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Water in Meteorites - Part 1 of 2
Ron Baalke schrieb:
> Water has been extracted from several Martian meteorites before
Hello Michael, Ron, and List!
Here are some references:
G.Turner, R.Burgess et al. (1989) Is there Martian surface water in
Nakhla? (Meteoritics 24-4, 1989, A333).
CARR M. et al. (1992) Earth and Mars: Water inventories as clues to
accretional histories (Icarus 98, 61-71).
KARLSSON H.R. et al. (1992) Water in SNC meteorites: Evidence for a
Martian hydrosphere (Science, 255, 1409-1411).
WATSON L.L. et al. (1993) D/H ratios and water contents of amphiboles in
magmatic inclusions in Chassigny and Shergotty (Meteoritics 28-3, 1993,
A456).
WATSON L.L. et al. (1994) D/H of Water Released by Stepped Heating of
Shergotty, Zagami, Chassigny, ALH 84001 and Nakhla (Meteoritics 29-4,
1994, A547).
J. Maynard et al. (1996) The O isotopic composition of primitive water
in meteorites - A new approach (Meteoritics 31-4, 1996, A086).
BAKER L. et al. (1998) Oxygen isotopes in water from Martian meteorites
(Meteoritics 33-4, 1998, A011).
> I'm not sure when the first water samples was extracted from a
> meteorite, but it was probably from a carbonaceous chondrite. CI's
> have been known to have relatively [much] water in them, which is why
> some scientists suspect their parent body is a comet.
Some further references:
ANDERS E. (1975) Do stony meteorites come from comets? (Icarus 24,
363-371).
J.F.Kerridge et al. (1979) Aqueous alteration on asteroids: Evidence
from carbonaceous chondrites (in Asteroids by T.Gehrels, pp. 745-764).
R.E.Grimm et al. (1989) Water and the thermal evolution of carbonaceous
chondrite parent bodies (Icarus 82, 244-280).
R.E.Grimm, H.Y. McSween (1989) Water and the thermal evolution of
carbonaceous chondrite parent bodies (Meteoritics 24-4, 1989, A272).
E.Deloule et al. (1994) Interstellar Water in Meteorites? An in situ
Analysis by Ion Microprobe (Meteoritics 29-4, 1994, A459).
E. Deloule et al. (1995) Deuterium-rich water in meteorites (Meteoritics
30-5, 1995, A502).
> CI's have been known to have relatively [much] water in them,
> which is why some scientists suspect their parent body is a comet.
C.P. Hartmetz et al. (1988) Comparison of volatiles released from
carbonaceous chondrites and IDPs with Halley cometary volatiles
(Meteoritics, 1988-3, 23, A272).
CAMPINS H. and SWINDLE T.D.(1998) Expected characteristics of cometary
meteorites (MAPS 33-6, 1998, 1201-1211).
> CI's have been known to have relatively [much] water in them, ...
O.R. Norton, Rock From Space, 2nd ed. 1998, p. 193:
CI carbonaceous chondrites => "... they contain the highest percentage
of water - 20 percent - of any carbonaecous meteorite. When heated in a
closed container, the water is easily driven off and condenses on the
side of the enclosing vessel."
CM carbonaceous chondrites => "... contain less water than the CI group,
only about 10 percent, ..."
Best regards,
Bernd
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- Re: MONHANS
- From: Ron Baalke <BAALKE@kelvin.jpl.nasa.gov>