Geochemistry of Early Cretaceous calc-alkaline lamprophyres in the Jiaodong Peninsula: Implication for lithospheric evolution of the eastern North China Craton

• Published in: Gondwana research Vol. 25; no. 2; pp. 859 - 872
• Main Authors: Ma, Liang, Jiang, Shao-Yong, Hou, Ming-Lan, Dai, Bao-Zhang, Jiang, Yao-Hui, Yang, Tao, Zhao, Kui-Dong, Pu, Wei, Zhu, Zhi-Yong, Xu, Bin
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.03.2014
• Subjects: Calc-alkaline lamprophyres; Geochemistry; Jiaodong Peninsula; Lithospheric evolution; North China Craton; Calc-alkaline lamprophyres; Geochemistry; Lithospheric evolution; North China Craton; Jiaodong Peninsula
• ISSN: 1342-937X; 1878-0571
• DOI: 10.1016/j.gr.2013.05.012

Mesozoic lamprophyres are widely present in gold province in the Jiaodong Peninsula. In this study, we analyzed major and trace elements and Sr–Nd–Pb isotopic compositions of lamprophyres from the Linglong and Penglai Au-ore districts in the Jiaodong Peninsula, in an attempt to better understand Mesozoic lithospheric evolution beneath the eastern North China Craton. These lamprophyre dikes are calc-alkaline in nature, and are characterized by low concentrations of SiO2, TiO2 and total Fe2O3, high concentrations of MgO, Mg# and compatible element, enriched in LREE and LILE but variably depleted in HFSE. They display initial 87Sr/86Sr ratios of 0.709134–0.710314, εNd(t) values of −13.2 to −18.3, 206Pb/204Pb of 17.364–17.645, 207Pb/204Pb of 15.513–15.571 and 208Pb/204Pb of 37.995–38.374. Interpretation of elemental and isotopic data suggests that the Linglong and Penglai lamprophyres were derived from partial melting of a phlogopite- and/or amphibole-bearing lherzolite in the spinel–garnet transition zone. The parental magma might have experienced fractionation of olivine and clinopyroxene, and minor crustal materials were incorporated during ascent of these mafic magmas. Before ~120Ma of emplacement of these calc-alkaline lamprophyres, the ancient lithospheric mantle was variably metasomatized by hydrous fluids rather than melts from subducted/foundered continental crust. It is proposed that continuous modification by slab-derived hydrous fluids from the Paleo-Pacific plate converted the old cratonic lithospheric mantle to Mesozoic enriched lithospheric mantle. Geodynamic force for generation of these lamprophyres may be related to large scale lithospheric thinning coupled with upwelling of the asthenosphere beneath the North China Craton. Continental arc-rifting related to the Paleo-Pacific plate subduction is favored as a geodynamic force for the cratonic lithosphere detachment. [Display omitted] •The lamprophyres were from partial melting of the local enriched lithospheric mantle.•Mesozoic lithospheric mantle was a phlogopite- and/or amphibole-bearing lherzolite.•The mantle was metasomatized by slab-derived hydrous fluids of Paleo-Pacific plate.•Continuous modification transformed old cratonic mantle to Mesozoic enriched mantle.