[meteorite-list] petrological type
From: Jim Wooddell <jim.wooddell_at_meteoritecentral.com>
Date: Sat, 12 Apr 2014 12:08:26 -0700 Message-ID: <53498F2A.5030100_at_suddenlink.net> Hi Alan and all, Is not the description/s part of the classification so that the researcher can better describe what is found without having to baffle over a number or preset definition that might...kind of...come close to what is found?? Jim On 4/12/2014 10:01 AM, Alan Rubin wrote: > Since Van Schmus and Wood (1967), the group/petrologic type designation has > been entrenched (i.e., LL3.0, H4, L6), that it would be impossible to purge. > So, calling Semarkona LL T3 just won't work -- no one would adopt it as a > new convention. If we wanted to call Semarkona LL3.00 A2.8, that might be > > okay, but you would have to convince people first that a two-tier system is > needed. It is probably best to exclude weathering and shock stage since we > > cannot designate every property in a classification (e.g., average olivine > > Fa content, cosmic-ray exposure age, oxygen-isotopic composition, chondrule > size, etc.). A problem of course is that it may be difficult to disentangle > thermal metamorphism from aqueous alteration, leaving a researcher baffled > > as to what to designate a particular rock. It would be better to leave out > a classificatory parameter and to just guess and have the rock > misclassified. > > Alan Rubin > Institute of Geophysics and Planetary Physics > University of California > 3845 Slichter Hall > 603 Charles Young Dr. E > Los Angeles, CA 90095-1567 > > office phone: 310-825-3202 > fax: 310-206-3051 > e-mail: aerubin at ucla.edu > website: http://cosmochemists.igpp.ucla.edu/Rubin.html > -- Jim Wooddell jim.wooddell at suddenlink.net http://pages.suddenlink.net/chondrule/Received on Sat 12 Apr 2014 03:08:26 PM PDT |
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