Zircon SHRIMP U-Pb geochronology, geochemistry and petrogenesis of the upper Eocene Shuangmaidi peraluminous granite in Baoshan Block, Western Yunnan Terrain, southwestern China

[1]  Chengshan Wang,et al.  Modeling the East Asian Climate During the Late Cretaceous (80 Ma) , 2009 .

[2]  Zhilong Huang,et al.  U–Pb zircon, geochemical and Sr–Nd–Hf isotopic constraints on the age and origin of Early Palaeozoic I-type granite from the Tengchong–Baoshan Block, Western Yunnan Province, SW China , 2009 .

[3]  Yue-heng Yang,et al.  Petrogenesis of highly fractionated I-type granites in the Zayu area of eastern Gangdese, Tibet: Constraints from zircon U-Pb geochronology, geochemistry and Sr-Nd-Hf isotopes , 2009 .

[4]  Bo Zhang,et al.  Strain and kinematic vorticity analysis: An indicator for sinistral transpressional strain-partitioning along the Lancangjiang shear zone, western Yunnan, China , 2009 .

[5]  Dunyi Liu,et al.  40Ar/39Ar dating of the Jiali and Gaoligong shear zones: Implications for crustal deformation around the Eastern Himalayan Syntaxis , 2009 .

[6]  Zhou Su.  On the Lithosphere of Indo-Asia Collision Zone in Southern Tibet:Petrological and Geochemical Constraints , 2009 .

[7]  Zhang Bo,et al.  Geology and Metallogenetic Setting of the Habo Porphyry Cu(Mo-Au) Deposit,Yunnan , 2009 .

[8]  Chen Zhizhong,et al.  Zircon U-Pb Age and Geochemistry of Granitoids Within Jinla Pb-Zn-Ag Poly-metallic Ore Field Across China and Myanmar Border , 2009 .

[9]  B. Burchfiel,et al.  Geometry, kinematics, and regional significance of the Chong Shan shear zone, Eastern Himalayan Syntaxis, Yunnan, China , 2008 .

[10]  K. Wemmer,et al.  The Lancang River Zone of southwestern Yunnan, China: A questionable location for the active continental margin of Paleotethys , 2007 .

[11]  Dunyi Liu,et al.  Dating of prograde metamorphic events deciphered from episodic zircon growth in rocks of the Dabie–Sulu UHP complex, China , 2006 .

[12]  Yigang Xu,et al.  Kinematics and Ar-40/Ar-39 geochronology of the Gaoligong and Chongshan shear systems, western Yunnan, China: Implications for early Oligocene tectonic extrusion of SE Asia , 2006 .

[13]  A. Du,et al.  Himalayan Cu–Mo–Au mineralization in the eastern Indo–Asian collision zone: constraints from Re–Os dating of molybdenite , 2006 .

[14]  Z. Yong,et al.  Structural and Geochronological Evidence for Multiple Episodes of Tertiary Deformation along the Ailaoshan‐Red River Shear Zone, Southeastern Asia, Since the Paleocene , 2006 .

[15]  Dong-sheng Guo,et al.  Three types of collisional and post-collisional magmatism in the Lhasa block,Tibet and implications for India intra-continental subduction and mineralization:evidence from Sr-Nd isotopes. , 2006 .

[16]  Chen Fu.  Zircon age and Sr-Nd-Hf isotopic composition of migmatite in the eastern Tengchong block,western Yunnan. , 2006 .

[17]  T. Rushmer,et al.  Evolution and differentiation of the continental crust , 2006 .

[18]  W. Qu,et al.  Mineralization episode of porphyry copper deposits in the Jinshajiang-Red River mineralization belt: Re-Os dating , 2005 .

[19]  Mo Xuan-xue.  Spatial and Temporal Distribution and Characteristics of Granitoids in the Gangdese,Tibet and Implication for Crustal Growth and Evolution , 2005 .

[20]  Li Jun-lai.  Structure and Evolution of the Post-Collisional Fault Structures in the Three River Orogenic Belt, Exemplified by the Cenozoic Jianchuan-Lanping Basin , 2004 .

