Not exact matches
A study led by Eleonora Ammannito
of the University
of California, Los Angeles, finds that clay - forming minerals called
phyllosilicates are all over Ceres.
To satisfy microbial nutritional fitness, the research team uses mineral mixtures that mimic the Martian regolith composition from different locations and historical periods
of Mars: «JSC 1A» is mainly composed
of palagonite — a rock that was created by lava; «P - MRS» is rich in hydrated
phyllosilicates; the sulfate containing «S - MRS,» emerging from acidic times on Mars and the highly porous «MRS07 / 52» that consists
of silicate and iron compounds and simulates sediments
of the Martian surface.
It first detected clays (technically called
phyllosilicates) last year, but the data were spotty, and some scientists wondered whether the clays were merely superficial layers, the result
of gradual weathering rather than thorough soaking.
Mineralogist Richard Morris
of the NASA Johnson Space Center says, «For something as important as
phyllosilicates, I'd like to see two things point to it» — that is, two independent lines
of evidence.
One
of these,
phyllosilicate, forms as liquid water interacts with volcanic rock over thousands
of years.
One
of the surprises found on Ceres was the presence
of ammonia in the
phyllosilicates.
Like the fine grains sampled in the Aru avalanche debris, Martian dust is talcum powder - sized particles
of platy
phyllosilicate minerals.
Last year, in a Nature study, De Sanctis» team reported that the surface
of Ceres contains ammoniated
phyllosilicates, or clays containing ammonia.
Phyllosilicates are clay - like minerals, formed in the presence
of a neutral - pH water, and are indicative
of a habitable environment.
This shallow angle would have permitted some
of the ejected material from the collision to fall back on the surface, spraying it with the observed
phyllosilicate traces.
Bentonite is a
phyllosilicate that does a lot
of good to the skin and the fur
of your pets.
Faults (contrary to very popular theory needs) are always lubricated to some degree by a combination
of, pore space water under pressure,
phyllosilicate clay slurry (lots
of it), lubricant metals like molybdenum (some - usually emplaced in hydrothermal processes
of transport and atom precipitation with changes in pressure) and especially by copious amounts
of «massive» (i.e. solid) graphite, that's almost always is present in fault surface,