Zircon U–Pb dating and the petrological and geochemical constraints on Lincang granite in Western Yunnan, China: Implications for the closure of the Paleo-Tethys Ocean
暂无分享,去创建一个
G. Dong | Zhidan Zhao | Di‐Cheng Zhu | X. Mo | R. C. Goodman | Shuo Wang | Huilei Kong
[1] K. Hui. Petrogenesis of Lincang granites in Sanjiang area of western Yunnan Province:Constraints from geochemistry,zircon U-Pb geochronology and Hf isotope , 2012 .
[2] Dong-sheng Guo. Petrological and geochemical characteristics,Ar-Ar geochronology study and their tectonic significance of Triassic volcanic rocks in southern Lancangjiang zone , 2012 .
[3] F. Bea,et al. Zircon dating, Sr and Nd isotopes, and element geochemistry of the Khalifan pluton, NW Iran: Evidence for Variscan magmatism in a supposedly Cimmerian superterrane , 2011 .
[4] W. Fan,et al. Permian arc–back-arc basin development along the Ailaoshan tectonic zone: Geochemical, isotopic and geochronological evidence from the Mojiang volcanic rocks, Southwest China , 2010 .
[5] K. Schmidt,et al. Early Permian seafloor to continental arc magmatism in the eastern Paleo-Tethys: U–Pb age and Nd–Sr isotope data from the southern Lancangjiang zone, Yunnan, China , 2009 .
[6] Kai‐Jun Zhang,et al. A new model for the Indochina and South China collision during the Late Permian to the Middle Triassic , 2009 .
[7] Shan Gao,et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard , 2008 .
[8] I. Metcalfe,et al. Parallel Tethyan sutures in mainland Southeast Asia: New insights for Palaeo-Tethys closure and implications for the Indosinian orogeny , 2008 .
[9] Liu Ji. Geological characteristics and tectonic setting of Yunxian granite in the northern part of South Lancangjiang convergent margin, Western Yunnan Province , 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] Yue-heng Yang,et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U–Pb geochronology , 2006 .
[12] Fan Weiming,et al. SHRIMP ziron U-Pb geochronology of early Mesozoic felsic igneous rocks from the southern Lancangjiang and its tectonic implications , 2006 .
[13] Hai-Ling Liu,et al. Cenozoic Cooling History of Lincang Granitoid Batholith in Western Yunnan: Evidence from Fission Track Data , 2006 .
[14] B. Barbarin. Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts , 2005 .
[15] C. Isachsen,et al. The decay constant of 176Lu determined from Lu-Hf and U-Pb isotope systematics of terrestrial Precambrian high-temperature mafic intrusions , 2003 .
[16] U. Schaltegger,et al. The Composition of Zircon and Igneous and Metamorphic Petrogenesis , 2003 .
[17] Zhang Hui-hua. A STUDY ON THE GRANODIORITE IN THE MIDDLE PART OF LINCANG GRANITE BATHOLITH , 2003 .
[18] C. German,et al. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections , 2002 .
[19] W. Griffin,et al. Zircon chemistry and magma mixing, SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes , 2002 .
[20] Y. Ezaki,et al. Late Paleozoic-Early Mesozoic Tectonics in South China Around Yangtze Massif: Closing Process of the Paleo-Tethys , 2001 .
[21] T. Fu. DEVONIAN-TRIASSIC BASIN-RANGE TRANSFORMATION AND THE TECTONIC EVOLUTION OF PALEO-TETHYS IN WESTERN YUNNAN, CHINA , 2001 .
[22] G. Dunning,et al. Petrochemistry, U–Pb (zircon) age, and palaeotectonic setting of the Lampang volcanic belt, northern Thailand , 2000, Journal of the Geological Society.
[23] W. Griffin,et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites , 2000 .
[24] B. Barbarin. A review of the relationships between granitoid types, their origins and their geodynamic environments , 1999 .
[25] 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 .
[26] U. Schärer,et al. The Ailao Shan-Red River shear zone (Yunnan, China), Tertiary transform boundary of Indochina , 1995 .
[27] Kaihui Yang,et al. Tectono-volcanic belts and late Paleozoic-early Mesozoic evolution of southwestern Yunnan, China , 1994 .
[28] Mo Xuanxue,et al. Volcanism and the evolution of Tethys in Sanjiang area, southwestern China , 1994 .
[29] M. Roberts,et al. Origin of high-potassium, talc-alkaline, I-type granitoids , 1993 .
[30] Philip England,et al. Crustal thickening versus lateral expulsion in the Indian‐Asian continental collision , 1993 .
[31] S. Maruyama,et al. Metamorphism and tectonic evolution of the Lancang paired metamorphic belts, south‐western China , 1993 .
[32] P. Bievre,et al. Table of the isotopic compositions of the elements , 1993 .
[33] 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.
[34] L. Changshi,et al. The Hercynian-Indonesian collision type granites of west Yunnan and their tectonic significance , 1989 .
[35] A. Tindle,et al. Geochemical characteristics of collision-zone magmatism , 1986, Geological Society, London, Special Publications.
[36] D. Helmcke. The Permo-Triassic »Paleotethys« in mainland Southeast-Asia and adjacent parts of China , 1985 .
[37] A. Tindle,et al. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks , 1984 .