All Outputs (14)

The syncollisional granitoid magmatism and crust growth during the West Qinling Orogeny, China: Insights from the Jiaochangba pluton (2018)
Journal Article
Kong, J., Niu, Y., Duan, M., Xiao, Y., Zhang, Y., Guo, P., Sun, P., & Gong, H. (2019). The syncollisional granitoid magmatism and crust growth during the West Qinling Orogeny, China: Insights from the Jiaochangba pluton. Geological Journal, 54(6), 4014-4033. https://doi.org/10.1002/gj.3368

The West Qinling Orogenic Belt (WQOB) is a major portion of the Qinling‐Dabie‐Sulu Orogen and holds essential information for understanding the protracted evolution of the north‐eastern branch of the Paleo‐Tethys in East Asia. In this study, we repor... Read More about The syncollisional granitoid magmatism and crust growth during the West Qinling Orogeny, China: Insights from the Jiaochangba pluton.

Tectonic significance of Cretasceous granitoids along the southeast coast of continental China (2018)
Journal Article
Xue, Q., Niu, Y., Chen, S., Sun, P., Duan, M., Gao, Y., …Guo, P. (2020). Tectonic significance of Cretasceous granitoids along the southeast coast of continental China. Geological Journal, 55(1), 173-196. https://doi.org/10.1002/gj.3388

We present the results of our study on 16 Cretaceous granitoid plutons along the south‐east coast of continental China. The zircon U–Pb ages and the bulk‐rock Rb–Sr isochron age (R2 = 0.935) indicate that the granitoids represent the last episode of... Read More about Tectonic significance of Cretasceous granitoids along the southeast coast of continental China.

Heterogeneous oceanic arc volcanic rocks in the South Qilian Accretionary Belt (Qilian Orogen, NW China) (2018)
Journal Article
Yang, L., Song, S., Su, L., Allen, M., Niu, Y., Zhang, G., & Zhang, Y. (2019). Heterogeneous oceanic arc volcanic rocks in the South Qilian Accretionary Belt (Qilian Orogen, NW China). Journal of Petrology, 60(1), 85-116. https://doi.org/10.1093/petrology/egy107

Primitive arc magmas in oceanic island arcs are probes of sub-arc magmatic processes and are crucial for understanding oceanic subduction. We report data for an Early Paleozoic oceanic arc volcanic complex in the Lajishan-Yongjing terrane, South Qili... Read More about Heterogeneous oceanic arc volcanic rocks in the South Qilian Accretionary Belt (Qilian Orogen, NW China).

Multiple mantle metasomatism beneath the Leizhou Peninsula, South China: Evidence from elemental and Sr-Nd-Pb-Hf isotope geochemistry of the late Cenozoic volcanic rocks (2018)
Journal Article
Sun, P., Niu, Y., Guo, P., Chen, S., Duan, M., Gong, H., …Xiao, Y. (2019). Multiple mantle metasomatism beneath the Leizhou Peninsula, South China: Evidence from elemental and Sr-Nd-Pb-Hf isotope geochemistry of the late Cenozoic volcanic rocks. International Geology Review, 61(14), 1768-1785. https://doi.org/10.1080/00206814.2018.1548307

We analysed whole-rock major and trace elements and Sr-Nd-Pb-Hf isotopes of the late Cenozoic volcanic rocks in the Leizhou Peninsula, South China to investigate their mantle source characteristics. These volcanic rocks, collected from Jiujiang, Tian... Read More about Multiple mantle metasomatism beneath the Leizhou Peninsula, South China: Evidence from elemental and Sr-Nd-Pb-Hf isotope geochemistry of the late Cenozoic volcanic rocks.

Origin of the Jurassic-cretaceous intraplate granitoids in Eastern China as a consequence of paleo-Pacific plate subduction (2018)
Journal Article
Hong, D., Niu, Y., Xiao, Y., Sun, P., Kong, J., Guo, P., …Chen, S. (2018). Origin of the Jurassic-cretaceous intraplate granitoids in Eastern China as a consequence of paleo-Pacific plate subduction. Lithos, 322, 405-419. https://doi.org/10.1016/j.lithos.2018.10.027

Jurassic-Cretaceous granitoids are widespread in eastern continental China and have been considered by many as resulting from paleo-Pacific subduction. However, the actual mechanism of their petrogenesis remains speculative. In order to address this... Read More about Origin of the Jurassic-cretaceous intraplate granitoids in Eastern China as a consequence of paleo-Pacific plate subduction.

