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 >Oxygen isotopes in calcium-aluminum-rich inclusions from enstatite chondrites: new evidence for a single CAI source in the solar nebula
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Oxygen isotopes in calcium-aluminum-rich inclusions from enstatite chondrites: new evidence for a single CAI source in the solar nebula

机译:顽辉长晶陨石中富含钙铝的包裹体中的氧同位素:太阳星云中单一CAI来源的新证据

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摘要

Calcium-aluminum-rich inclusions (CAIs) from enstatite chondrites have large ~(16)O excesses, similar to CAIs in carbonaceous and ordinary chondrites, and are also similar in morphology, mineralogy and Al-Mg isotopic systematics. These similarities provide new evidence that most CAIs might have formed in a single, restricted nebular locale and were then distributed unevenly throughout the various chondrite accretion regions.
机译:顽辉陨石球粒陨石中富含钙铝的夹杂物(CAI)具有较大的〜(16)O过量,与碳质和普通球粒陨石中的CAI相似,并且在形态,矿物学和Al-Mg同位素系统学方面也相似。这些相似性提供了新的证据,表明大多数CAI可能在单个受限的星云区域中形成,然后在各个球粒体的积聚区域分布不均匀。

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