Geochemistry, U-Pb dating, and Lu-Hf isotopes of zircon and monazite of porphyritic granites within the Jiao-Liao-Ji orogenic belt: Implications for petrogenesis and tectonic setting

Liu, Fulai; Liu, Chaohui; Itano, Keita; Iizuka, Tsuyoshi; Cai, Jia; Wang, Fang

doi:10.1016/j.precamres.2017.08.007

Cited by 74 publications

(26 citation statements)

References 86 publications

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“…Data from previous studies and this paper on the Palaeoproterozoic granites (Li et al, 2006;Liu, Liu, Itano, et al, 2017;Lu et al, 2005;Wang, Peng, Wang, & Yang, 2017;Yang et al, 2007;Zhang et al, 2016) Wang, Peng, Wang, & Yang, 2017 Mafeng Hornblende monzogranite SIMS 20 2,181 ± 6 Ma Mafeng Town, Haicheng City, Liaoning Province Wang, Peng, Wang, & Yang, 2017 Laoheishan Wang, Peng, Wang, & Yang, 2017 Mingan…”

Section: Geochronological Framework Of the Palaeoproterozoic Granitmentioning

confidence: 87%

“…The coeval 1.89-1.86 Ga granites in this paper were plotted into syn-collisional granite field (Figure 9), provides new understandings on the tectonic evolution in the Kuandian area within the JLJB. Triggered by the collapse of the thickened crust, anatexis and magmatism occurred in 1.89-1.86 Ga and lead to the regionalscale granite intrusion including the S-type porphyritic granites (Li et al, 2011;Liu, Liu, Itano, et al, 2017), I-type granites this paper). As that process involved contemporaneous intrusion of I-type and the S-type granites in the JLJB, a subduction geodynamic model is preferred.…”

Section: Implications For the Tectonic Evolution Of The Jljbmentioning

confidence: 94%

“…Although the granite samples were plotted into the boundary of Atype and I-and S-type granites in the geochemical discrimination diagrams, and all data for granite samples in this paper showed features between I-type and S-type granites in the P 2 O 5 versus SiO 2 diagram, we conclude these granites are I-type granites due to the observation of the many apatite grains under the microscope. (Liu, Liu, Itano, et al, 2017;Lu et al, 2005;Zhang et al, 2016).…”

Section: Zircon Lu-hf Isotopic Characteristicsmentioning

confidence: 99%

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Geochemistry of two types of Palaeoproterozoic granites, and zircon U–Pb dating, and Lu–Hf isotopic characteristics in the Kuandian area within the Jiao‐Liao‐Ji Belt: Implications for regional tectonic setting

Zhao

Zhang

et al. 2020

Geological Journal

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Palaeoproterozoic granites accompanied with granulite‐facies gneisses can be recognized in the Kuandian area, northern Jiao‐Liao‐Ji Belt (JLJB). This study highlights two episodes of Palaeoproterozoic magmatism, identified by granites and biotite monzogranitic gneisses herein. Zircon grains from biotite monzogranitic gneiss with homogeneous oscillatory zoning yielded a U–Pb age of 2,153 ± 16 Ma, in accordance with the age of zircon cores from the monzogranitic gneiss. Zircon grains from the two granites yielded upper intercept ages of 1,892 ± 38 Ma and 1,859 ± 36 Ma respectively. Monzogranitic gneiss samples are enriched in Th, Rb, Pb, U, and REE, but depleted in Sr and P. They have high 1,000 × Ga/Al ratios versus Zr, Ce, Nb, Y contents, which are usually interpreted as the features of classical A‐type granite that originated in a lithospheric extension setting. The ~1.89–1.86 Ga granite samples have relatively high Al, Rb, Th, U and low Sr, Zr, and Hf contents. These features, combined with the observation of minor apatite grains under the microscope are similar with the I‐type granites. In situ zircon Lu–Hf isotopic analyses revealed that ~1.89–1.86 Ga granite had a similar range and TDM2 ages with the monzogranitic gneiss, but with much lower εHf(t) values. The monzogranitic gneiss may have originated from an Archean crust, while the later granite may be derived from melting of the partial melting of the monzogranitic gneiss or the Archean crust that generated the monzogranitic gneiss. The ~1.89–1.86 Ga granites, together with the coeval S‐type granites in the JLJB, represent an orogeny process that may involve a Palaeoproterozoic subduction.