Perovskite U-Pb and Sr-Nd isotopic perspectives on melilitite magmatism and outward growth of the Tibetan Plateau (2018)
Journal Article
Liu, D., Zhao, Z., Niu, Y., Zhu, D.-C., & Li, X.-H. (2018). Perovskite U-Pb and Sr-Nd isotopic perspectives on melilitite magmatism and outward growth of the Tibetan Plateau. Geology, 46(12), 1027-1030. https://doi.org/10.1130/g45329.1

Mantle-derived alkaline magmatism along major strike-slip faults provides unique insights into the lateral growth of the Tibetan Plateau. Here we use the geochemistry of perovskites from the West Qinling melilitite to probe into the nature and dynami... Read More about Perovskite U-Pb and Sr-Nd isotopic perspectives on melilitite magmatism and outward growth of the Tibetan Plateau.

HP-UHP metamorphic belt in the East Kunlun Orogen: final closure of the Proto-Tethys Ocean and formation of the Pan-North-China Continent (2018)
Journal Article
Song, S., Bi, H., Qi, S., Yang, L., Allen, M. B., Niu, Y., Su, L., & Li, W. (2018). HP-UHP metamorphic belt in the East Kunlun Orogen: final closure of the Proto-Tethys Ocean and formation of the Pan-North-China Continent. Journal of Petrology, 59(11), 2043-2060. https://doi.org/10.1093/petrology/egy089

The East Kunlun Orogen, the northwestern part of the Central China Orogenic Belt, is a long-lived accretionary orogenic belt that records the evolution and eventual destruction of branches of the Tethys Ocean, from the Cambrian to the Triassic. Here... Read More about HP-UHP metamorphic belt in the East Kunlun Orogen: final closure of the Proto-Tethys Ocean and formation of the Pan-North-China Continent.

The petrological control on the lithosphere-asthenosphere boundary (LAB) beneath ocean basins (2018)
Journal Article
Niu, Y., & Green, D. H. (2018). The petrological control on the lithosphere-asthenosphere boundary (LAB) beneath ocean basins. Earth-Science Reviews, 185, 301-307. https://doi.org/10.1016/j.earscirev.2018.06.011

The plate tectonics theory established ~ 50 years ago has formed a solid framework for understanding how the earth works on all scales. In this theory, movement of the tectonic plates relative to the subjacent asthenosphere is one of the fundamental... Read More about The petrological control on the lithosphere-asthenosphere boundary (LAB) beneath ocean basins.

Provenance, depositional setting, and crustal evolution of the Cathaysia Block, South China: Insights from detrital zircon U–Pb geochronology and geochemistry of clastic rocks (2018)
Journal Article
Xiong, C., Chen, H., Niu, Y., Chen, A., Zhang, C., Li, F., Xu, S., & Yang, S. (2019). Provenance, depositional setting, and crustal evolution of the Cathaysia Block, South China: Insights from detrital zircon U–Pb geochronology and geochemistry of clastic rocks. Geological Journal, 53(5), 1-16. https://doi.org/10.1002/gj.3253

We report the results of a combined study of detrital zircon U–Pb geochronology and bulk‐rock elemental geochemistry on late Neoproterozoic to Cambrian clastic sedimentary rocks from South Jiangxi within Cathaysia. These clastic rocks are characteriz... Read More about Provenance, depositional setting, and crustal evolution of the Cathaysia Block, South China: Insights from detrital zircon U–Pb geochronology and geochemistry of clastic rocks.

