[meteorite-list] Finding fossil Meteorites
From: Chris Peterson <clp_at_meteoritecentral.com>
Date: Mon, 25 Oct 2010 15:05:21 -0600 Message-ID: <9F6AA1B883E049C9BC694068B8CD4A24_at_bellatrix> The fossil meteorites in question are Ordovician, L-chondrites that are mineralogically equivalent to around 20% of modern L-chondrites. All are presumed to have originated from a single asteroid collision event. Also interesting is that modern L-chondrites in this family have exposure ages close to the 480 million year old fossil meteorites. The suggestion is that a large population of fragments was generated, and some of these were injected into a fast track across Earth's orbit- something that has been modeled and found possible by considering orbital resonances in the Asteroid Belt caused by Jupiter. Also interesting is that the period of increased meteorite flux 480 million years ago corresponds to a simultaneous increase in global biodiversity. There have been some interesting talks on this subject at recent meteoritics conferences. Chris ***************************************** Chris L Peterson Cloudbait Observatory http://www.cloudbait.com ----- Original Message ----- From: "Yinan Wang" <veomega at gmail.com> To: <Meteorite-list at meteoritecentral.com> Sent: Monday, October 25, 2010 2:54 PM Subject: Re: [meteorite-list] Finding fossil Meteorites As a fossil collector, I can tell you that there are tons of meteor-wrongs in sedimentary rock. The main reason is that a lot of metallic concretions form in sedimentary rock diagenetically; hematite nodules, iron phosphates, pyrite concretions, marcasite, etc. So you would find good layers of limestone and then suddenly there's a meteorite-shaped nodule... But you guys know how to ID meteorites. For Count Deiro; here's a link to a geologic map of Nevada: http://geology.about.com/od/maps/ig/stategeomaps/NVgeomap.htm -Yinan Received on Mon 25 Oct 2010 05:05:21 PM PDT |
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