[meteorite-list] Ureilite Origins

2004-09-06 Thread bernd . pauli
 They had to have been carbonaceous meteorites of some sort to begin
 with, but the articles I've seen don't seem to offer a clear picture
 of what they were like before they were shocked. CM, perhaps?


Hello Marc, Frédéric, and List,

Here is what I've harvested during the last few minutes:


Cyrena Anne Goodrich, Lunar and Planetary
Laboratory, University of Arizona

Invited Review - Ureilites: A critical review
(Meteoritics 27-4, 1992, pp. 327-352):

1) Nilpena contains clasts of carbonaceous chondrite matrix material.
   Detailed petrographic and mineralogic studies have shown that this
   material has close affinities to CI - and differs substantially from
   CM-matrix (Brearley and Prinz, 1989; 1992).

Frédéric, close affinities to CI would also explain why we do not find any
chondrules or relict chondrules in ureilites - there have never been any.

But, ... now look at this - it is from the same review by C.A. Goodrich:

2) CI-matrix clasts in Nilpena have an oxygen-isotope composition plotting
   on the extension of the Allende mixing line on the 17^O-rich side of the
   terrestrial fractionation line, rather than within the field of CI matrix
   compositions (Brearley and Prinz, 1992).

So the starting material may have been CI-   o r   CV-like. If it was CV-like, we
might really expect to find traces of chondrules or at least chondrule precursor
material.

Best wishes,

Bernd

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Re: [meteorite-list] Ureilite Origins

2004-09-06 Thread meteoriteshow
Thanks for your response Bernd!
As far as CI are concerned, yes they have no chondrule and I did not think
of them before writing my e-mail. But then the oxygen-isotope study is
getting us confused... CV?...
As far as I know, there was no evidence of presolar diamonds existence. Am I
right or wrong? Should they exist, and should one find some in a Ureilite,
what can we expect then about the origin of those meteorites?
I know that some studies are on rails both in France and Japan about
Ureilites, so let's hope that they will bring some answers...
Cheers,
Fred

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From: [EMAIL PROTECTED]
To: [EMAIL PROTECTED]
Sent: Monday, September 06, 2004 8:31 PM
Subject: [meteorite-list] Ureilite Origins


 They had to have been carbonaceous meteorites of some sort to begin
 with, but the articles I've seen don't seem to offer a clear picture
 of what they were like before they were shocked. CM, perhaps?


Hello Marc, Frédéric, and List,

Here is what I've harvested during the last few minutes:


Cyrena Anne Goodrich, Lunar and Planetary
Laboratory, University of Arizona

Invited Review - Ureilites: A critical review
(Meteoritics 27-4, 1992, pp. 327-352):

1) Nilpena contains clasts of carbonaceous chondrite matrix material.
   Detailed petrographic and mineralogic studies have shown that this
   material has close affinities to CI - and differs substantially from
   CM-matrix (Brearley and Prinz, 1989; 1992).

Frédéric, close affinities to CI would also explain why we do not find any
chondrules or relict chondrules in ureilites - there have never been any.

But, ... now look at this - it is from the same review by C.A. Goodrich:

2) CI-matrix clasts in Nilpena have an oxygen-isotope composition plotting
   on the extension of the Allende mixing line on the 17^O-rich side of the
   terrestrial fractionation line, rather than within the field of CI matrix
   compositions (Brearley and Prinz, 1992).

So the starting material may have been CI-   o r   CV-like. If it was
CV-like, we
might really expect to find traces of chondrules or at least chondrule
precursor
material.

Best wishes,

Bernd

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Re: [meteorite-list] Ureilite Origins

2004-09-06 Thread Kashuba, Ontario, California
Bernd and List,
Aside from the origin of ureilites, it appears that traces of chondrules are 
found in polymict ureilites and are probably from impactors - like the 
chondrules sometimes found in howardites.  See Mr. Weir's page on DaG 319. 
I might be lucky enough to have a thin section of DaG 319 that contains a 
chondrule.  Tell me what you think.

http://www.johnkashuba.com/Ach_DaG_319_Ureilite_-_Polymict.html
Regards,
John  Kashuba
Ontario, California
- Original Message - 
From: [EMAIL PROTECTED]
To: [EMAIL PROTECTED]
Sent: Monday, September 06, 2004 11:31 AM
Subject: [meteorite-list] Ureilite Origins


They had to have been carbonaceous meteorites of some sort to begin
with, but the articles I've seen don't seem to offer a clear picture
of what they were like before they were shocked. CM, perhaps?

Hello Marc, Frédéric, and List,
Here is what I've harvested during the last few minutes:
Cyrena Anne Goodrich, Lunar and Planetary
Laboratory, University of Arizona
Invited Review - Ureilites: A critical review
(Meteoritics 27-4, 1992, pp. 327-352):
1) Nilpena contains clasts of carbonaceous chondrite matrix material.
  Detailed petrographic and mineralogic studies have shown that this
  material has close affinities to CI - and differs substantially from
  CM-matrix (Brearley and Prinz, 1989; 1992).
Frédéric, close affinities to CI would also explain why we do not find any
chondrules or relict chondrules in ureilites - there have never been any.
But, ... now look at this - it is from the same review by C.A. Goodrich:
2) CI-matrix clasts in Nilpena have an oxygen-isotope composition plotting
  on the extension of the Allende mixing line on the 17^O-rich side of the
  terrestrial fractionation line, rather than within the field of CI matrix
  compositions (Brearley and Prinz, 1992).
So the starting material may have been CI-   o r   CV-like. If it was 
CV-like, we
might really expect to find traces of chondrules or at least chondrule 
precursor
material.

Best wishes,
Bernd
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