Auswahl der wissenschaftlichen Literatur zum Thema „Isotopie Sm-Nd“
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Zeitschriftenartikel zum Thema "Isotopie Sm-Nd"
Vezinet, Adrien, Emilie Thomassot, Yan Luo, Chiranjeeb Sarkar und D. Graham Pearson. „Diachronous Redistribution of Hf and Nd Isotopes at the Crystal Scale—Consequences for the Isotopic Evolution of a Poly-Metamorphic Crustal Terrane“. Geosciences 12, Nr. 1 (12.01.2022): 36. http://dx.doi.org/10.3390/geosciences12010036.
Der volle Inhalt der QuelleSoloshenko, N. G., M. V. Streletskaya, M. V. Chervyakovskaya und D. V. Kiseleva. „Implementation and experience of using methods for analyzing the isotopic composition of Sm and Nd, Rb and Sr in rock samples at the Geoanalitik Center for Collective Use“. LITHOSPHERE (Russia) 24, Nr. 2 (07.05.2024): 364–75. http://dx.doi.org/10.24930/1681-9004-2024-24-2-364-375.
Der volle Inhalt der QuelleChervyakovskaya, M. V., und V. S. Chervyakovskiy. „Determination of Sm/Nd and Sr isotopic composition using an ICP-MS Neptune Plus equipped with an NWR 213 attachment for laser ablation“. LITHOSPHERE (Russia) 21, Nr. 5 (31.10.2021): 712–23. http://dx.doi.org/10.24930/1681-9004-2021-21-5-712-723.
Der volle Inhalt der QuelleDempsey, C. S., A. N. Halliday und I. G. Meighan. „Combined Sm-Nd and Rb-Sr isotope systematics in the Donegal granitoids and their petrogenetic implications“. Geological Magazine 127, Nr. 1 (Januar 1990): 75–80. http://dx.doi.org/10.1017/s0016756800014175.
Der volle Inhalt der QuelleHuber, Miłosz A., Stanisław Hałas, Yuri N. Neradovsky, Tamara B. Bayanova, Artem W. Mokrushin und Lesia Lata. „Stable isotope geochemistry of sulfides from intrusion in Monchegorsk, northern part of Baltic Shield“. Geochronometria 43, Nr. 1 (01.06.2016): 96–101. http://dx.doi.org/10.1515/geochr-2015-0034.
Der volle Inhalt der QuelleCollerson, Kenneth D., Malcolm T. McCulloch und Allan P. Nutman. „Sr and Nd isotope systematics of polymetamorphic Archean gneisses from southern West Greenland and northern Labrador“. Canadian Journal of Earth Sciences 26, Nr. 3 (01.03.1989): 446–66. http://dx.doi.org/10.1139/e89-039.
Der volle Inhalt der QuelleNedosekova, I. L., V. A. Koroteev, T. B. Bayanova, P. A. Serov, V. I. Popova und M. V. Chervyakovskaya. „On the age of pyrochlore carbonatites from the Ilmeno-Vishnevogorsky Alkaline Complex, the Southern Urals (insights from Rb-Sr and Sm-Nd isotopic data)“. LITHOSPHERE (Russia) 20, Nr. 4 (31.08.2020): 486–98. http://dx.doi.org/10.24930/1681-9004-2020-20-4-486-498.
Der volle Inhalt der QuelleDICKIN, ALAN P. „The Chondritic Moon: a solution to the 142Nd conundrum and implications for terrestrial mantle evolution“. Geological Magazine 153, Nr. 3 (08.01.2016): 548–55. http://dx.doi.org/10.1017/s0016756815000990.
Der volle Inhalt der QuelleCarlson, Richard W., Lars E. Borg, Amy M. Gaffney und Maud Boyet. „Rb-Sr, Sm-Nd and Lu-Hf isotope systematics of the lunar Mg-suite: the age of the lunar crust and its relation to the time of Moon formation“. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 372, Nr. 2024 (13.09.2014): 20130246. http://dx.doi.org/10.1098/rsta.2013.0246.
Der volle Inhalt der QuelleSakhno, V. G., und L. S. Tsurikova. „Isotopic and geochemical features of the genesis of igneous complexes and ore-magmatic systems in the Chukotka sector of the Russian Arctic coast“. LITHOSPHERE (Russia) 20, Nr. 2 (25.04.2020): 196–211. http://dx.doi.org/10.24930/1681-9004-2020-20-2-196-211.
