Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1038/s41561-019-0348-0 |
An isotopically depleted lower mantle component is intrinsic to the Hawaiian mantle plume | |
DeFelice, C.1; Mallick, S.2; Saal, A. E.2; Huang, S.1 | |
2019-06-01 | |
发表期刊 | NATURE GEOSCIENCE |
ISSN | 1752-0894 |
EISSN | 1752-0908 |
出版年 | 2019 |
卷号 | 12期号:6页码:487-+ |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Most ocean island basalts sample an isotopically depleted mantle component, but the origin of this component is unclear. It may come from either the entrained upper mantle or from a reservoir intrinsic to the plume, sourced from the lower mantle. For Hawaii, the isotopically depleted component is primarily sampled during the secondary rejuvenated-stage volcanism, 0.5-2 million years after the initial shield-stage volcanism. However, it is also inferred in shield and post-shield lavas. We analyse the radiogenic isotopic and trace element compositions of a suite of Mauna Kea shield-stage tholeiites, and found that they have the same isotopic compositions as rejuvenated-stage lavas. We use trace element models to show that these shield-stage basalts can be explained as higher degree partial melts of a rejuvenated-stage source. Our data, therefore, show that the depleted rejuvenated-stage component was directly sampled during shield-stage volcanism. The common source for both shield-stage and secondary rejuvenated volcanism implies that the depleted rejuvenated component is intrinsic to the Hawaiian mantle plume. It is further inferred that the mantle region from which the Hawaiian plume originates, probably in the lower mantle, is also isotopically depleted, similar but not identical to the upper mantle. |
领域 | 地球科学 ; 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000469459600018 |
WOS关键词 | SCIENTIFIC DRILLING PROJECT ; EAST PACIFIC RISE ; PB ISOTOPE SYSTEMATICS ; PUU OO ERUPTION ; TRACE-ELEMENT ; KILAUEA VOLCANO ; MAUNA-KEA ; HALEAKALA VOLCANO ; KOOLAU VOLCANO ; GEOCHEMICAL EVOLUTION |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/183940 |
专题 | 地球科学 气候变化 |
作者单位 | 1.Univ Nevada, Las Vegas, NV 89154 USA; 2.Brown Univ, Providence, RI 02912 USA |
推荐引用方式 GB/T 7714 | DeFelice, C.,Mallick, S.,Saal, A. E.,et al. An isotopically depleted lower mantle component is intrinsic to the Hawaiian mantle plume[J]. NATURE GEOSCIENCE,2019,12(6):487-+. |
APA | DeFelice, C.,Mallick, S.,Saal, A. E.,&Huang, S..(2019).An isotopically depleted lower mantle component is intrinsic to the Hawaiian mantle plume.NATURE GEOSCIENCE,12(6),487-+. |
MLA | DeFelice, C.,et al."An isotopically depleted lower mantle component is intrinsic to the Hawaiian mantle plume".NATURE GEOSCIENCE 12.6(2019):487-+. |
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