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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >From source to crust: Tracing magmatic evolution in a kimberlite and a melilitite using microsample geochemistry
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From source to crust: Tracing magmatic evolution in a kimberlite and a melilitite using microsample geochemistry

机译:从源头到地壳:使用微量样品地球化学追踪金伯利岩和陨石的岩浆演化

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摘要

We present an integrated microsampling trace element and isotopic study of primary minerals within the Jos kimberlite, Canada, in order to observe how different phases record progressive crustal interaction in the evolving kimberlite. Identification of the least contaminated phases provides the best information on kimberlite source geochemistry. We also carried out an analogue study on an olivine melilitite from Saltpetre Kop, South Africa, examining a similar mineral suite, with the addition of melilite. The two studies show that all phases except phenocryst olivine show some evidence of crustal modification. Perovskite has recently been used as a proxy for source isotope composition. Although perovskite may provide a better constraint on the isotopic composition of the kimberlite than the whole rock, it does not necessarily provide the best constraint on the source region. The lower initial ~(87)Sr/~(86)Sr ratio recorded by early crystallising phases in the kimberlite is similar to those of the low-Cr megacryst suite, strengthening the genetic relationship between kimberlite activity and megacryst formation.
机译:我们介绍了加拿大乔斯金伯利岩中主要矿物的微量采样微量元素和同位素研究,目的是观察不同的相如何记录不断演化的金伯利岩中地壳相互作用。鉴定污染最小的相可提供有关金伯利岩来源地球化学的最佳信息。我们还对南非Saltpetre Kop的橄榄石陨石进行了模拟研究,研究了类似的矿物套件,并添加了陨石。两项研究表明,除了橄榄石晶以外的所有相都显示出一些地壳变质的证据。钙钛矿最近已被用作源同位素组成的替代物。尽管钙钛矿可能对金伯利岩的同位素组成比整个岩石提供更好的约束,但不一定对源区提供最佳约束。在金伯利岩的早期结晶阶段记录的较低的初始〜(87)Sr /〜(86)Sr比与低Cr大晶组相似,从而增强了金伯利岩活动与大晶形成之间的遗传关系。

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