Der volle Inhalt der QuelleDissertationen zum Thema "Isotopie Sm-Nd"
De, Assunção Rodrigues Mariana. „Analyse de la provenance sédimentaire des bassins du Crétacé du système Andes-Amazonie-marge équatoriale et des relations avec la paléogéographie et la tectonique“. Electronic Thesis or Diss., Toulouse 3, 2023. http://www.theses.fr/2023TOU30363.
Der volle Inhalt der QuelleThe Cretaceous is characterized by major paleogeographic, geodynamic, and climatic changes, including the formation of new oceans such as the equatorial Atlantic Ocean, the continued fragmentation of Gondwana, and greenhouse effect periods. All these changes are potentially contained in the sedimentary records of the basins. The Andes-Amazonia-Equatorial Margin system is a vast sedimentary system whose geodynamic and palaeoenvironmental evolution is recorded in the Amazonian retroarc foreland basins, the Brazilian intracratonic basins, and those of the equatorial margin. In the western part (Andean region), recent studies suggest that the onset of the Andean orogeny occurred during the Late Cretaceous, but the development of drainage systems and the source of sediments deposited during the Cretaceous are still poorly understood. The Lower Cretaceous is recorded in Brazilian intracratonic and equatorial basins and bears witness to crustal rifting phases following Gondwana's break-up. The Araripe Basin is a good example of these basins since it contains a complete and particularly well-studied sedimentary record. However, the origin of the sediments from the various tectonic stages of basin formation and the Cretaceous origin of the marine incursions that affected it remain to be determined. The aim of this thesis is to propose a palaeogeographic reconstruction of the Andes-Amazonia-Equatorial Margin system during the Cretaceous and to analyze the geodynamic and tectonic changes that affected it. To do this, we used provenance methods, in particular major and trace element geochemistry, Sm and Nd isotopic composition, and U-Pb ages on zircons. The results obtained have enabled us to identify the source zones of the Araripe Basin during the pre-, syn- and post-rift phases and thus to gain a better understanding of the palaeogeographic configuration of the north-eastern region of Brazil at the beginning of the Cretaceous. The sediments in the Araripe basin come mainly from the Palaeoproterozoic (2.3-1.6 Ga) terrains of the Borborema province and the granitic plutons of the Brasiliano cycle (720-541Ma). The basin has a sedimentary history linked to the South Atlantic and equatorial break-up phases. During the pre-rift phase (~152-135 Ma), the basin was part of the Afro-Brazilian depression and received sediments from the N-NW. During the rift phase (~135-125Ma), there was a change in source due to continental break-up and the formation of the South Atlantic, with an influx of sediments from the eastern part of the Borborema province. During the post-rift phase (121-113 Ma), the basin ceased to be fed by the eastern part and marine incursions dominated the sedimentation environment. Finally, during the post-rift II phase (113-100 Ma) a last change in sources was observed, with sources to the NE reflecting the final moment of the fragmentation of Gondwana. A study of the provenance of sediments from the basins of western Amazonia (Acre and Madre de Dios) indicates that the sources are cratonic, originating mainly from the Ventuari-Tapajos (2.0 - 1.82 Ga) and Rio Negro - Juruena (1.82 - 1.54 Ga) terrains. These results indicate that a vast intracontinental drainage network ('Sanozama') emerged in response to the uplift of the Purus Arch and the cratonic regions of Brazil and the Guianas during the opening of the equatorial Atlantic Ocean. The integration of the results obtained compiled with data from the literature has made it possible to propose four palaeogeographic maps of the northern part of the South American platform. They highlight how geodynamic mechanisms linked to the opening of the South Atlantic and equatorial oceans controlled and shaped the paleogeography of this region
Chavagnac, Valérie. „Behaviour of the Sm-Nd isotopie system during metamorphism : Examples from the HT-LP metamorphic terrane of the Limpopo Belt, South Africa and the UHP metamorphic terrane of Dabieshan, Central China“. Phd thesis, Université Rennes 1, 1998. http://tel.archives-ouvertes.fr/tel-00620022.
Der volle Inhalt der QuelleNowicki, G. [Verfasser]. „Kernspektroskopische Untersuchungen der Isotone ¹³⁷Nd und ¹³⁹Sm / G. Nowicki“. Karlsruhe : KIT-Bibliothek, 2010. http://d-nb.info/118725276X/34.
Der volle Inhalt der QuelleThorogood, E. J. „Provenance of the pre-Devonian sediments of England and Wales : Sm-Nd isotopic evidence“. Thesis, University of Oxford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.293429.
