Contrasting geochemical signatures of Devonian and Permian granitoids from the Tseel Terrane, SW Mongolia
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N. Tsuchiya | A. Okamoto | K. Horie | M. Uno | T. Hokada | U. Burenjargal
[1] W. Griffin,et al. Are continental “adakites” derived from thickened or foundered lower crust? , 2015 .
[2] P. Hanžl,et al. P–T–t–D record of crustal‐scale horizontal flow and magma‐assisted doming in the SW Mongolian Altai , 2015 .
[3] T. Kuwatani,et al. Thermal evolution of the Tseel terrane, SW Mongolia and its relation to granitoid intrusions in the Central Asian Orogenic Belt , 2014 .
[4] N. Tsuchiya,et al. An exhumation pressure–temperature path and fluid activities during metamorphism in the Tseel terrane, SW Mongolia: Constraints from aluminosilicate-bearing quartz veins and garnet zonings in metapelites , 2012 .
[5] C. Yuan,et al. The high-grade Tseel Terrane in SW Mongolia: An Early Paleozoic arc system or a Precambrian sliver? , 2012 .
[6] G. Ortolano,et al. Metamorphic evolution of preserved Hercynian crustal section in the Serre Massif (Calabria–Peloritani Orogen, southern Italy) , 2010 .
[7] J. Moyen. High Sr/Y and La/Yb ratios: The meaning of the “adakitic signature” , 2009 .
[8] E. Hegner,et al. Devonian arc-related magmatism in the Tseel terrane of SW Mongolia: chronological and geochemical evidence , 2009, Journal of the Geological Society.
[9] D. Cunningham,et al. Structure and petrology of the Altan Uul Ophiolite: new evidence for a Late Carboniferous suture in the Gobi Altai, southern Mongolia , 2008, Journal of the Geological Society.
[10] Lin Qiu,et al. Transition of metamorphic series from the Kyanite- to andalusite-types in the Altai orogen, Xinjiang, China: Evidence from petrography and calculated KMnFMASH and KFMASH phase relations , 2007 .
[11] Brian F. Windley,et al. Tectonic models for accretion of the Central Asian Orogenic Belt , 2007, Journal of the Geological Society.
[12] R. Stern,et al. Geochemical mapping of the Mariana arc‐basin system: Implications for the nature and distribution of subduction components , 2005 .
[13] R. Korsch,et al. of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards , 2004 .
[14] B. Windley,et al. A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia , 2002 .
[15] E. Khain,et al. The most ancient ophiolite of the Central Asian fold belt: U–Pb and Pb–Pb zircon ages for the Dunzhugur Complex, Eastern Sayan, Siberia, and geodynamic implications , 2002 .
[16] A. Şengör,et al. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia , 1993, Nature.
[17] R. Stewart,et al. Dacite Genesis via both Slab Melting and Differentiation: Petrogenesis of La Yeguada Volcanic Complex, Panama , 1991 .
[18] G. Eby. The A-type granitoids: A review of their occurrence and chemical characteristics and speculations on their petrogenesis , 1990 .
[19] J. Whalen,et al. A-type granites: geochemical characteristics, discrimination and petrogenesis , 1987 .
[20] A. Tindle,et al. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks , 1984 .
[21] W. Compston,et al. U‐Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass‐resolution ion microprobe , 1984 .
[22] A. Irving,et al. Distribution of trace elements between garnet megacrysts and host volcanic liquids of kimberlitic to rhyolitic composition , 1978 .
[23] J. Kramers,et al. Approximation of terrestrial lead isotope evolution by a two-stage model , 1975 .
[24] T. Irvine,et al. A Guide to the Chemical Classification of the Common Volcanic Rocks , 1971 .
[25] F. Gauthier-Lafaye,et al. Elemental distribution in zircon: Alteration and radiation-damage effects , 2006 .
[26] Y. Amelin,et al. Distribution of U, Th, Pb and Nd Between Minerals in Chondrules and CAIs , 2003 .
[27] K. Ludwig. User's Manual for Isoplot 3.00 - A Geochronological Toolkit for Microsoft Excel , 2003 .
[28] P. Azimov,et al. Hercynian granulites of Mongolian and Gobian Altai: Geodynamic setting and formation conditions , 2002 .
[29] 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.
[30] W. Compston,et al. Two Carboniferous Ages: A Comparison of Shrimp Zircon Dating with Conventional Zircon Ages and 40Ar/39Ar Analysis , 1995 .
[31] W. McDonough,et al. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.
[32] W. Boynton. Geochemistry of the rare earth elements : meteorite studies , 1984 .
[33] B. Chappell,et al. Two contrasting granite types , 1974 .