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钙长辉石岩-石榴石转变在科拉拉陨石中。

Pyroxene-garnet transformation in coorara meteorite.

出版信息

Science. 1970 May 15;168(3933):832-3. doi: 10.1126/science.168.3933.832.

Abstract

Majorite is a new garnet in a veinlet of the Coorara meteorite. Its chemical composition is compatible with derivation mostly from original pyroxene, not from olivine as originally reported. Silicon is partly in sixfold coordination. Ringwoodite, a spinel of olivine composition, occurs as purple grains set in a matrix of fine-grained garnet. The similar mineralogy and texture of the Coorara and Tenham meteorites suggest a common parent body.

摘要

镁铝榴石是科拉拉陨石细脉中的一种新石榴石。其化学成分与主要源自原始辉石、而非原始橄榄石的成因相吻合,这与最初的报道不同。硅部分呈六配位。尖晶石型的林伍德石呈紫色颗粒状,嵌于细粒石榴石基质中。科拉拉和坦纳姆陨石具有相似的矿物学和结构,表明它们可能来自同一母体。

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