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Petrology and mineralogy of martian meteorite GRV 99027
Wang, HN; Liang, Y; Xu, WB
2006-02-01
Source PublicationACTA PETROLOGICA SINICA
ISSN1000-0569
Volume22Issue:2Pages:491-502
AbstractGRV 99027 is a new member of the martian lherzolitic shergottites(L-S) consisting of poikilitic, non-poikilitic and melt pocket textures. Its mineral modal composition is olivin (55vol%), pyroxene (37.5vol%, pigeonite and augite), a few maskelynite (6vol%), chromite (1.5vol%), and trace whitlockite, troilite and so on. The mineralogical chemistry of GRV 99027 are relatively homogeneous: olivine(Fo(69.1-76.6)Fa(23.4-30.9) avg. Fo(72.4) Fa(27.6)), pigeonite (En(59.3-75.1)Fs(20.5-26.9)Wo(3.1-14.9), avg. En(68.6) Fs(23.5), Wo(8.0) augite(En(46.6-53)Fs(13.1-16.1)Wo(31.9-37.8), avg. En(50.7)Fs(14.5)Wo(34.8)) and maskelynite (An(43.6-59.3)Ab(40.2-54.6)Or(0.5-1.8), avg. An(52.4)Ab(46.7) Or(0.8)). The crystallization sequence of GRV 99027 was two stages: firstly the primitive parent magma which originated from depleted martian mantle source region crystallized olivine and chromite in poikilitic area. Subsequently, a great deal of pigeonite crystallized into large oikio-crystals enclosing olivine and chromite, followed by abundant olivine, pigeonite, augite continuous crystallization in nonpoikilitic area, the interstitial melts in between crystals finally crystallized plagioclase, ilmenite and whitlockite etc. The coexistence of low-calcium pyroxene and augite in GRV 99027 indicated that the equilibrium temperature was about 1000 similar to 1190 degrees C (avg. 1146 degrees C). Sub-solidus re-equilibration experienced by GRV 99027 is ALH 77005 approximate to GRV 99027 > LEVI 88516 > Y 793605. The shock pressure of GRV 99027 was probably 30 similar to 45 G Pa and the post-shock temperature tended to be slightly lower than 600 degrees C.
KeywordMartian Meteorite Grv 99027 Lherzolitic Shergottite Crystallization Sequence Equilibrium Temperature Shock Pressure
Subject AreaGeology
WOS HeadingsScience & Technology ; Physical Sciences
WOS KeywordLEW88516 ; PETROGRAPHY ; CHEMISTRY
Indexed BySCI
Language英语
WOS Research AreaGeology
WOS SubjectGeology
WOS IDWOS:000236152700022
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://libir.pmo.ac.cn/handle/332002/3608
Collection天体化学和行星科学实验室
Affiliation1.Nanjing Univ, Dept Earth Sci, State Key Lab Mineral Deposits Res, Nanjing 210093, Peoples R China
2.Chinese Acad Sci, Purple Mt Observ, Nanjing 210008, Peoples R China
Recommended Citation
GB/T 7714
Wang, HN,Liang, Y,Xu, WB. Petrology and mineralogy of martian meteorite GRV 99027[J]. ACTA PETROLOGICA SINICA,2006,22(2):491-502.
APA Wang, HN,Liang, Y,&Xu, WB.(2006).Petrology and mineralogy of martian meteorite GRV 99027.ACTA PETROLOGICA SINICA,22(2),491-502.
MLA Wang, HN,et al."Petrology and mineralogy of martian meteorite GRV 99027".ACTA PETROLOGICA SINICA 22.2(2006):491-502.
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