[21]  C. Miller,et al.  Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance , 2003 .

[22]  T. Harrison,et al.  Direct dating of left‐lateral deformation along the Red River shear zone, China and Vietnam , 2003 .

[23]  D. Günther,et al.  Determination of Forty Two Major and Trace Elements in USGS and NIST SRM Glasses by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry , 2002 .

[24]  Shan Gao,et al.  Geochemical and Sr–Nd–Pb isotopic compositions of Cretaceous granitoids: constraints on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt, China , 2002 .

[25]  Jin Zhen-min.  Studies on Rb-Sr and Sm-Nd Isotope of Yadong Leucogranite in Tibet: Constraint on Its Age and Source Material , 2001 .

[26]  P. Jian,et al.  The Jinshajiang–Ailaoshan Suture Zone, China: tectonostratigraphy, age and evolution , 2000 .

[27]  E. Hegner,et al.  High-potassium, calc-alkaline I-type plutonism in the European Variscides: northern Vosges (France) and northern Schwarzwald (Germany) , 2000 .

[28]  B. Barbarin.  A review of the relationships between granitoid types, their origins and their geodynamic environments , 1999 .

[29]  P. Sylvester.  Post-collisional strongly peraluminous granites , 1998 .

[30]  N. Harris,et al.  Experimental Constraints on Himalayan Anatexis , 1998 .

[31]  K. Hodges,et al.  Shisha Pangma Leucogranite, South Tibetan Himalaya: Field Relations, Geochemistry, Age, Origin, and Emplacement , 1997, The Journal of Geology.

[32]  B. Burchfiel,et al.  Interpretation of Cenozoic Tectonics in the Right-Lateral Accommodation Zone Between the Ailao Shan Shear Zone and the Eastern Himalayan Syntaxis , 1997 .

[33]  B. Barbarin.  Genesis of the two main types of peraluminous granitoids , 1996 .

[34]  U. Schärer,et al.  The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina , 1995 .

[35]  R. Rudnick,et al.  Nature and composition of the continental crust: A lower crustal perspective , 1995 .

[36]  Stéphane Guillot,et al.  Geochemical constraints on the bimodal origin of High Himalayan leucogranites , 1995 .

[37]  P. Tapponnier,et al.  An Early Miocene Transition in deformation regime within the Red River Fault Zone, Yunnan, And its significance for Indo‐Asian tectonics , 1992 .

[38]  B. Chappell,et al.  I- and S-type granites in the Lachlan Fold Belt , 1992, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[39]  B. Scaillet,et al.  Badrinath-Gangotri plutons (Garhwal, India): petrological and geochemical evidence for fractionation processes in a high Himalayan leucogranite , 1990 .

[40]  P. Soler,et al.  Sr‐Nd isotope compositions of cenozoic granitoids along a traverse of the central Peruvian Andes , 1990 .

[41]  B. Barbarin.  Granitoids: Main petrogenetic classifications in relation to origin and tectonic setting , 1990 .

[42]  P. Piccoli,et al.  Tectonic discrimination of granitoids , 1989 .

[43]  W. McDonough,et al.  Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.

[44]  R. W. Le Maitre,et al.  A Classification of igneous rocks and glossary of terms : recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks , 1989 .

[45]  C. France‐Lanord,et al.  Crustal melting and granite genesis during the Himalayan collision orogenesis , 1988, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[46]  A. Tindle,et al.  Geochemical characteristics of collision-zone magmatism , 1986, Geological Society, London, Special Publications.

[47]  A. Tindle,et al.  Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks , 1984 .

[48]  W. Boynton.  Geochemistry of the rare earth elements : meteorite studies , 1984 .

[49]  W. Boynton.  Cosmochemistry of the rare earth elements: meteorite studies. , 1984 .

[50]  B. Doe,et al.  Plumbotectonics-the model , 1981 .

[51]  G. Morrison.  Characteristics and tectonic setting of the shoshonite rock association , 1980 .

[52]  B. Chappell,et al.  Ultrametamorphism and granitoid genesis , 1977 .

[53]  Konrad B. Krauskopf,et al.  Introduction to geochemistry , 1967 .