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Section: Geochronological Framework Of the Palaeoproterozoic Granitmentioning

confidence: 87%

Section: Implications For the Tectonic Evolution Of The Jljbmentioning

confidence: 94%

Section: Zircon Lu-hf Isotopic Characteristicsmentioning

confidence: 99%

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Geochemistry of two types of Palaeoproterozoic granites, and zircon U–Pb dating, and Lu–Hf isotopic characteristics in the Kuandian area within the Jiao‐Liao‐Ji Belt: Implications for regional tectonic setting

Zhao

Zhang

et al. 2020

Geological Journal

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“…The other group composed of post‐tectonic syenites, granitic pegmatites, and porphyritic granites have zircon U–Pb ages of ca. 1.85 Ga (Liu, Liu, et al, ; H. Yang, Wang, & Liu, ; J. H. Yang, Wu, Xie, & Liu, ). The present study area in the Anshan–Helan–Lianshanguan area is located in the northern segment of the JLJB and is dominantly composed of the North Liaohe Group.…”

Section: Regional Geologymentioning

confidence: 99%

Palaeoproterozoic tectonic evolution of the Jiao–Liao–Ji Belt, North China Craton: Geochemical and isotopic evidence from ca. 2.17 Ga felsic tuff

Liu

Wang

et al. 2019

Geological Journal

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The Palaeoproterozoic tectonic evolution of the Jiao-Liao-Ji Belt (JLJB) in the North China Craton remains controversial, particularly in the absence of adequate evidence for oceanic plate subduction. Here, we report SHRIMP U-Pb zircon ages, whole-rock geochemistry, and Sm-Nd isotope data on felsic tuffs from the Anshan-Helan-Lianshanguang area in the Liaodong Peninsula which provides important insights into the early tectonic evolution of the JLJB. The zircon SHRIMP U-Pb ages suggest formation of the tuffs crystallized at ca. 2.17 Ga, which coincide with the crystallization of the voluminous Liaoji granitoids in this belt. The felsic tuffs show calc-alkaline features and are characterized by a wide range of SiO 2 (61.89-72.55 wt.%), MgO (1.35-5.80 wt.%), Cr (36.0-67.8 ppm) and Ni (5.88-28.8 ppm) contents, and low TiO 2 (0.42-0.64 wt.%) and total Fe 2 O 3 (2.14-5.64 wt.%) concentrations. They also display enrichment in LREE and depletion in Nb, Ta, and Ti similar to the features of continental arc andesites. Their wide variation in whole-rock εNd(t) (−2.6 to +3.4)combined with the synchronous magmatic activity in this region suggests that they were derived from mixing of mafic (e.g., those in the Liaohe suite) and felsic (e.g., the Liaoji granitoids) magmas, followed by fractional crystallization. In view of the widespread distribution of magmatism, including the Helan felsic tuffs and Liaoji granitoids, and the synchronous sedimentary rocks in the Liaodong Peninsula, we propose that the evolution of the JLJB involved an initial back-arc extension stage, followed by arc-continent collision. KEYWORDS back-arc and arc-continent collision, felsic tuff, Jiao-Liao-Ji Belt, Liaohe Group, North China Craton, Palaeoproterozoic

