A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2019; you can also visit the original URL.
The file type is application/pdf
.
The olivine-clinopyroxene geobarometer: implication for the thermal structure of the upper mantle near the Rio Grande Rift
International Kimberlite Conference Extended Abstracts: 1982
unpublished
temperature and pressure range from 900°C to 1300°C and 10Kb to 15Kb, respectively. Systematic compositional variations have been introduced by varying the composition of the reactants in the following synthesizing reaction.
doi:10.29173/ikc2289
fatcat:yh2jtspl2ventfysukv76km3te