Geochemistry, zircon U-Pb chronology and Hf isotope composition of the Heishan’gou iron deposit in the Bikou Terrane, central China: Implication for the genesis of the Yudongzi banded iron formations
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H. Ye | M. Brzozowski | Xiaohui Sun | Chan Wu | Y. Luan | Tianbing Zhang
[1] Weiqiang Li,et al. Genesis of the Fulu Cryogenian iron formation in South China: Synglacial or interglacial? , 2022, Precambrian Research.
[2] San-zhong Li,et al. Trace element and isotope (C, S, Sr, Nd, Fe) geochemistry constraints on the sedimentary environment of the early Neoproterozoic Shilu BIF and associated dolostones, South China , 2022, Precambrian Research.
[3] Yunpeng Dong,et al. Petrogenesis and tectonic implications of the Neoproterozoic mafic intrusions in the Bikou Terrane along the northwestern margin of the Yangtze Block, South China , 2021, Ore Geology Reviews.
[4] F. Pirajno,et al. Cycles of hydrothermal activity, precipitation of chemical sediments, with special reference to Algoma-type BIF , 2021 .
[5] M. Bau,et al. Banded iron formation from Antarctica: The 2.5 Ga old Mt. Ruker BIF and the antiquity of lanthanide tetrad effect and super-chondritic Y/Ho ratio in seawater , 2020 .
[6] Chang‐Zhi Wu,et al. Neoproterozoic non-glaciogenic iron formation: Insights from Fe isotope and elemental geochemistry of the Shalong iron formation from the Central Tianshan block, southern Altaids , 2020 .
[7] F. Gao,et al. Further constraints on a Neoproterozoic active continental margin from sandstones of the Hengdan Group in the Bikou Terrane, northwestern margin of the Yangtze Block, South China , 2020 .
[8] Jun Hu,et al. U-Pb zircon geochronology and geochemistry of metavolcanics and associated iron ores of the magnetite-rich BIF deposits in the Western Kunlun orogenic belt: Constraints on the depositional age, origin and tectonic setting , 2020 .
[9] G. Shields,et al. Termination of Cryogenian ironstone deposition by deep ocean euxinia , 2020 .
[10] Lianchang Zhang,et al. Geochemistry of meta-sedimentary rocks associated with the Neoarchean Dagushan BIF in the Anshan-Benxi area, North China Craton: Implications for their provenance and tectonic setting , 2019, Precambrian Research.
[11] Jun Wang,et al. Episodic crustal growth and reworking of the Yudongzi terrane, South China: Constraints from the Archean TTGs and potassic granites and Paleoproterozoic amphibolites , 2019, Lithos.
[12] M. Santosh,et al. The Neoproterozoic “Blood Falls” in Tarim Craton and Their Possible Connection With Snowball Earth , 2019, Journal of Geophysical Research: Earth Surface.
[13] M. Santosh,et al. Discovery of the Huronian Glaciation Event in China: Evidence from glacigenic diamictites in the Hutuo Group in Wutai Shan , 2019, Precambrian Research.
[14] T. Zhao,et al. Geochemistry, U-Pb zircon geochronology and Sm-Nd isotopes of the Xincai banded iron formation in the southern margin of the North China Craton: Implications on Neoarchean seawater compositions and solute sources , 2017, Precambrian Research.
[15] N. Planavsky,et al. Origin of the Neoproterozoic Fulu iron formation, South China: Insights from iron isotopes and rare earth element patterns , 2018, Geochimica et Cosmochimica Acta.
[16] Jianping Zheng,et al. Identification of ca. 2.65 Ga TTGs in the Yudongzi complex and its implications for the early evolution of the Yangtze Block , 2018, Precambrian Research.
[17] N. Planavsky,et al. Earth’s youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean , 2018, Scientific Reports.
[18] Dunyi Liu,et al. Formation and evolution of the Archean continental crust of China: A review , 2018 .
[19] T. Yang,et al. Updating the Geologic Barcodes for South China: Discovery of Late Archean Banded Iron Formations in the Yangtze Craton , 2017, Scientific Reports.
[20] Yunpeng Dong,et al. Zircon U–Pb chronology, Hf isotope analysis and whole-rock geochemistry for the Neoarchean-Paleoproterozoic Yudongzi complex, northwestern margin of the Yangtze craton, China , 2017 .
[21] M. Santosh,et al. Volcano-sedimentary and metallogenic records of the Dharwar greenstone terranes, India: Window to Archean plate tectonics, continent growth, and mineral endowment , 2017 .
[22] Honglin Yuan,et al. Development of pressed sulfide powder tablets for in situ sulfur and lead isotope measurement using LA-MC-ICP-MS , 2017 .
[23] A. Bekker,et al. Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history , 2017 .
[24] Yan‐jing Chen,et al. Trace elements of magnetite and iron isotopes of the Zankan iron deposit, westernmost Kunlun, China: A case study of seafloor hydrothermal iron deposits , 2017 .
[25] G. Cox,et al. A model for Cryogenian iron formation , 2016 .
[26] Yunpeng Dong,et al. Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China , 2016 .
