Petrogenesis of Late Mesozoic mafic dykes in the Jiaodong Peninsula, eastern North China Craton and implications for the foundering of lower crust

Liu, Сhen; Hu, Ruizhong; Gao, Shan; Chen, Feng; Yu, Bobin; Guo, Feng; Qi, Youqiang; Wang, Tao; Coulson, Ian M.

doi:10.1016/j.lithos.2009.06.035

Cited by 116 publications

(73 citation statements)

References 115 publications

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“…북중 국지괴 동측에 분포하는 백악기초기(약 144-100 Ma) 화성암은 피크라이트(picrite)-현무암-현무암질 안산암 및 황반암(lamprophyre)의 분출암 (Qiu et al, 2002;Yang et al, 2004;Guo et al, 2005Guo et al, , 2013Liu et al, 2006;Gao et al, 2008;Ma et al, 2014a, b)과 반려암-섬록암-몬조니암-섬장암-화강암 및 휘록암의 관 입암체 (Xu et al, , 2006Chen et al, , 2004Zhang et al, 2004Zhang et al, , 2005Zhang et al, , 2010Zhang et al, , 2012Wu et al, 2005;Yang et al, 2006Yang et al, , 2012aLiu et al, , 2009 Guo et al, 2004;Wang et al, 2005)과 반려암-섬록암-몬조니암-섬장암-화강암 및 휘록암의 관입암체 (Jahn et al, 1999;Yang et al, 2005a;Guo et al, 2006Guo et al, , 2014Huang et al, 2006Huang et al, , 2007Wang et al, 2007;Zhao et al, 2005Zhao et al, , 2007aLiu et al, 2008b;Tang et al, 2008b;Zhang et al, 2010Zhang et al, , 2012He et al, 2011He et al, , 2013)로 구성되어 있다. TAS도( (Fig.…”

Section: 암 상unclassified

“…The boundary line dividing the alkaline and subalkaline series is from Irvine and Baragar (1971). Data sources for eastern China from Charoy and Raimbault (1994), Martin et al (1994), Lapierre et al (1997), Swell and Campbell (1997), Li and McCulloch (1998), Jahn et al (1999), Chen et al (2001Chen et al ( , 2004Chen et al ( , 2008, Fan et al (2001Fan et al ( , 2004, Guo et al (2001Guo et al ( , 2004Guo et al ( , 2005Guo et al ( , 2006Guo et al ( , 2013Guo et al ( , 2014, Xu et al (2002Xu et al ( , 2006, Zhang et al ( , 2004Zhang et al ( , 2005Zhang et al ( , 2010Zhang et al ( , 2012, , Wang et al (2003Wang et al ( , 2004Wang et al ( , 2005Wang et al ( , 2007Wang et al ( , 2008, Shu et al (2004), Yang et al (2004Yang et al ( , 2005aYang et al ( , 2006Yang et al ( , 2012aYang et al ( , b, 2013, Zhao et al (2005Zhao et al ( , 2007a, Huang et al (2006Huang et al ( , 2007, Liu et al (2006Liu et al ( , 2008aLiu et al ( , b, 2009…”

Section: 암 상mentioning

confidence: 99%

“…FC=fractional crystallization; AFC=assimilation and fractional crystallization. (Chen et al, 2001;Fan et al, 2001Fan et al, , 2004Guo et al, 2001Guo et al, , 2004Guo et al, , 2013Qiu et al, 2002;Zhang et al, , 2004Zhang et al, , 2005Chen et al, , 2004Wang et al, 2003;Yang et al, 2004;Wang et al, 2005Wang et al, , 2008Yang et al, 2005aYang et al, , 2006Yang et al, , 2012aZhao et al, 2005Zhao et al, , 2007bLiu et al, 2006Liu et al, , 2008aLiu et al, , b, 2009Gao et al, 2008;Tang et al, 2008b;Guo et al, 2014;Ma et al, 2014a, b). 이는 위 암석들이 고-칼륨 칼크-알 칼리 내지는 쇼쇼나이트 계열에 속한다 (Fig.…”