The evolution and ascent paths of mantle xenolith-bearing magma: Observations and insights from Cenozoic basalts in Southeast China (2018)
Journal Article
Sun, P., Niu, Y., Guo, P., Cui, H., Ye, L., & Liu, J. (2018). The evolution and ascent paths of mantle xenolith-bearing magma: Observations and insights from Cenozoic basalts in Southeast China. Lithos, 31-311, 171-181. https://doi.org/10.1016/j.lithos.2018.04.015

Studies have shown that mantle xenolith-bearing magmas must ascend rapidly to carry mantle xenoliths to the surface. It has thus been inferred inadvertently that such rapid ascending melt must have undergone little crystallization or evolution. Howev... Read More about The evolution and ascent paths of mantle xenolith-bearing magma: Observations and insights from Cenozoic basalts in Southeast China.

Origin of the LLSVPs at the base of the mantle is a consequence of plate tectonics – A petrological and geochemical perspective (2018)
Journal Article
Niu, Y. (2018). Origin of the LLSVPs at the base of the mantle is a consequence of plate tectonics – A petrological and geochemical perspective. Geoscience Frontiers, 9(5), 1265-1278. https://doi.org/10.1016/j.gsf.2018.03.005

In studying the petrogenesis of intra-plate ocean island basalts (OIB) associated with hotspots or mantle plumes, we hypothesized that the two large-low-shear-wave-velocity provinces(LLSVPs) at the base of the mantle beneath the Pacific (Jason) and A... Read More about Origin of the LLSVPs at the base of the mantle is a consequence of plate tectonics – A petrological and geochemical perspective.

Two epochs of eclogite metamorphism link ‘cold’ oceanic subduction and ‘hot’ continental subduction, the North Qaidam UHP belt, NW China (2018)
Journal Article
Song, S., Niu, Y., Zhang, G., & Zhang, L. (2018). Two epochs of eclogite metamorphism link ‘cold’ oceanic subduction and ‘hot’ continental subduction, the North Qaidam UHP belt, NW China. Geological Society Special Publications, 474, 1-15. https://doi.org/10.1144/sp474.2

Eclogites in the high-pressure (HP) and ultrahigh-pressure (UHP) belts record subduction-zone processes; exhumed eclogites of seafloor protoliths record low-temperature (mostly <600°C), high-pressure and ‘wet’ environments: that is, relatively ‘cold’... Read More about Two epochs of eclogite metamorphism link ‘cold’ oceanic subduction and ‘hot’ continental subduction, the North Qaidam UHP belt, NW China.

Syn-collisional felsic magmatism and continental crust growth: A case study from the North Qilian Orogenic Belt at the northern margin of the Tibetan Plateau (2018)
Journal Article
Chen, S., Niu, Y., & Xue, Q. (2018). Syn-collisional felsic magmatism and continental crust growth: A case study from the North Qilian Orogenic Belt at the northern margin of the Tibetan Plateau. Lithos, 308-309, 53-64. https://doi.org/10.1016/j.lithos.2018.03.001

The abundant syn-collisional granitoids produced and preserved at the northern Tibetan Plateau margin provide a prime case for studying the felsic magmatism as well as continental crust growth in response to continental collision. Here we present the... Read More about Syn-collisional felsic magmatism and continental crust growth: A case study from the North Qilian Orogenic Belt at the northern margin of the Tibetan Plateau.

Mesozoic high-Mg andesites from the Daohugou area, Inner Mongolia: Upper-crustal fractional crystallization of parental melt derived from metasomatized lithospheric mantle wedge (2018)
Journal Article
Meng, F., Gao, S., Song, Z., Niu, Y., & Li, X. (2018). Mesozoic high-Mg andesites from the Daohugou area, Inner Mongolia: Upper-crustal fractional crystallization of parental melt derived from metasomatized lithospheric mantle wedge. Lithos, 302-303, 535-548. https://doi.org/10.1016/j.lithos.2018.01.032

Mineral chemistry, major- and trace-element data, zircon U–Pb ages, and Sr–Nd isotopic data are presented for a suite of volcanic rocks from the Daohugou area, Ningcheng City, Inner Mongolia, on the northern margin of the North China Craton. Samples... Read More about Mesozoic high-Mg andesites from the Daohugou area, Inner Mongolia: Upper-crustal fractional crystallization of parental melt derived from metasomatized lithospheric mantle wedge.