[meteorite-list] crust % ?

From: Jeff Kuyken <jeff_at_meteoritecentral.com>
Date: Thu Apr 22 10:17:38 2004
Message-ID: <000a01c3b8b3$136cf3b0$08378690_at_mandin4f89ypwu>

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I often think the same thing. The only problem then is determining the =
grade of the crust. Eg, fresh, weathered, partly weathered, discoloured =
etc. Not a bad idea though!!!

Cheers,

Jeff Kuyken
I.M.C.A. #3085
www.meteorites.com.au
www.meteoritesaustralia.com


  ----- Original Message -----=20
  From: mark ford=20
  To: meteorite-list_at_meteoritecentral.com=20
  Sent: Tuesday, December 02, 2003 7:40 PM
  Subject: [meteorite-list] crust % ?




  Hi,
  =20
  Regarding Fusion Crust; I have long argued for a 'fusion crust scale'
  (like the weathering & shock level scale) only for specifying =
individual
  specimens

  What about something like an 0-6 'FC' scale (FC=3DFusion Crust)

  FC 0 for none=20
     1 ~Tiny Piece of crust
     2 ~33%
     3 ~50% Fusion Crust
     4 ~66%
     5 ~83%
     6 ~100% All Fusion Crust


  Just a thought?

  Mark Ford



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<DIV><FONT size=3D2>I often think the same thing. The only problem then =
is=20
determining the grade of the crust. Eg, fresh, weathered, partly =
weathered,=20
discoloured etc. Not a bad idea though!!!</FONT></DIV>
<DIV><FONT size=3D2></FONT>&nbsp;</DIV>
<DIV><FONT size=3D2>Cheers,</FONT></DIV>
<DIV><FONT size=3D2></FONT>&nbsp;</DIV>
<DIV><FONT size=3D2>Jeff Kuyken<BR>I.M.C.A. #3085<BR><A=20
href=3D"http://www.meteorites.com.au">www.meteorites.com.au</A><BR><A=20
href=3D"http://www.meteoritesaustralia.com">www.meteoritesaustralia.com</=
A></FONT></DIV>
<DIV><FONT size=3D2></FONT>&nbsp;</DIV>
<DIV>&nbsp;</DIV>
<BLOCKQUOTE=20
style=3D"PADDING-RIGHT: 0px; PADDING-LEFT: 5px; MARGIN-LEFT: 5px; =
BORDER-LEFT: #000000 2px solid; MARGIN-RIGHT: 0px">
  <DIV style=3D"FONT: 10pt arial">----- Original Message ----- </DIV>
  <DIV=20
  style=3D"BACKGROUND: #e4e4e4; FONT: 10pt arial; font-color: =
black"><B>From:</B>=20
  <A title=3Dmarkf_at_ssl.gb.com href=3D"mailto:markf@ssl.gb.com">mark =
ford</A> </DIV>
  <DIV style=3D"FONT: 10pt arial"><B>To:</B> <A=20
  title=3Dmeteorite-list_at_meteoritecentral.com=20
  =
href=3D"mailto:meteorite-list_at_meteoritecentral.com">meteorite-list@meteor=
itecentral.com</A>=20
  </DIV>
  <DIV style=3D"FONT: 10pt arial"><B>Sent:</B> Tuesday, December 02, =
2003 7:40=20
  PM</DIV>
  <DIV style=3D"FONT: 10pt arial"><B>Subject:</B> [meteorite-list] crust =
% ?</DIV>
  <DIV><BR></DIV><BR><BR>Hi,<BR>&nbsp;<BR>Regarding Fusion Crust; I have =
long=20
  argued for a 'fusion crust scale'<BR>(like the weathering &amp; shock =
level=20
  scale) only for specifying individual<BR>specimens<BR><BR>What about =
something=20
  like an 0-6 'FC' scale (FC=3DFusion Crust)<BR><BR>FC 0 for none =
<BR>&nbsp;&nbsp;=20
  1 ~Tiny Piece of crust<BR>&nbsp;&nbsp; 2 ~33%<BR>&nbsp;&nbsp; 3 ~50% =
Fusion=20
  Crust<BR>&nbsp;&nbsp; 4 ~66%<BR>&nbsp;&nbsp; 5 ~83%<BR>&nbsp;&nbsp; 6 =
~100%=20
  All Fusion Crust<BR><BR><BR>Just a thought?<BR><BR>Mark=20
  =
Ford<BR><BR><BR><BR>-----------------------------------------------------=
-----------------------<BR>The=20
  information contained in this email may be commercially sensitive=20
  and/or<BR>legally privileged. It is intended solely for the person(s) =
to whom=20
  it is<BR>addressed. If you are not a named recipient, you are on =
notice of its=20
  status.<BR>Please notify the sender immediately by reply e-mail and =
then=20
  delete this<BR>message from your system. You must not disclose it to =
any other=20
  person,<BR>copy or distribute it or use it for any=20
  =
purpose.<BR><BR>______________________________________________<BR>Meteori=
te-list=20
  mailing list<BR><A=20
  =
href=3D"mailto:Meteorite-list_at_meteoritecentral.com">Meteorite-list@meteor=
itecentral.com</A><BR><A=20
  =
href=3D"http://www.pairlist.net/mailman/listinfo/meteorite-list">http://w=
ww.pairlist.net/mailman/listinfo/meteorite-list</A><BR><BR></BLOCKQUOTE><=
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Received on Tue 02 Dec 2003 04:02:51 AM PST


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