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首页> 外文期刊>Geoscience frontiers >Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-G?m?r Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths
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Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-G?m?r Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths

机译:在Nógrád-g?M?r火山场(北Pannonian盆地)下面的上部地幔中的弥言主义诱导的Wehrlite形成:来自Xenoliths的证据

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Clinopyroxene-enriched upper mantle xenoliths classified as wehrlites are common (~20% of all xenoliths) in the central part of the Nógrád-G?m?r Volcanic Field (NGVF), situated in the northern margin of the Pannonian Basin in northern Hungary and southern Slovakia. In this study, we thoroughly investigated 12 wehrlite xenoliths, two from each wehrlite-bearing occurrence, to determine the conditions of their formation. Specific textural features, including clinopyroxene-rich patches in an olivine-rich lithology, orthopyroxene remnants in the cores of newly-formed clinopyroxenes and vermicular spinel forms all suggest that wehrlites were formed as a result of intensive interaction between a metasomatic agent and the peridotite wall rock. Based on the major and trace element geochemistry of the rock-forming minerals, significant enrichment in basaltic (Fe, Mn, Ti) and high field strength elements (Nb, Ta, Hf, Zr) was observed, compared to compositions of common lherzolite xenoliths. The presence of orthopyroxene remnants and geochemical trends in rock-forming minerals suggest that the metasomatic process ceased before complete wehrlitization was achieved. The composition of the metasomatic agent is interpreted to be a mafic silicate melt, which was further confirmed by numerical modelling of trace elements using the plate model. The model results also show that the melt/rock ratio played a key role in the degree of petrographic and geochemical transformation. The lack of equilibrium and the conclusions drawn by using variable lherzolitic precursors in the model both suggest that wehrlitization was the last event that occurred shortly before xenolith entrainment in the host mafic melt. We suggest that the wehrlitization and the Plio–Pleistocene basaltic volcanism are related to the same magmatic event.Graphical abstractDownload : Download high-res image (420KB)Download : Download full-size image
机译:作为Wehrlites的Closococexene-in型卵石Xenoleds在Nógrád-g?M?R火山田(NGVF)中的常见(〜20%的Xenoliths),位于匈牙利北部的Pannonian盆地的北边缘和斯洛伐克南部。在这项研究中,我们彻底调查了来自每种Wehrlite承载的两种Wehrlite Xenoliths,以确定其形成的条件。特异性纹理特征,包括富含橄榄石的岩性岩性的富含曲折的贴剂,在新形成的临床的核心和蠕虫尖晶石形式中,均表明,Wehrlites是由偏载剂和恒星壁之间的密集相互作用形成的岩石。基于岩石形成矿物质的主要和痕量元素地球化学,与普通甲绒岩氙气的组成相比,观察到玄武岩(Fe,Mn,Ti)和高场强元件(Nb,Ta,Hf,Zr)的显着富集。岩石形成矿物质的偏离甲肾上腺残余物和地球化学趋势表明,在完全Wehrlitization之前停止的态化过程。将偏载剂的组成被解释为乳酸镁硅酸盐熔体,其通过使用板模型的微量元素的数值建模进一步证实。模型结果还表明,熔体/岩石比在岩体和地球化学转化程度中起着关键作用。缺乏均衡和模型中的可变叶罗列洛丽特能前体吸引的结论既表明Wehrlitization是在宿主MAFIC熔体中Xenolith夹带之前不久发生的最后事件。我们建议我们的Wehrlitization和Plio-aloistocene玄武岩雌性与相同的魔法赛事有关。图形抽象:下载高分辨率图像(420KB)下载:下载全尺寸图像

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