新墨西哥州索科罗县塞维利亚塔国家野生动物保护区的长叶岩:初步结果

V. McLemore
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引用次数: 3

摘要

砖红色的表长岩是在新墨西哥州中部的塞维利亚国家野生动物保护区的一组异常的元古代岩石中发现的。长辉长岩这个术语是用来描述被富碱流体脱硅和交代的蚀变岩石。在新墨西哥州和科罗拉多州南部的其他地方也发现了类似的辉长岩,它们被认为是贯穿科罗拉多州南部和新墨西哥州的寒武纪-奥陶纪岩浆事件的一部分。与Caballo和Burro山脉的表长岩不同,后者含有中至高浓度的稀土元素(REE)、铀和钍;塞维利亚国家野生动物保护区的长叶岩没有经济潜力。255
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Episyenites in the Sevilleta National Wildlife Refuge, Socorro County, New Mexico: preliminary results
Brick-red episyenites are found in an outlier of Proterozoic-age rocks on the Sevilleta National Wildlife Refuge in central New Mexico. The term episyenite is used to describe altered rocks that were desilicified and metasomatized by alkali-rich fluids. Similar episyenites are found elsewhere in New Mexico and southern Colorado and are thought to be part of a Cambrian-Ordovician magmatic event that is documented throughout southern Colorado and New Mexico. Unlike episyenites in the Caballo and Burro Mountains, which contains moderate to high concentrations of rare earth elements (REE), uranium, and thorium; the episyenites in the Sevilleta National Wildlife Refuge have no economic potential. 255
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