Do meteoroids of sedimentary origin survive terrestrial atmospheric entry?: The ESA artificial meteorite experiment STONE

被引:31
作者
Brack, A
Baglioni, P
Borruat, G
Brandstätter, F
Demets, R
Edwards, HGM
Genge, M
Kurat, G
Miller, MF
Newton, EM
Pillinger, CT
Roten, CA
Wäsch, E
机构
[1] CNRS, Ctr Biophys Mol, F-45071 Orleans 2, France
[2] European Space Technol Ctr, NL-2200 AG Noordwijk, Netherlands
[3] Univ Lausanne, Fac Med, Inst Genet & Biol Microbiennes, CH-1005 Lausanne, Switzerland
[4] Nat Hist Museum, A-1014 Vienna, Austria
[5] Univ Bradford, Dept Chem & Forens Sci, Bradford BD7 1DP, W Yorkshire, England
[6] Nat Hist Museum, Dept Mineral, London SW7 5BD, England
[7] Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
[8] Humboldt Univ, Museum Nat, D-10115 Berlin, Germany
关键词
artificial meteorites; atmospheric entry; dolomite; Martian sediments; isotopes;
D O I
10.1016/S0032-0633(02)00018-1
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The 18 SNC meteorites identified to date are all igneous rocks, being basalts or basaltic cumulates. The lack of sedimentary rocks in this inventory is therefore surprising, in view of the collisional history of Mars and the likelihood that Mars experienced warmer conditions, possibly with a significant hydrosphere, earlier in its history. To address the possibility that sedimentary rocks ejected by impact from the surface of Mars may have reached the Earth, but did not survive terrestrial atmospheric entry, an experiment was performed in which samples of dolomite, a simulated Martian regolith (consisting of basalt fragments in a gypsum matrix) and a basalt were fixed to the heat shield of a recoverable capsule and flown in low Earth orbit. Temperatures attained during re-entry were high enough to melt basalt and the silica fibres of the heat shield and were therefore comparable to those experienced by meteorites. The dolomite sample survived space flight and atmospheric re-entry, in part, as did fragments of the simulated Martian regolith, allowing detailed examinations of these,artificial meteorites' to be conducted for chemical, mineralogical and isotopic modifications associated with atmospheric re-entry. Oxygen three-isotope measurements of the silica 'fusion crust' formed on the sample holder during atmospheric re-entry fit on a mixing line, with tropospheric O-2 and the interior of the sample holder as end members. Because much of the surface of Mars is covered by clastic sediments, meteorites of Martian provenance might be expected to be mostly sedimentary rocks rather than igneous ones. However, in the absence of a readily identifiable fusion crust, the extraterrestrial origin of such sedimentary rocks on Earth would most probably not be recognised without detailed petrological-geochemical examination and, ultimately, isotope measurements. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:763 / 772
页数:10
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