Recycling lower continental crust in the North China craton | |
Gao S; Rudnick RL; Yuan HL; Liu XM; Liu YS; Xu WL; Ling WL; Ayers J; Wang XC; Wang QH | |
2004-12-16 | |
发表期刊 | NATURE |
卷号 | 432期号:7019页码:892-897 |
摘要 | Foundering of mafic lower continental crust into underlying convecting mantle has been proposed as one means to explain the unusually evolved chemical composition of Earth's continental crust(1,2), yet direct evidence of this process has been scarce. Here we report that Late Jurassic high-magnesium andesites, dacites and adakites ( siliceous lavas with high strontium and low heavy-rare-earth element and yttrium contents) from the North China craton have chemical and petrographic features consistent with their origin as partial melts of eclogite that subsequently interacted with mantle peridotite. Similar features observed in adakites and some Archaean sodium-rich granitoids of the tonalite-trondhjemite-granodiorite series have been interpreted to result from interaction of slab melts with the mantle wedge. Unlike their arc-related counterparts, however, the Chinese magmas carry inherited Archaean zircons and have neodymium and strontium isotopic compositions overlapping those of eclogite xenoliths derived from the lower crust of the North China craton. Such features cannot be produced by crustal assimilation of slab melts, given the high Mg#, nickel and chromium contents of the lavas. We infer that the Chinese lavas derive from ancient mafic lower crust that foundered into the convecting mantle and subsequently melted and interacted with peridotite. We suggest that lower crustal foundering occurred within the North China craton during the Late Jurassic, and thus provides constraints on the timing of lithosphere removal beneath the North China craton. |
DOI | 10.1038/nature03162 |
语种 | 英语 |
ISSN | 0028-0836 |
收录类别 | SCI ; EI |
EI入藏号 | 2005028778227 |
WOS记录号 | WOS:000225733500050 |
WOS类目 | Multidisciplinary Sciences |
WOS研究方向 | Science & Technology - Other Topics |
出版者 | NATURE PUBLISHING GROUP |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.cug.edu.cn/handle/2XU834YA/99498 |
专题 | 中国地质大学(武汉) |
作者单位 | 1.Univ Maryland, Dept Geol, Geochem Lab, College Pk, MD 20742 USA; 2.NW Univ Xian, Dept Geol, Key Lab Continental Dynam, Xian 710069, Peoples R China; 3.China Univ Geosci, Fac Earth Sci, Wuhan 430074, Peoples R China; 4.Jilin Univ, Sch Earth Sci, Changchun 130061, Peoples R China; 5.Vanderbilt Univ, Dept Geol, Nashville, TN 37235 USA |
推荐引用方式 GB/T 7714 | Gao S,Rudnick RL,Yuan HL,et al. Recycling lower continental crust in the North China craton[J]. NATURE,2004,432(7019):892-897. |
APA | Gao S.,Rudnick RL.,Yuan HL.,Liu XM.,Liu YS.,...&Wang QH.(2004).Recycling lower continental crust in the North China craton.NATURE,432(7019),892-897. |
MLA | Gao S,et al."Recycling lower continental crust in the North China craton".NATURE 432.7019(2004):892-897. |
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