[meteorite-list] 3rd attempt
From: Matson, Robert <ROBERT.D.MATSON_at_meteoritecentral.com>
Date: Thu Apr 22 10:31:15 2004 Message-ID: <AF564D2B9D91D411B9FE00508BF1C86904EE5B7E_at_US-Torrance.mail.saic.com> This message is in MIME format. Since your mail reader does not understand this format, some or all of this message may not be legible. ------_=_NextPart_001_01C42763.DE2F2536 Content-Type: text/plain; charset="iso-8859-1" Hi All, This is getting frustrating, but I think I've figured out a pattern to which posts make it to Met Central, and which ones go to the twilight zone. I guess I'll know in a moment. I'm sending this message to BOTH 'meteorite-list-admin_at_meteoritecentral.com' and 'meteorite-list_at_meteoritecentral.com', as the latter by itself is clearly insufficient. --Rob - - - - -----Original Message----- From: Matson, Robert Sent: Monday, April 19, 2004 8:29 PM To: 'BOORX4_at_aol.com'; meteorite-list@meteoritecentral.com Subject: Meteorite pairing Hi Bob, > Could some knowledgeable list member please describe or give a definition > as to what "Meteorite Pairing" or "Paired Meteorites" exactly is. I have > a vague idea but would like to have a better understanding. The simplest definition is the process whereby it can be reasonably determined that two or more distinct meteorites or meteorite fragments are part of the same fall -- more specifically, that they were all once part of a single body immediately prior to entering the earth's atmosphere. I can think of at least three ways that one can "pair" meteorites. The most reliable is physical pairing: two fragments that can be unambiguously pieced together. Less reliable is proximity pairing (and in many areas this method is quite unreliable without additional evidence). A third pairing technique is by classification (typically coupled with proximity). The reliability of this method really depends on the rarity of the meteorite type. Two weathered H5s found 50 feet apart is obviously not as reliable as two fresh CV3s found a mile apart. I suppose a 4th method would be based on classification alone, though this would be limited to specimens which have something sufficiently distinctive about them (e.g. a fresh fall like Park Forest would certainly qualify). For common meteorite types (H, L, LL), petrologic grade, weathering, shock, fayalite and ferrosilite percentages generally would not be sufficient. Cheers, Rob ------_=_NextPart_001_01C42763.DE2F2536 Content-Type: text/html; charset="iso-8859-1" Content-Transfer-Encoding: quoted-printable <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 3.2//EN"> <HTML> <HEAD> <META HTTP-EQUIV=3D"Content-Type" CONTENT=3D"text/html; = charset=3Diso-8859-1"> <META NAME=3D"Generator" CONTENT=3D"MS Exchange Server version = 5.5.2657.71"> <TITLE>3rd attempt</TITLE> </HEAD> <BODY> <P><FONT SIZE=3D2>Hi All,</FONT> </P> <P><FONT SIZE=3D2>This is getting frustrating, but I think I've figured = out a pattern</FONT> <BR><FONT SIZE=3D2>to which posts make it to Met Central, and which = ones go to the</FONT> <BR><FONT SIZE=3D2>twilight zone. I guess I'll know in a = moment. I'm sending this</FONT> <BR><FONT SIZE=3D2>message to BOTH = 'meteorite-list-admin_at_meteoritecentral.com' and</FONT> <BR><FONT SIZE=3D2>'meteorite-list_at_meteoritecentral.com', as the latter = by itself is</FONT> <BR><FONT SIZE=3D2>clearly insufficient. --Rob</FONT> </P> <P><FONT SIZE=3D2>- - - -</FONT> </P> <P><FONT SIZE=3D2>-----Original Message-----</FONT> <BR><FONT SIZE=3D2>From: Matson, Robert</FONT> <BR><FONT SIZE=3D2>Sent: Monday, April 19, 2004 8:29 PM</FONT> <BR><FONT SIZE=3D2>To: 'BOORX4_at_aol.com'; = meteorite-list_at_meteoritecentral.com</FONT> <BR><FONT SIZE=3D2>Subject: Meteorite pairing</FONT> </P> <P><FONT SIZE=3D2>Hi Bob,</FONT> <BR><FONT SIZE=3D2> </FONT> <BR><FONT SIZE=3D2>> Could some knowledgeable list member please = describe or give a definition</FONT> <BR><FONT SIZE=3D2>> as to what "Meteorite Pairing" or = "Paired Meteorites" exactly is. I have</FONT> <BR><FONT SIZE=3D2>> a vague idea but would like to have a = better understanding. </FONT> <BR><FONT SIZE=3D2> </FONT> <BR><FONT SIZE=3D2>The simplest definition is the process whereby it = can be reasonably determined that two or more distinct meteorites or = meteorite fragments</FONT></P> <P><FONT SIZE=3D2>are part of the same fall -- more specifically, that = they were all once</FONT> <BR><FONT SIZE=3D2>part of a single body immediately prior to entering = the earth's atmosphere.</FONT> <BR><FONT SIZE=3D2> </FONT> <BR><FONT SIZE=3D2>I can think of at least three ways that one can = "pair" meteorites. The</FONT> <BR><FONT SIZE=3D2>most reliable is physical pairing: two = fragments that can be unambiguously</FONT> <BR><FONT SIZE=3D2>pieced together. Less reliable is proximity = pairing (and in many areas</FONT> <BR><FONT SIZE=3D2>this method is quite unreliable without additional = evidence). A third</FONT> <BR><FONT SIZE=3D2>pairing technique is by classification (typically = coupled with proximity).</FONT> <BR><FONT SIZE=3D2>The reliability of this method really depends on the = rarity of the</FONT> <BR><FONT SIZE=3D2>meteorite type. Two weathered H5s found 50 = feet apart is obviously not</FONT> <BR><FONT SIZE=3D2>as reliable as two fresh CV3s found a mile = apart.</FONT> <BR><FONT SIZE=3D2> </FONT> <BR><FONT SIZE=3D2>I suppose a 4th method would be based on = classification alone, though</FONT> <BR><FONT SIZE=3D2>this would be limited to specimens which have = something sufficiently</FONT> <BR><FONT SIZE=3D2>distinctive about them (e.g. a fresh fall like Park = Forest would certainly</FONT> <BR><FONT SIZE=3D2>qualify). For common meteorite types (H, L, = LL), petrologic grade,</FONT> <BR><FONT SIZE=3D2>weathering, shock, fayalite and ferrosilite = percentages generally would</FONT> <BR><FONT SIZE=3D2>not be sufficient.</FONT> <BR><FONT SIZE=3D2> </FONT> <BR><FONT SIZE=3D2>Cheers,</FONT> <BR><FONT SIZE=3D2>Rob</FONT> </P> </BODY> </HTML> ------_=_NextPart_001_01C42763.DE2F2536-- Received on Wed 21 Apr 2004 01:47:58 AM PDT |
StumbleUpon del.icio.us Yahoo MyWeb |