华北克拉通岩石圈减薄机制: 来自山东白垩纪基性-中基性岩浆岩Re-Os同位素地球化学特征的制约

杨红梅; 凌文黎; 张军波; 段瑞春; 高永娟; 邱啸飞; 卢山松

doi:10.3799/dqkx.2013.053

Volume 38 Issue 3

May 2013

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Article Navigation > Earth Science > 2013 > 38(3): 529-540

YANG Hong-mei, LING Wen-li, ZHANG Jun-bo, DUAN Rui-chun, GAO Yong-juan, QIU Xiao-fei, LU Shan-song, 2013. The Lithospheric Thinning Mechanism of North China Craton: Re-Os Isotopic Geochemistry Constraint from the Cretaceous Basic to Intermediate Basic Igneous Rocks in Shandong Province. Earth Science, 38(3): 529-540. doi: 10.3799/dqkx.2013.053

Citation:

YANG Hong-mei, LING Wen-li, ZHANG Jun-bo, DUAN Rui-chun, GAO Yong-juan, QIU Xiao-fei, LU Shan-song, 2013. The Lithospheric Thinning Mechanism of North China Craton: Re-Os Isotopic Geochemistry Constraint from the Cretaceous Basic to Intermediate Basic Igneous Rocks in Shandong Province. Earth Science, 38(3): 529-540. doi: 10.3799/dqkx.2013.053

Citation:

YANG Hong-mei, LING Wen-li, ZHANG Jun-bo, DUAN Rui-chun, GAO Yong-juan, QIU Xiao-fei, LU Shan-song, 2013. The Lithospheric Thinning Mechanism of North China Craton: Re-Os Isotopic Geochemistry Constraint from the Cretaceous Basic to Intermediate Basic Igneous Rocks in Shandong Province. Earth Science, 38(3): 529-540. doi: 10.3799/dqkx.2013.053

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The Lithospheric Thinning Mechanism of North China Craton: Re-Os Isotopic Geochemistry Constraint from the Cretaceous Basic to Intermediate Basic Igneous Rocks in Shandong Province

doi: 10.3799/dqkx.2013.053

1.
Isotope Geochemistry Lab., Wuhan Institute of Geology and Mineral Resources, Ministry of Land and Resources, Wuhan 430223, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-04-17
Publish Date: 2013-05-15

Abstract

Abstract

A Re-Os isotopic study of Mesozoic igneous basic to intermediate basic rocks from the western-, eastern- and Yishu fault belt tectonic units in Shandong province, North China Craton (NCC), is carried out. The samples consists of 13 intrusive rocks from the Jinan, Yinan plutons and Guanshui dykes, and 13 volcanic rocks from the Anqiu, Mengyin, Feixian and Fangcheng volcanic successions. Most samples have relatively low Re (0.076×10^-9-0.711×10^-9) and Os (0.006×10^-9-1.030×10^-9) contents and high radiogenic ¹⁸⁷Os/¹⁸⁸Os ratios, with corresponding initial ¹⁸⁷Os/¹⁸⁸Os ratio of 0.131 6-0.529 1 and γ_Os(t) of 4.30-319.00, except for rock MAQ0609 of the Anqiu trachyandesite with initial ¹⁸⁷Os/¹⁸⁸Os ratio of 1.463 and γ_Os(t) of 1 060.000. The igneous rocks show a wide range of 0.125 to 2.090 Ga in Os isotope modal age (T_MA). On the γ_Os(t) vs. ε_Nd(t) and (⁸⁷Sr/⁸⁶Sr)_i vs. γ_Os(t) diagrams, these rocks are positioned between the lithospheric mantle and crust fields, indicative of a crust-mantle interaction-related origin. All but one Guanshui gabbro (MGS0610) and Feixian basalts of the samples display no clear positive correlation between γ_Os(t) and (La/Ta)_N or (Th/Nb)_N, which suggests that the role of crustal assimilation or contamination during the magma ascending was insignificant. Compared with the Paleozoic mantle xenoliths, these mantle-derived rocks have evidently younger Os modal ages, higher Re/Os and ¹⁸⁷Os/¹⁸⁸Os ratios. These crustal signs are likely to have been resulted from interactions of partial melts derived from delaminated lower crust rocks with ambient mantle under an upper mantle depth. Besides, on the Re/Yb vs. Yb diagram, samples of the Mengyin andesites and Yinan diorites are plotted between the Mesozoic pyroxene xenoliths and crust components, which may be best explained by mantle source rocks metasomatized by partial melts of delaminated eclogitic lower crust. Furthermore, a Mengyin andesite MMY-12 (SiO₂=56.4%) has a modal age as old as 2.090 Ga, and high Mg^# (64.6) and Os content (0.089×10^-9), which provides an additional evidence for lithospheric thinning-related interaction between the delaminated lower crust and the convecting upper mantle.
- North China Craton,
- Shandong Province,
- basic to intermediate basic igneous rocks,
- Re-Os isotope,
- lithospheric thinning,
- geochemistry

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References(75)

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