首页> 外文期刊>Economic geology and the bulletin of the Society of Economic Geologists >U-Pb, Re-Os, and Ar/Ar Geochronology of Rare Earth Element (REE)-Rich Breccia Pipes and Associated Host Rocks from the Mesoproterozoic Pea Ridge Fe-REE-Au Deposit, St. Francois Mountains, Missouri
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U-Pb, Re-Os, and Ar/Ar Geochronology of Rare Earth Element (REE)-Rich Breccia Pipes and Associated Host Rocks from the Mesoproterozoic Pea Ridge Fe-REE-Au Deposit, St. Francois Mountains, Missouri

机译:密苏里州圣弗朗索瓦山脉中元古代豌豆岭Fe-REE-Au矿床中富含稀土元素(REE)的角砾岩管道和相关主岩的U-Pb,Re-Os和Ar / Ar地质年代学

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摘要

Rare earth element (REE)-rich breccia pipes (600,000 t @ 12% rare earth oxides) are preserved along the margins of the 136-million metric ton (Mt) Pea Ridge magnetite-apatite deposit, within Mesoproterozoic (similar to 1.47 Ga) volcanic-plutonic rocks of the St. Francois Mountains terrane in southeastern Missouri, United States. The breccia pipes cut the rhyolite-hosted magnetite deposit and contain clasts of nearly all local bedrock and mineralized lithologies.
机译:沿中元古代(约1.47 Ga)的1.36亿吨豌豆岭磁铁矿-磷灰石矿床的边缘保留了富含稀土元素(角砾岩)的角砾岩管(600,000吨,稀土氧化物含量为12%)。美国东南密苏里州圣弗朗索瓦山脉地层的火山-火山成岩。角砾岩管道切割了流纹岩中的磁铁矿沉积物,并包含了几乎所有当地基岩和矿化岩性的碎屑。

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