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“…1). Previous geochronological studies in the belt showed that most of the supracrustal successions and pre-tectonic granitoids formed during 2.20-2.10 Ga and were metamorphosed and deformed during 1.95-1.90 Ga (Luo et al 2004(Luo et al , 2008Li et al 2005;Lu et al 2006Lu et al , 2004Li & Zhao, 2007;Zhou et al 2008b;Tam et al 2011;Liu et al 2012aLiu et al , 2013c, whereas the post-tectonic granites were emplaced at 1.88-1.83 Ga (Hao et al 2004;Lu et al 2006;Li & Zhao, 2007;Liu et al 2017b). The Jiaobei Terrane, considered as the south segment of the JLJB (Zhao et al 2005), is bounded by the Tan-Lu Fault to the NW and the Wulian-Yantai Fault to the SE, the latter being commonly regarded as the boundary between the NCC and South China Craton (Wallis et al 1999;Tang et al 2007;Zhang et al 2014).…”

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confidence: 99%

A Palaeoarchean–Mesoarchean micro-continent entrained in the Jiao-Liao-Ji Belt at the southeastern North China Craton: evidence from the zircon record in the Bengbu area

et al. 2019

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The Bengbu area in the southeastern North China Craton (NCC) consists predominantly of Archean–Palaeoproterozoic (gneissic) granitoids with minor supracrustal rocks (the Fengyang and Wuhe groups). This study presents new zircon laser ablation – inductively coupled plasma – mass spectrometry U–Pb and Lu–Hf isotopic data and trace-element contents for these granitoids, which improve understanding the Archean–Palaeoproterozoic crustal evolution of the NCC. Magmatic zircon U–Pb data reveal that zircons in the (gneissic) granitoids were generated by multi-stage events at 2.93, 2.73, 2.53–2.52 and 2.18–2.13 Ga. Metamorphic zircon U–Pb data obtained from these rocks show two distinct metamorphic ages of 2.49–2.52 and 1.84 Ga, suggesting that the Bengbu area experienced a regional metamorphic event at the end of the Neoarchean Era and encountered reworking by a tectonothermal event associated with the formation of the Palaeoproterozoic Jiao-Liao-Ji Belt. Trace-element compositions of magmatic zircons reveal the highest Ti concentrations (8.08±3.38 ppm) and growth temperatures (718±44 °C) for the zircons aged 2.13–2.17 Ga and an increase in zircon U/Yb ratios from 2.93 Ga (0.34±0.12) through 2.73 Ga (0.96±0.42) to 2.53 Ga (1.05±0.46), but an evident decrease at 2.17–2.13 Ga (0.61±0.40 ppm). Similar Palaeoarchean xenocrystic and detrital zircons with negativeɛHf(t) values, late Mesoarchean magmatic zircons with juvenile Hf isotopic features, early Neoarchean magmatic zircons with model ages of 2.9–3.0 Ga, and two regional metamorphic events at 2.52–2.48 and 1.88–1.80 Ga in the Bengbu and Jiaobei areas indicate a Palaeoarchean–Mesoarchean micro-continent entrained in the Jiao-Liao-Ji Belt at the southeastern NCC.

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Geochemistry, U-Pb dating, and Lu-Hf isotopes of zircon and monazite of porphyritic granites within the Jiao-Liao-Ji orogenic belt: Implications for petrogenesis and tectonic setting

Cited by 74 publications

References 86 publications

Geochemistry of two types of Palaeoproterozoic granites, and zircon U–Pb dating, and Lu–Hf isotopic characteristics in the Kuandian area within the Jiao‐Liao‐Ji Belt: Implications for regional tectonic setting

Geochemistry of two types of Palaeoproterozoic granites, and zircon U–Pb dating, and Lu–Hf isotopic characteristics in the Kuandian area within the Jiao‐Liao‐Ji Belt: Implications for regional tectonic setting

Palaeoproterozoic tectonic evolution of the Jiao–Liao–Ji Belt, North China Craton: Geochemical and isotopic evidence from ca. 2.17 Ga felsic tuff

A Palaeoarchean–Mesoarchean micro-continent entrained in the Jiao-Liao-Ji Belt at the southeastern North China Craton: evidence from the zircon record in the Bengbu area

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