MINERALOGY OF TAGISH LAKE: AN UNGROUPED TYPE 2 CARBONACEOUS CHONDRITE

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dc.contributor.author Zolensky M.E.
dc.contributor.author Nakamura K.
dc.contributor.author Gounelle M.
dc.contributor.author Mikouchi T.
dc.contributor.author Kasama T.
dc.contributor.author Tachikawa O.
dc.contributor.author Tonui E.
dc.date.accessioned 2021-05-28T08:26:43Z
dc.date.available 2021-05-28T08:26:43Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=14247790
dc.identifier.citation Meteoritics and Planetary Science, 2002, 37, 5, 737-761
dc.identifier.issn 1086-9379
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/28731
dc.description.abstract In this paper we describe the recovery, handling and preliminary mineralogical investigation of the Tagish Lake meteorite. Tagish Lake is a type 2 carbonaceous chondrite which bears similarities to CI1 and CM chondrite groups, but is distinct from both. Abundant phyllosilicates as well as chondrules (however sparse) and common olivine grains in the matrix preclude any other classification. The bulk density of Tagish Lake (1.67 g/cc) is far lower than CI or CM chondrites (2.2-2.3 and 2.6-2.9 g/cc, respectively), or any other meteorite for that matter. We have identified two lithologies: a dominant carbonate-poor lithology and a less-abundant carbonate-rich lithology. The meteorite is a breccia at all scales. We have noted similarities between Tagish Lake and some clasts within the enigmatic meteorite Kaidun; possibly there are genetic relationships here worth exploring. In the paper we describe a clast of CM1 material within Tagish Lake which is very similar to a major lithology in Kaidun.
dc.title MINERALOGY OF TAGISH LAKE: AN UNGROUPED TYPE 2 CARBONACEOUS CHONDRITE
dc.type Статья


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