Posted by jbridges in Mars Science Laboratory Blog on July 30, 2015
We have started drilling at Belkin, first a minidrill hole before the main drill hole. Belkin has been chosen because this sedimentary horizon has some very high silica enrichments. That may have occurred as the Gale sediments were altered by subsurface fluids after burial. As the basaltic composition was altered (as we saw from the clay and Fe oxide at Yellowknife Bay) ultimately a lot of silica is released which can be precipitated at horizons like this.
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About jbridges
This blog is a record of my experiences and work during the Mars Science Laboratory mission, from the preparation, landing on August 5th 2012 Pacific Time, and onwards...
I will also post updates about our other Mars work on meteorites, ExoMars and new missions. You can also follow the planetary science activities with @LeicsPlanets
Professor John Bridges, School of Physics and Astronomy
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