蒙切戈尔斯克岩浆岩群层状侵入体形成条件

IF 1 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Petrology Pub Date : 2022-07-24 DOI:10.1134/S0869591122030079
V. S. Semenov, O. V. Kazanov, S. I. Korneev, E. B. Salnikova, S. V. Semenov
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引用次数: 0

摘要

本文介绍了蒙切戈尔斯克和蒙切顿德拉层状地块的年代学资料和岩石学模拟结果。尼提斯山边缘带黑岩的U-Pb ID-TIMS锆石定年结果为2506±7 Ma,与其他地区类似岩石的锆石定年结果一致。通过对Monchegorsk和Kivakka地块剖面的比较,估算出Monchegorsk地块的侵蚀前厚度为3700 m。在6.5 ~ 5.5 kbar压力下对Monchegorsk岩体边缘带岩石进行计算,结果表明:与Ol平衡的熔体中SiO2≤55 wt %, TiO2≤0.50 wt %, MgO≤14 wt %。原始岩浆的温度可达1390℃。在较低的压力下(低于6.5 kbar),得到的熔体变得更硅。在Monchegorsk侵入岩中,根据该模型,藻内橄榄石的组成变化范围在88-92 mol % Fo之间。熔体中藻内橄榄石的含量,根据压力的不同,可以从11%到24%不等。形成Monchegorsk侵入岩和Monchetundra侵入岩(742孔)层状序列的岩浆来源不同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Conditions of Formation of Layered Intrusions of the Monchegorsk Magmatic Cluster

The paper presents geochronological data and results of petrological modeling of the Monchegorsk and Monchetundra layered massifs. The U-Pb ID-TIMS zircon dating of norite from the marginal zone of Mt. Nittis yielded 2506 ± 7 Ma, which coincides with previous data on similar rocks from other areas. Based on the comparison of sections of the Monchegorsk and Kivakka massifs, the pre-erosion thickness of the Monchegorsk massif is estimated as 3700 m. Calculations using rocks of the marginal zone of the Monchegorsk intrusion at a pressure of 6.5–5.5 kbar showed that the melt in equilibrium with Ol contained SiO2 ≤ 55 wt %, TiO2 ≤ 0.50 wt %, and MgO ≤14 wt %. The temperature of the primary magma could be equal to 1390°C. At a lower pressure (below 6.5 kbar), the obtained melt becomes more siliceous. In the Monchegorsk intrusion, the composition of intratelluric olivine according to this model could vary within 88–92 mol % Fo. The content of intratelluric olivine in the melt, depending on pressure, could vary from 11 to 24 vol %. Magmas that formed the Monchegorsk intrusion and the layered series of the Monchetundra intrusion (hole 742) were derived from different sources.

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来源期刊
Petrology
Petrology 地学-地球科学综合
CiteScore
2.40
自引率
20.00%
发文量
27
审稿时长
>12 weeks
期刊介绍: Petrology is a journal of magmatic, metamorphic, and experimental petrology, mineralogy, and geochemistry. The journal offers comprehensive information on all multidisciplinary aspects of theoretical, experimental, and applied petrology. By giving special consideration to studies on the petrography of different regions of the former Soviet Union, Petrology provides readers with a unique opportunity to refine their understanding of the geology of the vast territory of the Eurasian continent. The journal welcomes manuscripts from all countries in the English or Russian language.
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