Neoproterozoic magmatism in eastern Himalayan terrane.

[1]  Paul D. Asimow,et al.  Contrasting geochemical signatures of fluid-absent versus fluid-fluxed melting of muscovite in metasedimentary sources: The Himalayan leucogranites , 2017 .

[2]  Wu Fu,et al.  Himalayan leucogranite: Petrogenesis and implications to orogenesis and plateau uplift , 2015 .

[3]  K. Hou,et al.  Eocene magmatism in the Tethyan Himalaya, southern Tibet , 2014 .

[4]  L. Zeng,et al.  Fluxed melting of metapelite and the formation of Miocene high-CaO two-mica granites in the Malashan gneiss dome, southern Tibet , 2014 .

[5]  Bo Zhang,et al.  Rapid denudation of the Himalayan orogen in the Nyalam area, southern Tibet, since the Pliocene and implications for tectonics–climate coupling , 2014 .

[6]  K. Hou,et al.  Episodic crustal anatexis and the formation of Paiku composite leucogranitic pluton in the Malashan Gneiss Dome, Southern Tibet , 2013 .

[7]  A. Pêcher,et al.  Orogen‐parallel ductile extension and extrusion of the Greater Himalaya in the late Oligocene and Miocene , 2013 .

[8]  Shuhab D. Khan,et al.  Isotopic ages for alkaline igneous rocks, including a 26 Ma ignimbrite, from the Peshawar plain of northern Pakistan and their tectonic implications , 2013 .

[9]  Dunyi Liu,et al.  Episodic Paleoproterozoic (~2.45, ~1.95 and ~1.85 Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry , 2013 .

[10]  Chuan-Lin Zhang,et al.  Multiple phases of the Neoproterozoic igneous activity in Quruqtagh of the northeastern Tarim Block, NW China: Interaction between plate subduction and mantle plume? , 2012 .

[11]  M. Santosh,et al.  Andean-type orogeny in the Himalayas of south Tibet: Implications for early Paleozoic tectonics along the Indian margin of Gondwana , 2012 .

[12]  Z. Hou,et al.  Eocene-Oligocene granitoids in southern Tibet: Constraints on crustal anatexis and tectonic evolution of the Himalayan orogen , 2012 .

[13]  T. Harrison,et al.  The origin of Eo- and Neo-himalayan granitoids, Eastern Tibet , 2012 .

[14]  T. Harrison,et al.  Age and thermal history of Eo- and Neohimalayan granitoids, eastern Himalaya , 2012 .

[15]  Bo Zhang,et al.  Tectonics of the northern Himalaya since the India–Asia collision , 2012 .

[16]  Gao Li.  Two types of garnets in the Cenozoic granites from the Himayalan Orogenic Belt:Geochemical characteristics and implications for crustal anatexis , 2012 .

[17]  C. Dong,et al.  High-pressure melting of metapelite and the formation of Ca-rich granitic melts in the Namche Barwa Massif, southern Tibet , 2012 .

[18]  Dunyi Liu,et al.  India's hidden inputs to Tibetan orogeny revealed by Hf isotopes of Transhimalayan zircons and host rocks , 2011 .

[19]  L. Zeng,et al.  Early Miocene leucogranites in Dinggye area, southern Tibet: Formation mechanism and tectonic implications , 2011 .

[20]  Sun-Lin Chung,et al.  Crustal–lithospheric structure and continental extrusion of Tibet , 2011, Journal of the Geological Society.

[21]  L. Zeng,et al.  Mid-Eocene high Sr/Y granites in the Northern Himalayan Gneiss Domes: Melting thickened lower continental crust , 2011 .

[22]  R. Parrish,et al.  Contribution of crustal anatexis to the tectonic evolution of Indian crust beneath southern Tibet , 2011 .

[23]  K. Pogue,et al.  Extraordinary transport and mixing of sediment across Himalayan central Gondwana during the Cambrian–Ordovician , 2010 .

[24]  T. Harrison,et al.  Geologic correlation of the Himalayan orogen and Indian craton: Part 2. Structural geology, geochronology, and tectonic evolution of the Eastern Himalaya , 2010 .

[25]  Shan Gao,et al.  Continental and Oceanic Crust Recycling-induced Melt^Peridotite Interactions in the Trans-North China Orogen: U^Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths , 2010 .

[26]  Yue-heng Yang,et al.  The 132 Ma Comei-Bunbury large igneous province: Remnants identified in present-day southeastern Tibet and southwestern Australia , 2009 .

[27]  M. Searle,et al.  Geochronology of granulitized eclogite from the Ama Drime Massif: Implications for the tectonic evolution of the South Tibetan Himalaya , 2009 .

[28]  J. Miller,et al.  Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICPMS , 2008 .

[29]  F. Corfu,et al.  Zircon M257 ‐ a Homogeneous Natural Reference Material for the Ion Microprobe U‐Pb Analysis of Zircon , 2008 .

[30]  M. Whitehouse,et al.  Plesovice zircon : A new natural reference material for U-Pb and Hf isotopic microanalysis , 2008 .

[31]  K. Karlstrom,et al.  Assembly, configuration, and break-up history of Rodinia: A synthesis , 2008 .

[32]  L. Zeng,et al.  Early Oligocene anatexis in the Yardoi gneiss dome, southern Tibet and geological implications , 2008 .

[33]  Xian‐Hua Li,et al.  Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust , 2007 .

[34]  Peter A. Cawood,et al.  Early Palaeozoic orogenesis along the Indian margin of Gondwana: Tectonic response to Gondwana assembly , 2007 .

[35]  Z. Tian,et al.  Laser ablation-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications. , 2007 .

