New initiatives to bolster analytical facilities in India for in situ U-Th-Pb Geochronology, Hf and O isotope systematics in zircon: a focus on laboratories at the IUAC, WIHG and CSIR-NGRI
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P. Mukherjee | S. Chopra | S. Singhal | B. Sreenivas | Pankaj Kumar | E V. S. S. K. Babu | T. Kumar | Y. Rao | Vikas Adlakha
[1] P. Mukherjee,et al. Terrane characterization in the Himalaya since Paleoproterozoic , 2020, Episodes.
[2] Pankaj Kumar,et al. Paleoenvironmental shifts spanning the last ~6000 years and recent anthropogenic controls inferred from a high-altitude temperate lake: Anchar Lake, NW Himalaya , 2020, The Holocene.
[3] P. Mukherjee,et al. U-Pb zircon ages and Sm-Nd isotopic characteristics of the Lesser and Great Himalayan sequences, Uttarakhand Himalaya, and their regional tectonic implications , 2019, Gondwana Research.
[4] S. Dey,et al. A new cache of Eoarchaean detrital zircons from the Singhbhum craton, eastern India and constraints on early Earth geodynamics , 2019, Geoscience Frontiers.
[5] P. Srivastava,et al. Late Pleistocene history of aggradation and incision, provenance and channel connectivity of the Zanskar River, NW Himalaya , 2019, Global and Planetary Change.
[6] P. Mukherjee,et al. Accuracy and precision of U–Pb zircon geochronology at high spatial resolution (7–20 μm spots) by laser ablation-ICP-single-collector-sector-field-mass spectrometry , 2019, Journal of Analytical Atomic Spectrometry.
[7] D. Kanjilal,et al. AMS and upcoming geochronology facility at Inter University Accelerator Centre (IUAC), New Delhi, India , 2019, Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms.
[8] Dhirendra Kumar,et al. Climate events between 47.5 and 1 ka BP in glaciated terrain of the Ny-Alesund region, Arctic, using geomorphology and sedimentology of diversified morphological zones , 2018, Polar Science.
[9] S. Singhal,et al. Age and geochemistry of the Paleoproterozoic Bhatwari Gneiss of Garhwal Lesser Himalaya, NW India: implications for the pre-Himalayan magmatic history of the Lesser Himalayan basement rocks , 2018, Special Publications.
[10] Meenakshi,et al. High resolution 14C AMS ages (∼50 ka) of organic matter associated with the loess-palaeosol Holocene-Late Pleistocene (8–130 ka) sediments of Dilpur Formation, Karewa Group, Kashmir, India , 2018, Quaternary Geochronology.
[11] S. Singhal,et al. U-Pb geochronology and geochemistry from the Kumaun Himalaya, NW India, reveal Paleoproterozoic arc magmatism related to formation of the Columbia supercontinent , 2018 .
[12] S. Singhal,et al. Migmatization and intrusion of “S‐type” granites in the trans‐Himalayan Ladakh Magmatic Arc of north India and their bearing on Indo‐Eurasian collisional tectonics , 2018 .
[13] J. Sanwal,et al. On the paleoseismic evidence of the 1803 earthquake rupture (or lack of it) along the frontal thrust of the Kumaun Himalaya , 2018 .
[14] B. Sreenivas,et al. Evidence for Neoarchean basement for the Deccan Volcanic flows around Koyna-Warna region, western India: Zircon U-Pb age and Hf-isotopic results , 2017, Journal of the Geological Society of India.
[15] S. S. Bhakuni,et al. Tectonic implications of U-Pb (zircon) Geochronology of Chor Granitoids of the Lesser Himalaya, Himachal Pradesh, NW Himalaya , 2017 .
[16] Peter A. Cawood,et al. Earth's Continental Lithosphere Through Time , 2017 .
[17] Takao Yamaguchi,et al. What Hf isotopes in zircon tell us about crust–mantle evolution , 2017 .
[18] S. Rai,et al. In situ U-Pb Zircon Micro-Geochronology of MCT Zone Rocks in the Lesser Himalaya Using LA–MC–ICPMS Technique , 2017 .
[19] V. M. Tiwari,et al. Investigations of continued reservoir triggered seismicity at Koyna, India , 2016, Special Publications.
[20] D. Kanjilal,et al. A new AMS facility at Inter University Accelerator Centre, New Delhi , 2015 .
[21] N. Roberts,et al. The zircon archive of continent formation through time , 2014 .
[22] Peter A. Cawood,et al. The continental record and the generation of continental crust , 2013 .
[23] Peter A. Cawood,et al. A Change in the Geodynamics of Continental Growth 3 Billion Years Ago , 2012, Science.
[24] D. Kanjilal,et al. 10Be measurements at IUAC-AMS facility , 2011 .
[25] Peter J. Voice,et al. Quantifying the Timing and Rate of Crustal Evolution: Global Compilation of Radiometrically Dated Detrital Zircon Grains , 2011, The Journal of Geology.
[26] W. Griffin,et al. The growth of the continental crust: Constraints from zircon Hf-isotope data , 2010 .
[27] Richard C. Aster,et al. Episodic zircon age spectra of orogenic granitoids: The supercontinent connection and continental growth , 2010 .
[28] T. Harrison,et al. Early (≥ 4.5 Ga) formation of terrestrial crust: Lu–Hf, δ18O, and Ti thermometry results for Hadean zircons , 2008 .
[29] P. Sylvester,et al. Present Trends and the Future of Zircon in Geochronology: Laser Ablation ICPMS , 2003 .
[30] J. Valley. Oxygen Isotopes in Zircon , 2003 .
[31] F. Corfu,et al. Atlas of Zircon Textures , 2003 .
[32] R. Parrish,et al. Zircon U-Th-Pb Geochronology by Isotope Dilution -- Thermal Ionization Mass Spectrometry (ID-TIMS) , 2003 .
[33] I. Williams,et al. Considerations in Zircon Geochronology by SIMS , 2003 .
[34] R. Maas,et al. Lu–Hf and Sm–Nd isotope systems in zircon , 2003 .
[35] Simon A. Wilde,et al. Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago , 2001, Nature.
[36] R. Parrish. An improved micro-capsule for zircon dissolution in UPb geochronology , 1987 .
[37] W. Compston,et al. U‐Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass‐resolution ion microprobe , 1984 .
[38] T. Krogh. Improved accuracy of U-Pb zircon dating by selection of more concordant fractions using a high gradient magnetic separation technique , 1982 .
[39] T. Krogh,et al. Improved accuracy of U-Pb zircon ages by the creation of more concordant systems using an air abrasion technique , 1982 .
[40] V. Guinn. Principles of Isotope Geology , 1978 .
[41] G. Wasserburg,et al. U-Th-Pb systematics in lunar highland samples from the Luna 20 and Apollo 16 missions , 1972 .
[42] G. Wetherill. Discordant uranium‐lead ages, I , 1956 .