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DOI | 10.1016/j.epsl.2020.116123 |
Geochemistry of Etendeka magmatism: Spatial heterogeneity in the Tristan-Gough plume head | |
Zhou H.; Hoernle K.; Geldmacher J.; Hauff F.; Homrighausen S.; Garbe-Schönberg D.; Jung S. | |
发表日期 | 2020 |
ISSN | 0012821X |
卷号 | 535 |
英文摘要 | The origin and distribution of geochemically distinct source components in continental flood volcanism (generally associated with the initial phase of a mantle plume head) are poorly understood. Here we present new geochemical (major and trace element and Sr-Nd-Pb-Hf isotope) data from the Etendeka flood basalts and associated dikes from northern and central Namibia that are believed to have been produced during the initial stage of the Tristan-Gough hotspot. Following earlier studies, the Etendeka lava flows and dikes are divided into high-Ti and low-Ti groups. The trace element and isotopic composition of the high-Ti tholeiitic basalts, exclusively outcropping in northern Etendeka (northwestern Namibia), are similar to the Gough-type enriched mantle I (EMI) composition found on the Walvis Ridge (the Atlantic type locality for the EMI end member). The low-Ti tholeiitic basalts, primarily outcropping in Southern Etendeka (central western Namibia), have higher 143Nd/144Nd and 207Pb/204Pb but lower 208Pb/204Pb ratios than the Gough composition. Combining our data with newly published 3He/4He data and estimates of the magma source's potential temperature from 1520-1680°C, we conclude that the source of the low-Ti basalts was also intrinsic to the Tristan-Gough plume, consistent with a spatially-zoned plume head. The low-Ti basalts were derived from a distinct EMI-type source component that has thus far only been detected in the initial Tristan-Gough plume head (∼132 Ma), but not the later submarine hotspot track. © 2020 Elsevier B.V. |
关键词 | Etendeka flood basaltsGoughLarge Igneous Province (LIP)Namibiaplume zonationSr-Nd-Pb-Hf isotope ratios |
英文关键词 | Basalt; Floods; Geochemistry; Hafnium alloys; Isotopes; Levees; Neodymium alloys; Strontium alloys; Trace elements; Flood basalt; Gough; Large igneous provinces; Namibia; plume zonation; Sr-Nd-Pb-Hf isotopes; Lead alloys; flood basalt; hafnium; hot spot; igneous geochemistry; large igneous province; lava flow; lead isotope; magmatism; neodymium isotope; strontium isotope; Namibia |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203009 |
作者单位 | GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, Kiel, 24148, Germany; Institute of Geosciences, Kiel University, Ludewig-Meyn-Str. 10, Kiel, 24118, Germany; Institute of Mineralogy and Petrography, Universität Hamburg, Grindelallee 48, Hamburg, 20146, Germany |
推荐引用方式 GB/T 7714 | Zhou H.,Hoernle K.,Geldmacher J.,et al. Geochemistry of Etendeka magmatism: Spatial heterogeneity in the Tristan-Gough plume head[J],2020,535. |
APA | Zhou H..,Hoernle K..,Geldmacher J..,Hauff F..,Homrighausen S..,...&Jung S..(2020).Geochemistry of Etendeka magmatism: Spatial heterogeneity in the Tristan-Gough plume head.Earth and Planetary Science Letters,535. |
MLA | Zhou H.,et al."Geochemistry of Etendeka magmatism: Spatial heterogeneity in the Tristan-Gough plume head".Earth and Planetary Science Letters 535(2020). |
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