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MINERALOGICAL ABSTRACTS FROM SCIENTIFIC PAPERS PUBLISHED IN JAPAN, Edited by the Abstracting Committee, Japan Association of Mineralogical Sciences

机译:日本出版的科学论文的矿物文摘,由日本矿物学协会抽象委员会编辑

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103001 Arai, T., Takeda, H. & Miyamoto, M. Experimental petrology of ancient lunar mare basalt Asuka-881757: Spinel crystallization as a petrologic indicator. Antarctic Meteorite Res., No. 19, 1-19, 5 figs., 10 tables, 2006. The paucity of titanian chromites in lunar-meteorite basalt Asuka (A) 881757 is unusual compared to the general occurrence of coexisting chromites and ulvospinels in the Apollo and Luna mare basalts. The unique spinel crystallization of A 881757 is expected to hold a key to elucidate the crystallization and cooling episodes of the basalt. In this study, we investigated the possible reason for the missing chromite by conducting isothermal and cooling experiments on the bulk-rock composition of A 881757 and discuss the petrogenesis of the ancient low-Ti mare basalt in light of spinel crystallization. A series of isothermal experiments showed the A 881757 basalt magma is not saturated with chromite under the expected lunar oxygen fugacity condition (IWIW-1). A peritectic reaction among chromite, melt, and pyroxene is present for A 881757 basalt magma under the more oxidized condition which is one or two log unit higher than the lunar condition.
机译:103001 Arai,T.,Takeda,H.&Miyamoto,M.古代月球玄武岩的实验岩石学Asuka-881757:尖晶石结晶作为岩石学指示剂。 《南极陨石研究》,第19期,第1-19期,5图,第10张,2006年。与在该地区普遍存在的铬铁矿和硫代松岩相比,月陨玄武岩明日香(A)881757中钛铁矿的缺乏是不寻常的。阿波罗和露娜·马雷的玄武岩。预期A 881757的独特尖晶石结晶将成为阐明玄武岩结晶和冷却现象的关键。在这项研究中,我们通过对A 881757的块岩成分进行等温和冷却实验,研究了缺少铬铁矿的可能原因,并根据尖晶石的结晶性讨论了古代低钛母马玄武岩的成因。一系列等温实验表明,在预期的月度氧气逸度条件下(IWIW-1),A 881757玄武岩岩浆不会被亚铬酸盐饱和。 881757玄武岩岩浆在更高氧化条件下(比月球条件高一个或两个对数单位)存在亚铬铁矿,熔体和辉石之间的包晶反应。

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