanical Mixing
Gorman J, Penniston-Dorland S, Walker R & Marschall H
(2012) Equilibrium Partitioning of Li between Olivine and Clinopyroxene at Mantle Conditions
Deane J, Feineman M, Yakob J, Eggler D & Penniston-Dorland S
(2011) Can Multiple Sulfur Isotopes be Used as a Tracer of Sub-Continental Lithospheric Mantle in the Bushveld?
Penniston-Dorland S, Farquhar J, Polley G, Mathez E & Kinnaird J
(2010) Highly Siderophile Elements as Tracers of Mantle-Crust Interactions in Subduction Zone Metamorphic Rocks: Evidence from the Franciscan Complex, CA
Penniston-Dorland S, Walker R, Pitcher L & Sorensen S
(2009) Oxygen Isotopic Exchange at a Contact between the Bushveld Complex and Meta-Sedimentary Rocks of the Phepane Dome
Potter R, Penniston-Dorland S & Valley J
(2009) Lithium as a Tracer of Fluids in Subduction Zones: The Franciscan Complex, CA
Penniston-Dorland S, Ash R, Piccoli P & Sorensen S
(2007) Mass-Independent Sulfur Isotopes Trace Magma-Wall Rock Interactions in the Bushveld Complex
Penniston-Dorland S, Wing B, Farquhar J, Brown M & Nex P
(2005) Coupled Dichotomies of Apatite and Fluid Composition in Contact Metamorphosed Siliceous Carbonates
Penniston-Dorland S & Ferry J