Experimental investigations have been conducted on the partition coefficients of first-transition row elements between olivine and silicate melt. Olivine is the first mineral to crystallize from basaltic magma, and accurate knowledge of olivine/melt partition coefficients (DOl–melt) for first-transition row elements (FTREs) Ga and Ge, is required in quantitative modeling of petrogenetic processes in planetary basalts. […]
/https://tf-cmsv2-smithsonianmag-media.s3.amazonaws.com/filer_public/d1/82/d18228f6-d319-4525-bb18-78b829f0791f/mammalevolution_web.jpg "How to Make a Mammal in Nine Evolutionary Steps")
;Resize=(1180) "WATCH | South Africa agrees to rescue illegal miners sealed for weeks underground")
This website uses cookies so that we can provide you with the best user experience possible. Cookie information is stored in your browser and performs functions such as recognising you when you return to our website and helping our team to understand which sections of the website you find most interesting and useful.
Discussion about this post