All Stories

  1. In situ measurements of lead and other trace elements in abyssal peridotite sulfides
  2. Testing constitutive equations for brittle-ductile deformation associated with faulting in granitic rock
  3. Comparison of thermal modeling, microstructural analysis, and Ti-in-quartz thermobarometry to constrain the thermal history of a cooling pluton during deformation in the Mount Abbot Quadrangle, CA
  4. Effect of latent heat of freezing on crustal generation at low spreading rates
  5. Crustal shortening, exhumation, and strain localization in a collisional orogen: The Bajo Pequeño Shear Zone, Sierra de Pie de Palo, Argentina
  6. Evaluation of transtension and transpression within contractional fault steps: Comparing kinematic and mechanical models to field data
  7. The influence of water and LPO on the initiation and evolution of mantle shear zones
  8. Abyssal peridotites reveal the near-chondritic Fe isotopic composition of the Earth
  9. Helium distribution in a mantle shear zone from the Josephine Peridotite
  10. Lead and osmium isotopic constraints on the oceanic mantle from single abyssal peridotite sulfides
  11. The influence of deformation history on the interpretation of seismic anisotropy
  12. Executive Summary: “Mantle Frontier” Workshop
  13. Cryptic Variations in Abyssal Peridotite Compositions: Evidence for Shallow-level Melt Infiltration in the Oceanic Lithosphere
  14. Mantle Melting, Melt Transport, and Delivery Beneath a Slow-Spreading Ridge: The Paleo-MAR from 23 15'N to 23 45'N
  15. An assessment of upper mantle heterogeneity based on abyssal peridotite isotopic compositions
  16. Microstructural and Rheological Evolution of a Mantle Shear Zone
  17. Mantle deformation and noble gases: Helium and neon in oceanic mylonites
  18. Evolution of olivine lattice preferred orientation during simple shear in the mantle
  19. Correlation of seismic and petrologic thermometers suggests deep thermal anomalies beneath hotspots
  20. Pyroxenites from the Southwest Indian Ridge, 9-16 E: Cumulates from Incremental Melt Fractions Produced at the Top of a Cold Melting Regime
  21. Grain size sensitive deformation mechanisms in naturally deformed peridotites