Chuan-Zhou Liu
Chinese Academy of Sciences
Network
Latest external collaboration on country level. Dive into details by clicking on the dots.
Publication
Featured researches published by Chuan-Zhou Liu.
Nature | 2008
Chuan-Zhou Liu; J. E. Snow; Eric Hellebrand; Gerhard Brügmann; Anette von der Handt; Anette Büchl; Albrecht W. Hofmann
The Earth’s mantle beneath ocean ridges is widely thought to be depleted by previous melt extraction, but well homogenized by convective stirring. This inference of homogeneity has been complicated by the occurrence of portions enriched in incompatible elements. Here we show that some refractory abyssal peridotites from the ultraslow-spreading Gakkel ridge (Arctic Ocean) have very depleted 187Os/188Os ratios with model ages up to 2 billion years, implying the long-term preservation of refractory domains in the asthenospheric mantle rather than their erasure by mantle convection. The refractory domains would not be sampled by mid-ocean-ridge basalts because they contribute little to the genesis of magmas. We thus suggest that the upwelling mantle beneath mid-ocean ridges is highly heterogeneous, which makes it difficult to constrain its composition by mid-ocean-ridge basalts alone. Furthermore, the existence of ancient domains in oceanic mantle suggests that using osmium model ages to constrain the evolution of continental lithosphere should be approached with caution.
The Journal of Geology | 2005
Wenjiao Xiao; Brian F. Windley; D. Y. Liu; Ping Jian; Chuan-Zhou Liu; Chao Yuan; Min Sun
Our new SHRIMP U‐Pb zircon ages from the Western Kunlun Orogen allow us to constrain the history of an active continental margin developed on the southern boundary of the Tarim block from the Ordovician to the Triassic. A \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace} \usepackage{amsmath,amsxtra} \usepackage[OT2,OT1]{fontenc} \newcommand\cyr{ \renewcommand\rmdefault{wncyr} \renewcommand\sfdefault{wncyss} \renewcommand\encodingdefault{OT2} \normalfont \selectfont} \DeclareTextFontCommand{\textcyr}{\cyr} \pagestyle{empty} \DeclareMathSizes{10}{9}{7}{6} \begin{document} \landscape
American Journal of Science | 2014
Fu-Yuan Wu; Wei-Qiang Ji; Jian-Gang Wang; Chuan-Zhou Liu; Sun-Lin Chung; Peter D. Clift
Geology | 2016
Chuan-Zhou Liu; Sun-Lin Chung; Fu-Yuan Wu; Chang Zhang; Yang Xu; Jian-Gang Wang; Yi Chen; Shun Guo
492\pm 7
Geology | 2014
Ling Chen; Mingming Jiang; Jin-Hui Yang; Zigen Wei; Chuan-Zhou Liu; Yuan Ling
Geology | 2011
Chuan-Zhou Liu; Fu-Yuan Wu; Sun-Lin Chung; Zhidan Zhao
\end{document} ‐Ma dacite from Yixieke extrusive rocks that contain \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace} \usepackage{amsmath,amsxtra} \usepackage[OT2,OT1]{fontenc} \newcommand\cyr{ \renewcommand\rmdefault{wncyr} \renewcommand\sfdefault{wncyss} \renewcommand\encodingdefault{OT2} \normalfont \selectfont} \DeclareTextFontCommand{\textcyr}{\cyr} \pagestyle{empty} \DeclareMathSizes{10}{9}{7}{6} \begin{document} \landscape
Geology | 2016
Wei-Qiang Ji; Fu-Yuan Wu; Sun-Lin Chung; Xuan-Ce Wang; Chuan-Zhou Liu; Qiu-Li Li; Zhi-Chao Liu; Xiao-Chi Liu; Jian-Gang Wang
Scientific Reports | 2015
Chuan-Zhou Liu; Fu-Yuan Wu; Sun-Lin Chung; Qiu-Li Li; Weidong Sun; Wei-Qiang Ji
220\pm 5
The Journal of Geology | 2012
Wei-Qiang Ji; Fu-Yuan Wu; Sun-Lin Chung; Chuan-Zhou Liu
Acta Geologica Sinica-english Edition | 2016
Tong Liu; Fuyuan Wu; Liang-Liang Zhang; Qingguo Zhai; Chuan-Zhou Liu; Wenbin Ji Ji; Chang Zhang; Yang Xu
\end{document} ‐Ma reheated zircons is interpreted as an intra‐oceanic arc complex that accreted to the Tarim block. The Yirba granodiorite has a continental arc geochemical signature, a \documentclass{aastex} \usepackage{amsbsy} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{bm} \usepackage{mathrsfs} \usepackage{pifont} \usepackage{stmaryrd} \usepackage{textcomp} \usepackage{portland,xspace} \usepackage{amsmath,amsxtra} \usepackage[OT2,OT1]{fontenc} \newcommand\cyr{ \renewcommand\rmdefault{wncyr} \renewcommand\sfdefault{wncyss} \renewcommand\encodingdefault{OT2} \normalfont \selectfont} \DeclareTextFontCommand{\textcyr}{\cyr} \pagestyle{empty} \DeclareMathSizes{10}{9}{7}{6} \begin{document} \landscape