Deconvolving episodic age spectra from zircons of the Ladakh Batholith, northwest Indian Himalaya

[1]  M. Searle,et al.  Zircon age determinations for the Ladakh batholith at Chumathang (Northwest India): Implications for the age of the India–Asia collision in the Ladakh Himalaya , 2010 .

[2]  U. Andersson,et al.  Hybridization of granitic magmas in the source: The origin of the Karakoram Batholith, Ladakh, NW India , 2010 .

[3]  T. Ahmad,et al.  Mineral chemistry and K–Ar ages of plutons across the Karakoram fault in the Shyok-Nubra confluence of northern Ladakh Himalaya, India , 2010 .

[4]  Fu-Yuan Wu,et al.  Zircon U–Pb and Hf isotopic constraints on petrogenesis of the Cretaceous–Tertiary granites in eastern Karakoram and Ladakh, India , 2009 .

[5]  W. Frisch,et al.  Tectonic implications of new U–Pb zircon ages of the Ladakh batholith, Indus suture zone, northwest Himalaya, India , 2008 .

[6]  R. Phillips.  Geological map of the Karakoram fault zone, Eastern Karakoram, Ladakh, NW Himalaya , 2008 .

[7]  A. Jain,et al.  SHRIMP U–Pb ages and depth of emplacement of Ladakh Batholith, Eastern Ladakh, India , 2007 .

[8]  A. Zanchi,et al.  Age and isotopic constraints on magmatism along the Karakoram-Kohistan Suture Zone, NW Pakistan: evidence for subduction and continued convergence after India-Asia collision , 2007 .

[9]  T. R. Venkatesan,et al.  Tectono-thermal evolution of the India-Asia collision zone based on40Ar-39Ar thermochronology in Ladakh, India , 2004 .

[10]  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 .

[11]  K. Ludwig.  User's Manual for Isoplot 3.00 - A Geochronological Toolkit for Microsoft Excel , 2003 .

[12]  K. Pande,et al.  Age of the Karakoram fault activation: 40Ar-39Ar geochronological study of Shyok suture zone in northern Ladakh, India , 2003 .

[13]  G. Zeilinger,et al.  Multiple mantle sources during island arc magmatism: U–Pb and Hf isotopic evidence from the Kohistan arc complex, Pakistan , 2002 .

[14]  H. Lapierre,et al.  The cretaceous Ladakh arc of NW himalaya—slab melting and melt–mantle interaction during fast northward drift of Indian Plate , 2002 .

[15]  B. Chappell,et al.  Two contrasting granite types: 25 years later , 2001 .

[16]  A. Pêcher,et al.  Middle Cretaceous back-arc formation and arc evolution along the Asian margin: the Shyok Suture Zone in northern Ladakh (NW Himalaya) , 2000 .

[17]  T. Harrison,et al.  The Zedong Window: A record of superposed Tertiary convergence in southeastern Tibet , 2000 .

[18]  An Yin,et al.  Geologic Evolution of the Himalayan-Tibetan Orogen , 2000 .

[19]  R. Weinberg,et al.  Growth and Deformation of the Ladakh Batholith, Northwest Himalayas: Implications for Timing of Continental Collision and Origin of Calc‐Alkaline Batholiths , 2000, The Journal of Geology.

[20]  M. Whitehouse,et al.  New field, structural and geochronological data from the Shyok and Nubra valleys, northern Ladakh: linking Kohistan to Tibet , 2000, Geological Society, London, Special Publications.

[21]  V. Thakur,et al.  Geochemistry and geodynamic implications of magmatic rocks from the Trans-Himalayan arc , 1998 .

[22]  M. Searle,et al.  Transpressional tectonics along the Karakoram fault zone, northern Ladakh: constraints on Tibetan extrusion , 1998, Geological Society, London, Special Publications.

[23]  P. Zeitler,et al.  Episodic unroofing of the Kohistan Batholith, Pakistan: Implications from K‐feldspar thermochronology , 1996 .

[24]  D. Rowley.  Age of initiation of collision between India and Asia: A review of stratigraphic data , 1996 .

[25]  S. Weaver,et al.  Ion microprobe dating of Paleozoic granitoids: Devonian magmatism in New Zealand and correlations with Australia and Antarctica , 1996 .

[26]  T. Harrison,et al.  Thermal evolution of the Gangdese batholith, southern Tibet: A history of episodic unroofing , 1995 .

[27]  Malcolm Sambridge,et al.  Mixture modeling of multi-component data sets with application to ion-probe zircon ages , 1994 .

[28]  A. Jain,et al.  New age constraints on the cooling and unroofing history of the Trans-Himalayan Ladakh Batholith (Kargil area), N. W. India , 1994 .

[29]  R. Butler,et al.  The tectonic implications of contrasting granite magmatism between the Kohistan island arc and the Nanga Parbat-Haramosh Massif, Pakistan Himalaya , 1993, Geological Society, London, Special Publications.

[30]  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.

[31]  M. Gaetani,et al.  Multicyclic History of the Northern India Continental Margin (Northwestern Himalaya) (1) , 1991 .

[32]  B. Windley,et al.  K‐Ar and Ar‐Ar geochronology of the Himalayan collision in NW Pakistan: Constraints on the timing of suturing, deformation, metamorphism and uplift , 1989 .

[33]  Jin Chengwei,et al.  Plutonic rocks of the 1985 Tibet Geotraverse, Lhasa to Golmud , 1988, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[34]  D. Cooper,et al.  Collision tectonics of the Ladakh-Zanskar Himalaya , 1988, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[35]  D. Cooper,et al.  The closing of Tethys and the tectonics of the Himalaya , 1987 .

[36]  A. Baud,et al.  Sedimentary record of the northward flight of India and its collision with Eurasia (Ladakh Himalaya, India) , 1987 .

[37]  P. Fort,et al.  Granites of western Karakorum and northern Kohistan (Pakistan): A composite mid-cretaceous to upper cenozoic magmatism , 1987 .

[38]  S. Sheppard,et al.  The Four Plutonic Belts of the Transhimalaya-Himalaya: a Chemical, Mineralogical, Isotopic, and Chronological Synthesis along a Tibet-Nepal Section , 1986 .

[39]  B. Windley,et al.  RbSr dating of the Kohistan arc-batholith in the Trans-Himalaya of north Pakistan, and tectonic implications , 1985 .

[40]  U. Schärer,et al.  The Transhimalaya (Gangdese) plutonism in the Ladakh region: a UPb and RbSr study , 1984 .

[41]  D. K. Misra,et al.  Tectonic framework of the Indus and Shyok suture zones in Eastern Ladakh, Northwest Himalaya , 1984 .

[42]  V. Trommsdorff,et al.  Magmatism and metamorphism in the Ladakh Himalayas (the Indus-Tsangpo suture zone) , 1982 .

[43]  J. R. Trivedi,et al.  Rb−Sr age of Gaik granite, Ladakh batholith, northwest Himalaya , 1982 .

[44]  M. Brookfield,et al.  Late Cretaceous emplacement of the Indus suture zone ophiolitic mélanges and an Eocene-Oligocene magmatic arc on the northern edge of the Indian plate , 1981 .

[45]  P. K. Mehta.  Tectonic significance of the young mineral dates and the rates of cooling and uplift in the Himalaya , 1980 .

[46]  A. Gansser.  Geology of the Himalayas , 1964 .