NOBLE-GASES IN PRESOLAR DIAMONDS .2. COMPONENT ABUNDANCES REFLECT THERMAL-PROCESSING

被引:164
作者
HUSS, GR [1 ]
LEWIS, RS [1 ]
机构
[1] UNIV CHICAGO,ENRICO FERMI INST,CHICAGO,IL 60637
来源
METEORITICS | 1994年 / 29卷 / 06期
关键词
D O I
10.1111/j.1945-5100.1994.tb01095.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Using the isotopic compositions derived in Huss and Lewis, 1994a (Paper I), abundances of the P3, HL, and P6 noble-gas components were determined for 15 diamond separates from primitive chondrites of 8 chondrite classes. Within a meteorite class, the relative abundances of these components correlate with the petrologic subtype of the host meteorite, indicating that metamorphism is primarily responsible for the variations. Relative abundances of P3, HL, and P6 among diamond samples can be understood in terms of thermal processing of a single mixture of diamonds like those now found in CI and CM2 chondrites. With relatively gentle heating, primitive diamonds first lose their low-temperature P3 gases and a ''labile'' fraction of the HL component. Mass loss associated with release of these components produces an increase in the HL and P6 content of the remaining diamond relative to unprocessed diamond. Higher temperatures initiate destruction of the main HL carrier, while the HL content of the surviving diamonds remains essentially constant. At the same time, the P6 carrier begins to preferentially lose light noble gases. Meteorites that have experienced metamorphic temperatures greater than or similar to 650 degrees C have lost essentially all of their presolar diamond through chemical reactions with surrounding minerals. The P3 abundance seems to be a function only of the maximum temperature experienced by the diamonds and thus is independent of the nature of the surrounding environment. If all classes inherited the same mixture of primitive diamonds, then P3 abundances would tie together the metamorphic scales in different meteorite classes. However, if the P3 abundance indicates a higher temperature than do other thermometers applicable to the host meteorite, then the P3 abundance may contain information about heating prior to accretion. Diamonds in the least metamorphosed EH, CV, and CO chondrites seem to carry a record of pre-accretionary thermal processing.
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页码:811 / 829
页数:19
相关论文
共 52 条
[1]   THE MICROSTRUCTURE OF SEMARKONA AND BISHUNPUR [J].
ALEXANDER, CMO ;
BARBER, DJ ;
HUTCHISON, R .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (11) :3045-3057
[2]   PRESOLAR COMPONENTS IN THE ORDINARY CHONDRITES [J].
ALEXANDER, CMO ;
ARDEN, JW ;
ASH, RD ;
PILLINGER, CT .
EARTH AND PLANETARY SCIENCE LETTERS, 1990, 99 (03) :220-229
[3]   INTERSTELLAR GRAPHITE IN METEORITES [J].
AMARI, S ;
ANDERS, E ;
VIRAG, A ;
ZINNER, E .
NATURE, 1990, 345 (6272) :238-240
[4]   UNEQUILIBRATED ORDINARY CHONDRITES - A TENTATIVE SUBCLASSIFICATION BASED ON VOLATILE-ELEMENT CONTENT [J].
ANDERS, E ;
ZADNIK, MG .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1985, 49 (05) :1281-1291
[5]   ORGANIC COMPOUNDS IN METEORITES [J].
ANDERS, E ;
HAYATSU, R ;
STUDIER, MH .
SCIENCE, 1973, 182 (4114) :781-790
[6]   INTERSTELLAR GRAINS IN PRIMITIVE METEORITES - DIAMOND, SILICON-CARBIDE, AND GRAPHITE [J].
ANDERS, E ;
ZINNER, E .
METEORITICS, 1993, 28 (04) :490-514
[7]   ABUNDANCES OF THE ELEMENTS - METEORITIC AND SOLAR [J].
ANDERS, E ;
GREVESSE, N .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (01) :197-214
[8]   INTERSTELLAR GRAINS WITHIN INTERSTELLAR GRAINS [J].
BERNATOWICZ, TJ ;
AMARI, S ;
ZINNER, EK ;
LEWIS, RS .
ASTROPHYSICAL JOURNAL, 1991, 373 (02) :L73-L76
[9]   COGNATE XENOLITHS IN CHONDRITIC METEORITES - EXAMPLES IN MEZO-MADARAS AND GHUBARA [J].
BINNS, RA .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1968, 32 (03) :299-&
[10]  
CHRISTOPHEMICHE.M, 1976, EARTH PLANET SC LETT, V30, P143