Fluorite REE characteristics of the Diyanqinamu Mo deposit, Inner Mongolia, China

[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 .