By
comparing rock samples from those sources with the depleted ash, the team was able to calculate how much phosphorus, iron and silica were missing.
Not exact matches
Wang and Jacobsen examined seven lunar
rock samples from different lunar missions and
compared their potassium isotope ratios to those of eight terrestrial
rocks representative of Earth's mantle.
To evaluate each influence 3.26 billion years ago, geoscience Professor Clark Johnson and Satkoski collected
samples from South Africa and
compared isotopes in two forms of a
rock called barite.
Using
samples collected from the Liwu and Wulu river basins in Taiwan, which run off the central range, the team
compared the radiocarbon profiles of organic carbon in the
rock with the soil directly above it.
But when his team
compared DNA sequences from the bacteria in the
rock samples with those available in databases, he discovered an entire microbial ecosystem consisting of a wide variety of both archaebacteria and eubacteria, common «modern» bacteria that normally take up residence in lush places such as cheese and humans.
Team members then extrapolated to Mercury a model that was originally developed for
comparing the Moon's crater distribution to a chronology based on the ages of
rock samples gathered during the Apollo missions.