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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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