ReeOs geochronology of Cu and WeMo deposits in the Balkhash metallogenic belt, Kazakhstan and its geological significance

Key Laboratory of Neotectonic Movement & Geohazard, Ministry of Land and Resources, Beijing 100081, PR China b Institute of Geomechanics, Chinese Academy of Geological Sciences, 11 Minzudaxue Nan Road, Beijing 100081, PR China National Research Center for Geoanalysis, Beijing 100037, PR China d Laboratory of Geological Formations, K. Satpaev Institute of Geological Sciences, Almaty 050010, Kazakhstan

[1]  H. T. Tran,et al.  Geological evolution and metallogeny of Vietnam , 2010 .

[2]  Dunyi Liu,et al.  Paleozoic multiple subduction-accretion processes of the southern Altaids , 2009, American Journal of Science.

[3]  Chen Xuanhua,et al.  STUDY ON REGIONAL MINERALIZATIONS AND ORE-FIELD STRUCTURES: BUILDING OF MINERALIZING TECTONIC SYSTEMS , 2009 .

[4]  S. Ping.  Host-rocks and alteration characters of the Baogutu porphyry copper-molybdenum deposit in Xinjiang, NW China. , 2009 .

[5]  Zuoheng Zhang,et al.  Re–Os dating of two Cu–Ni sulfide deposits in northern Xinjiang, NW China and its geological significance , 2008 .

[6]  Min Sun,et al.  Middle Cambrian to Permian subduction-related accretionary orogenesis of Northern Xinjiang, NW China: Implications for the tectonic evolution of central Asia , 2008 .

[7]  Guangming Li,et al.  Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia , 2008 .

[8]  Tian Pei-ren.  Knowledge of porphyry Cu (Mo) ore belts in the Central Asian metallogenic domain and their establishment , 2007 .

[9]  Liu Yu,et al.  Geological characters of Baogutu porphyry copper deposit in Xinjiang,NW China. , 2007 .

[10]  D. An.  Subgrain-size decoupling of Re and ~(187)Os within molybdenite , 2007 .

[11]  Nie Fengjun.  Re-Os Isotopic Dating on Molybdenite Separates from the Xiaodonggou Porphyry Mo Deposit,Hexigten Qi,Inner Mongolia , 2007 .

[12]  F. Cong,et al.  Genetic connection of Sareshike tin deposit with the alkaline A-type granites of Sabei body in Xinjiang:constraint from isotopic ages. , 2007 .

[13]  An Fang.  Geological evolution and metallogeny in the core part of the Central Asian metallogenic domain , 2007 .

[14]  Zhu Yong-feng.  Comparative study of the geology and mineral resources in Xinjiang,China,and its adjacent regions , 2006 .

[15]  JI Hou-gui.  Zircon SHRIMP U-Pb dating of plagiogranite porphyry in the Chihu molybdenum-copper district, Hami, East Tianshan , 2006 .

[16]  Han Bao,et al.  Late Paleozoic vertical growth of continental crust around the Junggar Basin,Xinjiang,China(PartI):Timing of post-collisionai plutonism , 2006 .

[17]  Hailei Tang,et al.  ISOTOPE DATING OF THE BE′ERKUDUKE TIN DEPOSIT IN THE EASTERN JUNGGAR AREA , 2006 .

[18]  M. Wieser.  Atomic weights of the elements 2005 (IUPAC Technical Report) , 2006 .

[19]  P. De Bièvre,et al.  Isotopic Compositions of the Elements, 2001 , 2005 .

[20]  Du An-dao.  Re-Os isotopic age dating of molybdenite separates from Elegen porphyry Mo (Cu) mineralized area, northwestern Alxa, western Inner Mongolia , 2005 .

[21]  Chen Fuwen.  Zircon SHRIMP U-Pb Dating and Its Geological Significance of Mineralization in Tuwu—Yandong Porphyry Copper Mine,East Tianshan Mountain , 2005 .

[22]  A. Du,et al.  Preparation and Certification of Re‐Os Dating Reference Materials: Molybdenites HLP and JDC , 2004 .

[23]  H. Stein,et al.  Subgrain-scale decoupling of Re and 187Os and assessment of laser ablation ICP-MS spot dating in molybdenite , 2003 .

[24]  Yuanchao Shen,et al.  Characteristics and genesis of Kanggur gold deposit in the eastern Tianshan mountains, NW China: evidence from geology, isotope distribution and chronology , 2003 .

[25]  A. Du,et al.  Re–Os ages for the Shameika porphyry Mo deposit and the Lipovy Log rare metal pegmatite, central Urals, Russia , 2003 .

[26]  K. Ludwig.  User's Manual for Isoplot 3.00 - A Geochronological Toolkit for Microsoft Excel , 2003 .

[27]  J. Morgan,et al.  The remarkable Re–Os chronometer in molybdenite: how and why it works , 2001 .

[28]  C. Heubeck.  Assembly of central Asia during the middle and late Paleozoic , 2001 .

[29]  D. An.  Precise Re-Os Dating for Molybdenite by ID-NTIMS with Carius Tube Sample Preparation , 2001 .

[30]  R. Creaser,et al.  Re-Os Geochronology and Systematics in Molybdenite from the Endako Porphyry Molybdenum Deposit, British Columbia, Canada , 2001 .

[31]  B. Lehmann,et al.  Paleozoic crustal growth and metallogeny of Central Asia: evidence from magmatic-hydrothermal ore systems of Central Kazakhstan , 2000 .

[32]  J. Morgan,et al.  Highly precise Re-Os dating for molybdenite using alkaline fusion and NTIMS. , 1998, Talanta.

[33]  A. J. Naldrett,et al.  Re–Os isotopic systematics of the Voisey's Bay Ni–Cu–Co magmatic ore system, Labrador, Canada , 1999 .

[34]  N. Mozgova,et al.  BISMUTH MINERALIZATION OF THE AKCHATAU MOLYBDENUM-TUNGSTEN DEPOSIT, CENTRAL KAZAKHSTAN , 1990 .

[35]  A. A. Burmistrov,et al.  STRUCTURAL AND MINERALOGICAL TYPES OF MOLYBDENUM-TUNGSTEN DEPOSITS OF CENTRAL KAZAKHSTAN , 1990 .

[36]  J. Morgan,et al.  Rhenium and non‐radiogenic osmium in Australian molybdenites and other sulphide minerals by neutron activation analysis , 1968 .