[27] Weiqiang Li,et al. Biologically recycled continental iron is a major component in banded iron formations , 2015, Proceedings of the National Academy of Sciences.
[28] Yaowu Song,et al. Magma mixing and crust–mantle interaction in the Triassic monzogranites of Bikou Terrane, central China: Constraints from petrology, geochemistry, and zircon U–Pb–Hf isotopic systematics , 2015 .
[29] P. Nadoll,et al. Geochemistry of magnetite from porphyry Cu and skarn deposits in the southwestern United States , 2015, Mineralium Deposita.
[30] D. French,et al. The chemistry of hydrothermal magnetite: A review , 2014 .
[31] Xiaoqing Zhu,et al. The Gongchangling BIFs from the Anshan–Benxi area, NE China: Petrological–geochemical characteristics and genesis of high-grade iron ores , 2014 .
[32] Zuoheng Zhang,et al. Spatio-temporal distribution and tectonic settings of the major iron deposits in China: An overview , 2014 .
[33] Jing Chen,et al. Types and general characteristics of the BIF-related iron deposits in China , 2014 .
[34] E. Bellefroid,et al. Neoproterozoic iron formation: An evaluation of its temporal, environmental and tectonic significance , 2013 .
[35] D. Davis,et al. 2.1–1.85 Ga tectonic events in the Yangtze Block, South China: Petrological and geochronological evidence from the Kongling Complex and implications for the reconstruction of supercontinent Columbia , 2013 .
[36] Yan‐jing Chen,et al. Global glaciations and atmospheric change at ca.2.3 Ga , 2013 .
[37] Guochun Zhao,et al. Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications , 2013 .
[38] Tao Yang,et al. REE geochemistry of carbonates from the Guanmenshan Formation, Liaohe Group, NE Sino-Korean Craton: Implications for seawater compositional change during the Great Oxidation Event , 2013 .
[39] Janisar M. Sheikh,et al. Geochemistry of pillow basalts from Bompoka, Andaman–Nicobar islands, Bay of Bengal, India , 2013 .
[40] Shan Gao,et al. 2.6–2.7 Ga crustal growth in Yangtze craton, South China , 2013 .
[41] Peter A. Cawood,et al. Precambrian geology of China , 2012 .
[42] Peter A. Cawood,et al. Amalgamation of the North China Craton: Key issues and discussion , 2012 .
[43] Lianchang Zhang,et al. Formation age and tectonic setting of the Shirengou Neoarchean banded iron deposit in eastern Hebei Province: Constraints from geochemistry and SIMS zircon U–Pb dating , 2012 .
[44] Zhou Hongying,et al. Formation Ages of Early Precambrian BIFs in the North China Craton:SHRIMP Zircon U-Pb Dating , 2012 .
[45] Shen Baofeng. Geological Characters and Resource Prospect of the BIF Type Iron Ore Deposits in China , 2012 .
[46] Lianchang Zhang,et al. Zircon U–Pb age, Hf isotopes and geochemistry of Shuichang Algoma-type banded iron-formation, North China Craton: Constraints on the ore-forming age and tectonic setting , 2011 .
[47] Yan‐jing Chen,et al. Paleoproterozoic positive δ13Ccarb excursion in the northeastern Sino-Korean craton: Evidence of the Lomagundi Event , 2011 .
[48] Wang Hongliang. Constraints from Zircon U-Pb Chronology of Yudongzi Group Magnetite-Quartzite in the Lueyang Area,Southern Qinling,China , 2011 .
[49] L. Yongsheng,et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS , 2010 .
[50] Noah J. Planavsky,et al. Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic, and Biospheric Processes , 2010 .
[51] Liang Ting. Zircon LA-ICP-MS U-Pb dating and significance of Yudongzi Group deformation granite from Lueyang area,western Qinling,China , 2010 .
[52] M. Bau,et al. Distribution of high field strength elements (Y, Zr, REE, Hf, Ta, Th, U) in adjacent magnetite and chert bands and in reference standards FeR-3 and FeR-4 from the Temagami iron-formation, Canada, and the redox level of the Neoarchean ocean , 2009 .
[53] Shang Gao,et al. Zircon U–Pb age, trace element and Hf isotope composition of Kongling terrane in the Yangtze Craton: refining the timing of Palaeoproterozoic high‐grade metamorphism , 2009 .
[54] A. Gerdes,et al. Zircon formation versus zircon alteration — New insights from combined U–Pb and Lu–Hf in-situ LA-ICP-MS analyses, and consequences for the interpretation of Archean zircon from the Central Zone of the Limpopo Belt , 2009 .
[55] R. Frei,et al. Trace element and isotopic characterization of Neoarchean and Paleoproterozoic iron formations in the Black Hills (South Dakota, USA): Assessment of chemical change during 2.9–1.9 Ga deposition bracketing the 2.4–2.2 Ga first rise of atmospheric oxygen , 2008 .
[56] D. Günther,et al. Simultaneous determinations of U–Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-ablation quadrupole and multiple-collector ICP-MS , 2008 .
[57] P. Andersson,et al. Continentally-derived solutes in shallow Archean seawater: Rare earth element and Nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa , 2008 .