[36]  B. N. Upreti,et al.  Geologic and U–Pb geochronologic evidence for early Paleozoic tectonism in the Dadeldhura thrust sheet, far-west Nepal Himalaya , 2006 .

[37]  R. Parrish,et al.  Correlation of lithotectonic units across the eastern Himalaya, Bhutan , 2006 .

[38]  Xiaolei Wang,et al.  LA-ICP-MS U-Pb zircon geochronology of the Neoproterozoic igneous rocks from Northern Guangxi, South China: Implications for tectonic evolution , 2006 .

[39]  B. N. Upreti,et al.  Geologic and U-Th-Pb geochronologic evidence for early Paleozoic tectonism in the Kathmandu thrust sheet, central Nepal Himalaya , 2006 .

[40]  Subhasis Ghosh,et al.  Geochemistry and Origin of Neoproterozoic Granitoids of Meghalaya, Northeast India: Implications for Linkage with Amalgamation of Gondwana Supercontinent , 2005 .

[41]  L. Ding,et al.  Paleocene–Eocene record of ophiolite obduction and initial India‐Asia collision, south central Tibet , 2005 .

[42]  Xu Zhi.  Pan-African and Early Paleozoic orogenic events in the Himalaya terrane: Inference from SHRIMP U-Pb zircon ages , 2005 .

[43]  N. Rogers,et al.  Causes and consequences of protracted melting of the mid-crust exposed in the North Himalayan antiform , 2004 .

[44]  William L. Griffin,et al.  The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology , 2004 .

[45]  B. N. Upreti,et al.  Five generations of monazite in Langtang gneisses: implications for chronology of the Himalayan metamorphic core , 2004 .

[46]  Zhenyu Yang,et al.  A long connection (750–380 Ma) between South China and Australia: paleomagnetic constraints , 2004 .

[47]  P. G. DeCellesa,et al.  Detrital geochronology and geochemistry of Cretaceous – Early Miocene strata of Nepal : implications for timing and diachroneity of initial Himalayan orogenesis , 2004 .

[48]  R. Korsch,et al.  TEMORA 1: a new zircon standard for Phanerozoic U–Pb geochronology , 2003 .

[49]  G. Gehrels,et al.  Initiation of the Himalayan orogen as an early Paleozoic thin-skinned thrust belt: GSA Today , 2003 .

[50]  S. Bowring,et al.  Integrated tectonostratigraphic analysis of the Himalaya and implications for its tectonic reconstruction , 2003 .

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

[52]  Xian‐Hua Li.  Neoproterozoic granitoids in South China: crustal melting above a mantle plume at ca. 825 Ma? , 2003 .

[53]  K. Ludwig.  Mathematical–Statistical Treatment of Data and Errors for 230Th/U Geochronology , 2003 .

[54]  A. Jain,et al.  SHRIMP U–Pb in zircon geochronology of the Chor granitoid: evidence for Neoproterozoic magmatism in the Lesser Himalayan granite belt of NW India , 2002 .

[55]  Mei-Fu Zhou,et al.  SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China. , 2002 .

[56]  S. Pisarevsky,et al.  Late Neoproterozoic assembly of East Gondwana , 2002 .

[57]  C. Isachsen,et al.  U‐Pb zircon ages from the Indian plate in northwest Pakistan and their significance to Himalayan and pre‐Himalayan geologic history , 2001 .

[58]  T. Torsvik.  Neoproterozoic geochronology and palaeogeography of the Seychelles microcontinent: the India link , 2001 .

[59]  T. Torsvik.  Rodinia refined or obscured: palaeomagnetism of the Malani igneous suite (NW India) , 2001 .

[60]  E. Draganits,et al.  The early Palaeozoic magmatic event in the Northwest Himalaya, India: source, tectonic setting and age of emplacement , 2001, Geological Magazine.

[61]  N. Harris,et al.  Fluid-enhanced melting during prograde metamorphism , 2001, Journal of the Geological Society.

[62]  G. Gehrels,et al.  Tectonic implications of U-Pb zircon ages of the himalayan orogenic belt in nepal , 2000, Science.

[63]  M. Searle,et al.  Crustal shortening estimates across the north Indian continental margin, Ladakh, NW India , 2000, Geological Society, London, Special Publications.

[64]  Xian‐Hua Li,et al.  The breakup of Rodinia: did it start with a mantle plume beneath South China? , 1999 .

[65]  T. Harrison,et al.  The origin of Himalayan anatexis and inverted metamorphism: Models and constraints , 1999 .

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

[67]  R. Voo,et al.  THE PROTEROZOIC SUPERCONTINENT RODINIA : PALEOMAGNETICALLY DERIVED RECONSTRUCTIONS FOR 1100 TO 800 MA , 1998 .

[68]  T. Harrison,et al.  New insights into the origin of two contrasting Himalayan granite belts , 1997 .

[69]  M. Brasier,et al.  Continental break-up and collision in the Neoproterozoic and Palaeozoic — A tale of Baltica and Laurentia , 1996 .

[70]  M. Brookfield.  The Himalayan passive margin from Precambrian to Cretaceous times , 1993 .

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

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

[73]  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 .

[74]  M. Searle.  Structural evolution and sequence of thrusting in the High Himalayan, Tibetan-Tethys and Indus Suture zones of Zanskar and Ladakh, Western Himalaya: Reply , 1988 .

[75]  M. Schidlowski,et al.  Chronostratigraphic markers in the end-Precambrian carbon isotope record of the Lesser Himalaya , 1987, Nature.

[76]  B. N. Upreti,et al.  Crustal generation of the Himalayan leucogranites , 1987 .

[77]  T. M. Harrison,et al.  Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types , 1983 .

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

[79]  M. Saxena.  The crystalline axis of the Himalaya: The Indian shield and continental drift , 1971 .