Continental crust and lithospheric mantle interaction beneath North China: isotopic evidence from granulite xenoliths in Hannuoba, Sino-Korean craton

被引:224
作者
Zhou, XH [1 ]
Sun, M
Zhang, GH
Chen, SH
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Lab Lithosphere Tecton Evolut, Beijing 100029, Peoples R China
[2] Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
lower crust; granulite xenolith; basaltic underplating; subcontinental lithosphere; Sr-Nd-Pb isotopes; North China Craton;
D O I
10.1016/S0024-4937(02)00110-X
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Mafic granulite and pyroxenite xenoliths from Cenozoic alkaline basalts at Hannuoba, Hebei Province, North China have been selected for a systematic geochemical and Sr-Nd-Pb isotopic study, which provides a unique opportunity to explore nature of the lower crust and the interaction between the continental crust and lithospheric mantle beneath an Archean craton. The major, compatible and incompatible elements and radiogenic isotopes of these xenoliths suggest great chemical heterogeneity of the lower crust beneath the Hannuoba region. Petrological and geochemical evidences indicate a clear cumulate origin, and most likely, they are related to basaltic underplating in different geological episodes. However, the Sr-Nd-Pb isotopic compositions of the xenoliths reveal a profound enriched source signature (EM 1) with some influence of EM 11, which implies that some portion of pre-existing, old metasomatized subcontinental lithospheric mantle could have played an important role in their genesis. It is suggested that the interaction between continental crust and subcontinental mantle as manifested by basaltic underplating would be closely related to regional tectonic episodes and geodynamic processes in the deep part of subcontinental lithospheric mantle. (C) 2002 Elsevier Science B.V. All fights reserved.
引用
收藏
页码:111 / 124
页数:14
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