Section: 제될 수 있다unclassified

“…이는 위 암석들이 고-칼륨 칼크-알 칼리 내지는 쇼쇼나이트 계열에 속한다 (Fig. 2) Sr isotopic ratios for Early Cretaceous basaltic rocks from eastern China (Lapierre et al, 1997;Li and McCulloch, 1998;Jahn et al, 1999;Chen et al, 2001Chen et al, , 2004Chen et al, , 2008Fan et al, 2001Fan et al, , 2004Guo et al, 2001Guo et al, , 2004Guo et al, , 2005Guo et al, , 2013Guo et al, , 2014Xu et al, 2002;Zhang et al, , 2004Zhang et al, , 2012Wang et al, 2003Wang et al, , 2004Wang et al, , 2005Wang et al, , 2008Yang et al, 2004Yang et al, , 2005aYang et al, , 2006Yang et al, , 2012aLiu et al, 2006Liu et al, , 2008aLiu et al, , b, 2009Yu et al, 2006;Huang et al, 2007;Zhao et al, 2007b;Gao et al, 2008;Xie et al, 2008;Tang et al, 2009;Ma et al, 2014a, b). Data source for basaltic rocks from the Hayang Group in the Gyeongsang basin from Kwon et al (2013).…”

Section: 제될 수 있다mentioning

confidence: 99%

“…OIB=oceanic island basalt (Sun and McDonough, 1989); N-MORB=normal mid-ocean ridge basalt (Sun and McDonough, 1989); LCC=average lower continental crust (Rudnick and Gao, 2005); UCC=average upper continental crust (Rudnick and Gao, 2005). Pb ratios for Early Cretaceous basaltic rocks from eastern China (Qiu et al, 2002;Xu et al, 2002;Zhang et al, , 2004Chen et al, 2004Chen et al, , 2008Yang et al, 2004Yang et al, , 2012bLiu et al, 2006Liu et al, , 2008aLiu et al, , b, 2009Huang et al, 2007;Zhao et al, 2007b;Wang et al, 2005Wang et al, , 2008Ma et al, 2014a, b). For comparison, Pb isotope data for basement rocks from the North China block, South China block I (represented by rocks from the middle-lower Yangtze valley and the regions south of it) and South China block II (represented by the Dabie-Sulu ultra-high pressure eclogites and gneisses, all calculated back to t = 130 Ma) from Yang et al (2012b), and Zeng and Yan (2014).…”

Section: 제될 수 있다mentioning

confidence: 99%

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Petrogenesis of Early Cretaceous Magmatism in Eastern China and the Gyeongsang Basin, Korean Peninsula

Choi¹

2016

The Journal of the Petrological Society of Korea

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핵심어: 백악기초기, 동중국, 경상분지, 현무암, 암석권맨틀Abstract: Geochemical characteristics of the Early Cretaceous igneous rocks from eastern China and the Gyeongsang Basin, Korean Peninsula has been summarized. They have wide range of lithological variation with extrusive picrite-basalt-andesite-trachyte-rhyolite and lamprophyre, and intrusive gabbro-dioritemonzonite-syenite-granite and diabase in eastern China, mostly belonging to the high-K calc-alkaline or shoshonitic series. The volcanic rocks intercalated with the Hayang Group sedimentary assemblages in the Gyeongsang basin are high-K to shoshonitic basaltic trachyandesites. The Early Cretaceous basaltic rocks studied mostly fall within the field of within-plate basalts on the Zr/Y-Zr and Nb-Zr-Y tectonic discrimination diagrams. On a Sr-Nd isotope correlation diagram, basaltic rocks from the North China block (NCB) and the continent-continent collision zone (CZ) between the North and South China blocks plot into the enriched lower right quadrant along the extension of the mantle array. The initial Pb(t) correlation. Meanwhile, the SCB basaltic

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Section: 암 상unclassified

Section: 암 상mentioning

confidence: 99%

Section: 제될 수 있다unclassified

Section: 제될 수 있다mentioning

confidence: 99%

Section: 제될 수 있다mentioning

confidence: 99%

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Petrogenesis of Early Cretaceous Magmatism in Eastern China and the Gyeongsang Basin, Korean Peninsula

