[meteorite-list] NWA 482
From: Dennis Beatty <apollocollector_at_meteoritecentral.com>
Date: Tue, 26 Jan 2010 11:37:47 -0800 Message-ID: <BLU0-SMTP9887C39D9F4139786D5AE1B65E0_at_phx.gbl> Is there any reason to believe that one side might be more prone to impacts than the other?? Dennis Beatty On Jan 26, 2010, at 11:14 AM, Randy Korotev wrote: > At 00:54 26-01-10 Tuesday, you wrote: >> Randy, why did you write that there is no scientific evidence that >> any particular lunar meteorite originates from the lunar farside? > > > Dear Walter and list: > > We don't know exactly where on the Moon any lunar meteorite comes > from. It has, nevertheless, become fashionable, if not obligatory, > for lunar meteorite scientists to speculate where a new lunar > meteorite might come from in a regional sense when they write papers > about them. I've done it myself. > > The people who understand the dynamics of these things tell me that > the chance of having a rock achieve escape velocity from the farside > is the same as from the nearside. Any rock that leaves the Moon has > the same chance of landing on Earth. Some of this is discussed in a > recent (and much too long) paper: > > http://epsc.wustl.edu/~rlk/papers/korotev_et_al_2009_m&ps_intermediate_iron.pdf > > To me this all means that half the lunar meteorites must come from > the farside, we just don't know which ones. > > What we do know is that NWA 482 is highly feldspathic (~80% > plagioclase) and poor in radioactive elements like Th (thorium). We > know from orbital measurements that a larger fraction of the surface > material on the farside is feldspathic and low in Th than for the > nearside. The nearside has more basalts and most of the Th-rich > stuff. So, on the basis of chemical composition, NWA 482 has a >50% > chance of being from the farside. But, the same argument applies to > the other 32 feldspathic lunar meteorites. Surely, some feldspathic > lunar meteorites come from the nearside. NWA 4936/5406, for > example, is very similar in composition to soil from the Apollo 16 > site on the nearside. > > The corresponding argument is that most of the basaltic (lun-b) > meteorites come from the nearside because most of the mare basalts > are exposed on the nearside. We also can say that Th-rich > meteorites like SaU 169 and Dhofar 1442 must come the anomalously Th- > rich region in the northwest quadrant of the nearside known as the > Procellarum KREEP Terrane. But again, the source crater for none of > the lunar meteorites has been established with certainty. An impact > making a 1-km-crater can launch a lunar meteorite. > > Randy Korotev > > > ______________________________________________ > Visit the Archives at http://www.meteoritecentral.com/mailing-list-archives.html > Meteorite-list mailing list > Meteorite-list at meteoritecentral.com > http://six.pairlist.net/mailman/listinfo/meteorite-list > Received on Tue 26 Jan 2010 02:37:47 PM PST |
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