Sources of Phanerozoic granitoids in the transect Bayanhongor–Ulaan Baatar, Mongolia: geochemical and Nd isotopic evidence, and implications for Phanerozoic crustal growth

[1]  Bin Chen,et al.  Genesis of post-collisional granitoids and basement nature of the Junggar Terrane, NW China: Nd–Sr isotope and trace element evidence , 2004 .

[2]  A. M. Larin,et al.  Isotope provinces, mechanisms of generation and sources of the continental crust in the Central Asian mobile belt: geological and isotopic evidence , 2004 .

[3]  S. Wilde,et al.  Highly fractionated I-type granites in NE China (II): isotopic geochemistry and implications for crustal growth in the Phanerozoic , 2003 .

[4]  D. Cunningham,et al.  Timing of accretion and collisional deformation in the Central Asian Orogenic Belt: Implications of granite geochronology in the Bayankhongor Ophiolite Zone , 2002 .

[5]  B. Windley,et al.  A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia , 2002 .

[6]  A. Saunders,et al.  Petrogenesis of syenite-granite suites from the Bryansky Complex (Transbaikalia, Russia): Implications for the origin of A-type granitoid magmas , 2002 .

[7]  S. Wilde,et al.  A-type granites in northeastern China: age and geochemical constraints on their petrogenesis , 2002 .

[8]  Yixian Wang,et al.  Highly evolved juvenile granites with tetrad REE patterns: the Woduhe and Baerzhe granites from the Great Xing'an Mountains in NE China , 2001 .

[9]  D. Cunningham,et al.  Structural and lithological characteristics of the Bayankhongor Ophiolite Zone, Central Mongolia , 2001, Journal of the Geological Society.

[10]  Scott M. McLennan,et al.  Relationships between the trace element composition of sedimentary rocks and upper continental crust , 2001 .

[11]  Bin Chen,et al.  Two contrasting paleozoic magmatic belts in northern Inner Mongolia, China: petrogenesis and tectonic implications , 2000 .

[12]  S. Wilde,et al.  Phanerozoic crustal growth: U–Pb and Sr–Nd isotopic evidence from the granites in northeastern China , 2000 .

[13]  Bin Chen,et al.  Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic , 2000 .

[14]  Y. Zorin.  Geodynamics of the western part of the Mongolia–Okhotsk collisional belt, Trans-Baikal region (Russia) and Mongolia , 1999 .

[15]  C. Lo,et al.  Crust–mantle interaction induced by deep subduction of the continental crust: geochemical and Sr–Nd isotopic evidence from post-collisional mafic–ultramafic intrusions of the northern Dabie complex, central China , 1999 .

[16]  W. Irber.  Quantification of the lanthanide tetrad effect and its correlation with K/Rb, Eu/Eu*, Sr/Eu, Y/Ho, and Zr/Hf of evolving peraluminous granite suites , 1999 .

[17]  V. Yarmolyuk,et al.  Sources of Phanerozoic granites in Central Asia; Sm-Nd isotope data , 1996 .

[18]  I. Bindeman,et al.  A Stable Isotope Study of Anorogenic Magmatism in East Central Asia , 1996 .

[19]  B. Natal’in,et al.  TURKIC-TYPE OROGENY AND ITS ROLE IN THE MAKING OF THE CONTINENTAL CRUST , 1996 .

[20]  M. Bau.  Controls on the fractionation of isovalent trace elements in magmatic and aqueous systems: evidence from Y/Ho, Zr/Hf, and lanthanide tetrad effect , 1996 .

[21]  T. Yui,et al.  Ultrahigh-ϵNd eclogites from an ultrahigh-pressure metamorphic terrane of China , 1996 .

[22]  I. Bindeman,et al.  Geochemical evolution of Phanerozoic magmatism in Transbaikalia, East Asia: A key constraint on the origin of K‐rich silicic magmas and the process of cratonization , 1995 .

[23]  S. Taylor,et al.  The geochemical evolution of the continental crust , 1995 .

[24]  F. Bea,et al.  Genesis of Alkaline and Peralkaline Syenite-Granite Series: The Kharitonovo Pluton (Transbaikalia, Russia) , 1995, The Journal of Geology.

[25]  Huang Huaizeng,et al.  The Permian alkaline granites in Central Inner Mongolia and their geodynamic significance , 1994 .

[26]  A. Şengör,et al.  Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia , 1993, Nature.

[27]  K. Condie.  Chemical composition and evolution of the upper continental crust: Contrasting results from surface samples and shales , 1993 .

[28]  P. Kepezhinskas,et al.  Lower Paleozoic oceanic crust in Mongolian Caledonides: SM‐ND isotope and trace element data , 1991 .

[29]  M. Štemprok.  Ongonite from Ongon Khairkhan, Mongolia , 1991 .

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

[31]  S. Jacobsen,et al.  Nd and Sr isotopic variations of Early Paleozoic oceans , 1987 .

[32]  A. Masuda,et al.  Fine structures of mutually normalized rare-earth patterns of chondrites , 1973 .

[33]  B. Jahn.  The Central Asian Orogenic Belt and growth of the continental crust in the Phanerozoic , 2004, Geological Society, London, Special Publications.

[34]  W. Todt,et al.  Timing of the structural evolution of metamorphic rocks in the Tuva-Mongolian Massif , 2001 .

[35]  Bin Chen,et al.  Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic , 2000, Earth and Environmental Science Transactions of the Royal Society of Edinburgh.

[36]  W. Ridley,et al.  Applications of Microanalytical Techniques to Understanding Mineralizing Processes , 1998 .

[37]  S. N. Rudnev,et al.  Late paleozoic - Early mesozoic granitoid magmatism in Altai , 1997 .

[38]  Han Bao-fu,et al.  Post-orogenic alkaline granites from China and comparisons with anorogenic alkaline granites elsewhere , 1996 .

[39]  L. Zonenshain,et al.  Geology of the USSR : a plate-tectonic synthesis , 1990 .

[40]  A. Masuda,et al.  Lanthanide tetrad effect observed in leucogranites from China , 1989 .

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

[42]  S. Taylor,et al.  The continental crust: Its composition and evolution , 1985 .