Fluorite REE characteristics of the Diyanqinamu Mo deposit, Inner Mongolia, China
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[1] Zhilong Huang,et al. GEOLOGY, Re-Os AGES, SULFUR AND LEAD ISOTOPES OF THE DIYANQINAMU PORPHYRY Mo DEPOSIT, INNER MONGOLIA, NE CHINA , 2015 .
[2] L. Ye,et al. Geochronological, isotopic and mineral geochemical constraints on the genesis of the Diyanqinamu Mo deposit, Inner Mongolia, China , 2015 .
[3] Zhilong Huang,et al. Chronology, geochemistry and Sr–Nd isotope studies of Jurassic intrusions in the Diyanqinamu porphyry Mo mine, central Inner Mongolia, China , 2014 .
[4] R. Rudnick,et al. Composition of the Continental Crust , 2014 .
[5] Sun He. A Model for Alteration Zoning of Hydrothermal Mineralization Based on Surpac Software for the Diyanqinamu Mo Mine District,Inner Mongolia , 2012 .
[6] Farhad Ehya. Variation of mineralizing fluids and fractionation of REE during the emplacement of the vein-type fluorite deposit at Bozijan, Markazi Province, Iran , 2012 .
[7] H. Dill,et al. REE contents, REE minerals and Sm/Nd isotopes of granite- and unconformity-related fluorite mineralization at the western edge of the Bohemian Massif: With special reference to the Nabburg-Wölsendorf District, SE Germany , 2011 .
[8] Huang Zhilong,et al. Trace Elements and Rare Earth Elements of Sulfide Minerals in the Tianqiao Pb‐Zn Ore Deposit, Guizhou Province, China , 2011 .
[9] L. Zhang. Distribution of Uranium and Molybdenum Deposits and Their Relations with Medium Massifs in Central Asian Orogenic Zone , 2011 .
[10] Nie Xiu-lan. The Discovery of the Diyanqinamu Large-Size Mo-Ag Deposit,Inner Mongolia,and Its Geological Significance , 2010 .
[11] Xue Huai. The Xilingeie complex from the eastern part of the Central Asian-Mongolia Orogenic Belt, China: Products of Early Variscan orogeny other than ancient block: Evidence from zircon SHRIMP U-Pb ages. , 2009 .
[12] F. Castorina,et al. Trace-element and Sr-Nd isotopic evidence for the origin of the Sardinian fluorite mineralization (Italy) , 2008 .
[13] Yang Zhi. Direct record of primary fluid exsolved from magma:Evidence from unidirectional solidification texture(UST) in quartz found in Qulong porphyry copper deposit,Tibet , 2008 .
[14] R. Moritz,et al. The use of vein fluorite as probe for paleofluid REE and Sr-Nd isotope geochemistry : The Santa Catarina Fluorite District, southern Brazil , 2005 .
[15] G. Markl,et al. REE systematics in hydrothermal fluorite , 2005 .
[16] R. Romer,et al. Tracing element sources of hydrothermal mineral deposits: REE and Y distribution and Sr-Nd-Pb isotopes in fluorite from MVT deposits in the Pennine Orefield, England , 2003 .
[17] A. Williams-Jones,et al. COMPOSITIONAL HETEROGENEITY IN FLUORITE AND THE GENESIS OF FLUORITE DEPOSITS: INSIGHTS FROM LA-ICP-MS ANALYSIS , 2003 .
[18] R. Rudnick,et al. 3.01 – Composition of the Continental Crust , 2003 .
[19] Hong-Ju Da. Metallogenic Province Derived from Mantle Sources: A Case Study of Central Asian Orogenic Belt , 2003 .
[20] A. Brachmann,et al. Stabilisation of divalent rare earth elements in natural fluorite , 2002 .
[21] R. Hannigan,et al. The development of middle rare earth element enrichments in freshwaters: weathering of phosphate minerals , 2001 .
[22] D. Aubert,et al. REE fractionation during granite weathering and removal by waters and suspended loads: Sr and Nd isotopic evidence , 2001 .
[23] Martin L. Smith,et al. Fractionation of the REE during hydrothermal processes: Constraints from the Bayan Obo Fe-REE-Nb deposit, Inner Mongolia, China , 2000 .
[24] D. Grégoire,et al. Determination of Trace Elements in Twenty Six Chinese Geochemistry Reference Materials by Inductively Coupled Plasma‐Mass Spectrometry , 2000 .
[25] P. Kyle,et al. Geochemistry of southwestern New Mexico fluorite occurrences implications for precious metals exploration in fluorite-bearing systems , 2000 .
[26] W. Prochaska,et al. Hydrothermal Alteration and Fluid Chemistry of the Endako Porphyry Molybdenum Deposit, British Columbia , 2000 .
[27] P. Dulski,et al. Comparative study of yttrium and rare-earth element behaviours in fluorine-rich hydrothermal fluids , 1995 .
[28] P. Möller,et al. Rare earth element fractionation in metamorphogenic hydrothermal calcite, magnesite and siderite , 1992 .
[29] M. Bau. Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium , 1991 .
[30] S. Wood. The aqueous geochemistry of the rare-earth elements and yttrium: 2. Theoretical predictions of speciation in hydrothermal solutions to 350°C at saturation water vapor pressure , 1990 .
[31] B. M. Walker,et al. Unidirectional solidification textures and their significance in determining relative ages of intrusions at the Henderson Mine, Colorado , 1982 .
[32] H. Holland,et al. Fluorite deposition in hydrothermal systems , 1979 .
[33] S. Ishihara. The Magnetite-series and Ilmenite-series Granitic Rocks , 1977 .
[34] P. Parekh,et al. The application of Tb/Ca-Tb/La abundance ratios to problems of fluorspar genesis , 1976 .
[35] K. F. Clark. Stockwork Molybdenum Deposits in the Western Cordillera of North America , 1972 .