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首页> 外文期刊>Doklady Earth Sciences >Heterogeneity of Isotope Sources of Alkaline Magmatism in the Hot Spot of the Southwestern Atlantic: Fernando de Noronha Islands
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Heterogeneity of Isotope Sources of Alkaline Magmatism in the Hot Spot of the Southwestern Atlantic: Fernando de Noronha Islands

机译:西南大西洋热点的碱性岩浆作用同位素源的非均质性:费尔南多·迪诺罗尼亚群岛

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摘要

New data on age and isotopic characteristics of alkaline magmatism in the hot spot of the Fernando de Noronha Islands have been obtained. For the first time, a new aspect of isotope heterogeneity expressed in enrichment in radiogenic Sr was revealed. The Fernando de Noronha Archipelago is situated 345 km away from the Atlantic coast of Brazil and is confined to a transform fracture zone. The Fernando de Noronha lineament is traced far to the west by the Rocas atoll, a chain of seamounts, and occurrences of alkaline magmatism on the continent. According to the tectonic interpretation, this lineament is regarded as a track of a hot spot.
机译:获得了有关费尔南多·迪诺罗尼亚群岛热点地区碱性岩浆作用的年龄和同位素特征的新数据。首次揭示了在放射性Sr富集中表达的同位素异质性的新方面。费尔南多·迪诺罗尼亚群岛(Fernando de Noronha Archipelago)距巴西大西洋沿岸345公里,被限制在一个转换断裂带中。罗纳斯环礁,一连串的海山和大陆上发生的碱性岩浆作用可以追溯到费尔南多·迪诺罗尼亚河系的西部。根据构造的解释,这种线条被认为是热点的轨迹。

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