[58] D. Lascelles. Black smokers and density currents: A uniformitarian model for the genesis of banded iron-formations , 2007 .
[59] A. Vaughan,et al. The source of granitic gneisses and migmatites in the Antarctic Peninsula: a combined U–Pb SHRIMP and laser ablation Hf isotope study of complex zircons , 2006 .
[60] C. Klein. Some Precambrian banded iron-formations (BIFs) from around the world: Their age, geologic setting, mineralogy, metamorphism, geochemistry, and origins , 2005 .
[61] S. Wilde,et al. Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited , 2005 .
[62] Yong‐Fei Zheng,et al. Genesis of zircon and its constraints on interpretation of U-Pb age , 2004 .
[63] M. Whitehouse,et al. Characterisation of early Archaean chemical sediments by trace element signatures , 2004 .
[64] G. Logan,et al. Barite, BIFs and bugs: evidence for the evolution of the Earth’s early hydrosphere , 2004 .
[65] W. Bleeker. The late Archean record: a puzzle in ca. 35 pieces , 2003 .
[66] C. Isachsen,et al. The decay constant of 176Lu determined from Lu-Hf and U-Pb isotope systematics of terrestrial Precambrian high-temperature mafic intrusions , 2003 .
[67] T. Kano,et al. Negative Ce Anomaly in the Indian Banded Iron Formations: Evidence for the Emergence of Oxygenated Deep‐Sea at 2.9‐2.7 Ga , 2002 .
[68] Zhang Zongqing. On the Age of Metamorphic Rocks of the Yudongzi Group and the Archean Crystalline Basement of the Qinling Orogen , 2001 .
[69] W. Griffin,et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites , 2000 .
[70] D. Abbott,et al. Plume‐related mafic volcanism and the deposition of banded iron formation , 1999 .
[71] P. Dulski,et al. Comparing yttrium and rare earths in hydrothermal fluids from the Mid-Atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater , 1999 .
[72] Y. Nozaki,et al. Rare earth elements in seawater: particle association, shale-normalization, and Ce oxidation , 1999 .
[73] R. Powell,et al. Calculating phase diagrams involving solid solutions via non‐linear equations, with examples using THERMOCALC , 1998 .
[74] M. Basei,et al. SHRIMP zircon U–Pb constraints on the age of the Carajás formation, Grão ParáGroup, Amazon Craton , 1998 .
[75] F. Albarède,et al. “The Lu–Hf isotope geochemistry of chondrites and the evolution of the mantle–crust system”: [Earth Planet. Sci. Lett. 148 (1997) 243–258]1 , 1998 .
[76] Chen Yanjing,et al. Geochemical characteristics and evolution of REE in the Early Precambrian sediments : evidence from the southern margin of the North China Craton , 1997 .
[77] T. Kano,et al. Rare-earth element geochemistry of banded iron formations and associated amphibolite from the Sargur belts, south India , 1996 .
[78] P. Dulski,et al. Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa , 1996 .
[79] A. Koschinsky,et al. Comparison of the partitioning behaviours of yttrium, rare earth elements, and titanium between hydrogenetic marine ferromanganese crusts and seawater , 1996 .
[80] S. M. Naqvi,et al. Geochemistry, depositional environment and tectonic setting of the BIF's of the Late Archaean Chitradurga Schist Belt, India , 1995 .
[81] C. German,et al. Dissolved rare earth elements in the Southern Ocean: Cerium oxidation and the influence of hydrography , 1995 .
[82] J. Edmond,et al. Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges , 1994 .
[83] M. Bau. Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium , 1991 .
[84] C. German,et al. Redox cycling of rare earth elements in the suboxic zone of the Black Sea , 1991 .
[85] J. Monger,et al. Anatomy of North America: thematic geologic portrayals of the continent , 1991 .
[86] G. Kelling,et al. Geochemistry and tectonic environment of basaltic rocks from the Misis ophiolitic mélange, south Turkey , 1991 .
[87] 陈衍景,et al. VARIATION OF REE PATTERNS IN EARLY PRECAMBRIAN SEDIMENTS——THEORETICAL STUDY AND EVIDENCE FROM THE SOUTHERN MARGIN OF THE NORTH CHINA CRATON , 1991 .
[88] Scott M. McLennan,et al. Rare earth elements in sedimentary rocks; influence of provenance and sedimentary processes , 1989 .
[89] W. McDonough,et al. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.
[90] J. D. Wonder,et al. Geochemistry and origin of manganese-rich rocks related to iron-formation and sulfide deposits, western Georgia , 1988 .
[91] G. Gross. Tectonic Systems and the Deposition of Iron-Formation , 1983 .
[92] Julian A. Pearce,et al. Tectonic setting of basic volcanic rocks determined using trace element analyses , 1973 .
[93] B. Leake,et al. Report. Nomenclature of Amphiboles: Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names , 1971, Mineralogical Magazine.
[94] J. Lovering,et al. Metamorphic and metasomatic convergence of basic igneous rocks and lime‐magnesia sediments of the precambrian of North‐western Queensland∗ , 1959 .
[95] H. L. James. Sedimentary facies of iron-formation , 1954 .