Choi¹

2016

The Journal of the Petrological Society of Korea

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Origin of dyke swarms by mixing of metasomatized subcontinental lithospheric mantle‐derived and lower crustal magmas in the Guocheng fault belt, Jiaodong Peninsula, North China Craton

et al. 2012

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Cretaceous dyke swarms are widespread in the Guocheng fault belt, Jiaodong Peninsula, eastern North China Craton (NCC). Elemental analyses show that these dykes are classified as high‐K calc‐alkaline to shoshonitic series, and are characterized by high MgO (up to 10.33 wt%; Mg# < 69.8), Cr (<571 ppm) and Ni (<235 ppm) at low silica contents. They are enriched in LILEs (e.g. Sr, Ba, K and Pb) and LREEs, depleted in HFSEs (e.g. Nb–Ta, Zr–Hf, Ti and P), and possess relatively radiogenic Sr (initial 87Sr/86Sr = 0.7078 to 0.7116) and Nd [εNd(t) = −20.8 to −13.5] and much less radiogenic Pb (206Pb/204Pb = 17.13 to 17.56) isotope signatures. These data, combined with inversely zoned amphibole and pyroxene phenocrysts, suggest a hybrid origin for the Guocheng dykes. The inferred magma evolution is dominated by repeated injection of basic magma from metasomatized subcontinental lithospheric mantle (SCLM) into a lower crustal reservoir of intermediate‐felsic composition. This refertilized lithospheric mantle source, probably together with its overlying enriched lower crust, was formed by subduction‐related fluid metasomatism in the Palaeoproterozoic, which resulted from final cratonization of the NCC at ca. 1.8 Ga during assembly of Columbia supercontinent. Our observations also imply that similar mixed magma system with oxidized and sulphur‐rich signatures may be the key to the formation of hydrothermal polymetal deposits and the potential target for mineral exploration in some undiscovered areas. Copyright © 2012 John Wiley & Sons, Ltd.

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The Early Cretaceous sedimentary‐tectonic attributes of Lingshan Island Basin, East Shandong Province, China: Constraints from the chemical compositions of detrital heavy minerals

Gao

Zhong

2019

Geological Journal

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North China Craton experienced significant lithospheric destruction or delamination during the Late Mesozoic, accompanied with the emergence of numerous basins and intensive volcanism. Extensional basins also formed in East Shandong Province.Even though they have been studied for decades, the relationship between basin development and tectonic processes still remains obscure. Recently, a set of Early Cretaceous strata has been found in Lingshan Island. It is characterized by translating from turbidite deposits to terrestrial strata units and ending up with a unique volcaniclastic layer within a relatively short time span. Previous studies have reached an agreement that Lingshan Island strata are formed in a distinct sedimentary background compared with the coeval sedimentary units in Jiaolai Basin. Essential information about basin development and its tectonic setting in this region during Early Cretaceous are preserved in Lingshan Island strata. In this study, it shows the characteristics of heavy mineral assemblage and the characteristics of detrital minerals' chemical component in the two representative samples. Based on these studies, itindicates that Lingshan Island Basin was developed in a transpressional tectonic setting with complex source materials, mainly from Qianliyan Uplift during the period ca. 123-120 Ma. Then, the basin evolved within an extensional setting and was filled with locally derived clastics during 120 to 105 Ma. In addition, the basin evolved during the process of progressive lithospheric thinning and asthenosphere upwelling.

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Petrogenesis of Late Mesozoic mafic dykes in the Jiaodong Peninsula, eastern North China Craton and implications for the foundering of lower crust

Cited by 116 publications

References 115 publications

Petrogenesis of Early Cretaceous Magmatism in Eastern China and the Gyeongsang Basin, Korean Peninsula

Petrogenesis of Early Cretaceous Magmatism in Eastern China and the Gyeongsang Basin, Korean Peninsula

Origin of dyke swarms by mixing of metasomatized subcontinental lithospheric mantle‐derived and lower crustal magmas in the Guocheng fault belt, Jiaodong Peninsula, North China Craton

The Early Cretaceous sedimentary‐tectonic attributes of Lingshan Island Basin, East Shandong Province, China: Constraints from the chemical compositions of detrital heavy minerals

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