>From what Serge told me, only a small piece of the original iron was analyzed; therefore, the olivines were probably missed. Many of the slabs contain regions completely devoid of olivine, these remind me of the Glorieta and Brenham masses in appearance. The etch of these do not look like Brahin. So I do not think that is it. Plus Serge is an honest man and showed me where these pieces were found. Matt
-----Original Message----- From: [EMAIL PROTECTED] [mailto:[EMAIL PROTECTED] On Behalf Of Jörn Koblitz Sent: Monday, September 20, 2004 6:12 AM To: mark ford; Meteorite List Subject: AW: [meteorite-list] Seymchan Pallasite Hello Mark and List, here is an extract from MetBase on Seymchan: ------------------------------------------------------- A mass of 272.3kg was found in the bed of a stream flowing into the river Hekandue, a tributary of the Jasachnaja, a second mass of 51kg was later found at a distance of 20 m from the first one, Met. Bull. 42, 43, Meteoritics, 1970, 5, p.97; see also, A.L.Graham et al., Cat. Met., 1985, p.323. The coordinates are of the town of Seymchan. Find circumstances, V.I.Tsvetkov, Meteoritika, 1969, 29, p.152. Illustrated description, with an analysis, 9.47% Ni, O.A.Kirova and M.I.Dyakonova, Meteoritika, 1972, 31, p.104. Further analysis, 9.15% Ni, 24.6 ppm Ga, 68.3 ppm Ge, 0.55 ppm Ir, E.R.D.Scott and J.T.Wasson, GCA, 1976, 40, p.103. Further INAA data, previously classified into the IIE group, but now designated ungrouped based on the chemical composition, J.T.Wasson and J.Wang, GCA, 1986, 50, p.725. Another analysis, A.N.Krot et al., Meteoritics, 1992, 27, p.465. Nitrogen isotopic composition, R.L.Palma et al., LPSC, 1997, 28, p.1057 (abs.); see also, K.Marti et al., MAPS, 1997, 32, p.A84 (abs.); K.J.Mathew et al., GCA, 2000, 64, p.545. ------------------------------------------------------- Acording to the more recent analysis by Wasson and Chang (1986), the metal of Seymchan is ungrouped, thus cannot be related to - at least - the main-group pallasites (e.g. Brenham, Esquel, Imilac) which are genetically linked to IIIAB irons. So, may be we have a new kind of pallasite here (exotic like e.g. Eagle Station)! On the other hand, rounded silicate inclusions are commonly found in IIE irons like Miles, Elga, or Kodaikanal. Thus, it is well possible to mix such silicated irons up with pallasites and Seymchan is actually an ungrouped silicated iron. Best regards, Jörn ________________________________________________________________________ _______ Joern Koblitz MetBase Editor The MetBase Library of Meteoritics and Planetary Sciences Benquestrasse 27 D-28209 Bremen, Germany phone: +49 421 24 100 24 fax: +49 421 168 2799 email: [EMAIL PROTECTED] ________________________________________________________________________ _______ > -----Ursprüngliche Nachricht----- > Von: mark ford [mailto:[EMAIL PROTECTED] > Gesendet: Montag, 20. September 2004 10:54 > An: Meteorite List > Betreff: RE: [meteorite-list] Seymchan Pallasite > > > > Hi, > > Anyone got a link to any classification details for this seymchan > pallasite? > > Looks quite interesting, very sharp Olivine pieces.... > > Best > Mark > ______________________________________________ > Meteorite-list mailing list [EMAIL PROTECTED] > http://six.pairlist.net/mailman/listinfo/meteorite-list > ______________________________________________ Meteorite-list mailing list [EMAIL PROTECTED] http://six.pairlist.net/mailman/listinfo/meteorite-list ______________________________________________ Meteorite-list mailing list [EMAIL PROTECTED] http://six.pairlist.net/mailman/listinfo/meteorite-list