Der volle Inhalt der QuelleAnglin, Carolyn Diane Carleton University Dissertation Geology. „Sm-Nd and Sr isotopic studies of scheelite from some Superior Province gold deposits“. Ottawa, 1992.
Den vollen Inhalt der Quelle findenGoodwin-Bell, Jo-Anne Stafford. „A geochemical and Sm-Nd isotopic study of Cordilleran eclogites from the Yukon-Tanana terrane“. Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape17/PQDD_0007/MQ28939.pdf.
Der volle Inhalt der QuelleKay, Andrew. „Sm-Nd isotope, major element, and trace element geochemistry of the Nashoba terrane, eastern Massachusetts“. Thesis, Boston College, 2012. http://hdl.handle.net/2345/bc-ir:107672.
Der volle Inhalt der QuelleThe Nashoba terrane in eastern Massachusetts comprises Cambrian-Ordovician mafic to felsic metavolcanic rocks and interlayered sediments metamorphosed during the mid-Paleozoic and intruded by a series of dioritic to granitic plutons during the Silurian to earliest Carboniferous. This work comprises two parts discussing the Sm-Nd isotope characteristics and major and trace element geochemistry of the Nashoba terrane: the first discusses the Cambrian-Ordovician metamorphosed units, the second discusses the Silurian-Carboniferous plutons. Part I: The Nashoba terrane in eastern Massachusetts lies between rocks of Ganderian affinity to the northwest and Avalonian affinity to the southeast. Its relationship to either domain was unclear and has been investigated. Major and trace element geochemical data indicate a mix of arc, MORB, and alkaline rift related signatures consistent with an origin of the terrane as a primitive volcanic arc-backarc complex built on thinned continental crust. Newly determined Sm-Nd isotopic data clarifies the original tectonic setting. Amphibolites of the Marlboro and Nashoba Formations have high εNd values (+4 to +7.5) consistent with formation in a primitive volcanic arc with minimal interaction between arc magmas and crust. Intermediate and felsic gneisses have moderate εNd values between +1.2 and –0.75 indicating a mixture of juvenile arc magmas and an evolved (likely basement) source. Depleted mantle model ages of 1.2 to 1.6 Ga indicate a Mesoproterozoic or older age for this source. Metasedimentary rocks have negative εNd values between –6 and –8.3 indicating derivation primarily from an isotopically evolved source (or sources). The model ages of these metasedimentary rocks (1.6 to 1.8 Ga) indicate a source area of Paleoproterozoic or older age. The εNd values and model ages of the intermediate and felsic rocks and metasedimentary rocks indicates that the basement to the Nashoba terrane is Ganderian rather than Avalonian. The Nashoba terrane therefore represents a southward continuation of Ganderian arc-backarc activity as typified by the Penobscot and/or Popelogan-Victoria arc systems and the Tetagouche-Exploits backarc basin in the northern Appalachians. Part II: Between 430 and 350 Ma the Nashoba terrane experienced episodic dioritic and granitic plutonism. Previous workers have suggested a supra-subduction zone setting for this magmatism based on the calc-alkaline nature of the diorites. Previously determined major and trace element geochemical data along with newly determined Sm-Nd isotopic data indicate that a subduction zone was active beneath the Nashoba terrane during the majority of the 430 to ca. 350 Ma magmatism (and likely throughout). Trace element geochemistry indicates a strong arc component in all magmas and suggests that the various Silurian to Carboniferous plutonic rocks of the Nashoba terrane could all have been derived by modification of a slightly enriched NMORB-type source via subduction zone input and crustal contamination. Most of the rocks from this period have intermediate εNd values consistent with contamination of juvenile magmas by an evolved source. The late Proterozoic model ages for most of these rocks suggest the Ganderian basement of the Nashoba terrane as the source of evolved material. One rhyolite from the nearby Newbury Volcanic Complex (of unknown affinity) has a moderately negative εNd value consistent with derivation by partial melting of Cambrian-Ordovician metasedimentary rocks of the Nashoba terrane. This suggests that the Newbury Volcanic Complex formed as the surface expression of mid-Paleozoic Nashoba terrane plutonism. Geochemical and isotopic similarities between the plutonic rocks of the Nashoba terrane and widespread contemporary Ganderian plutonism suggest that the Nashoba terrane remained a part of Ganderia during its transit and accretion to the Laurentian margin. Significantly younger model ages in the youngest granitic rocks indicate that Avalonian crust may have underthrust the Nashoba terrane after 400 Ma and contributed to the generation of these granites
Thesis (MS) — Boston College, 2012
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
Flageole, Janick. „Sm-Nd Isotopic Composition of Mantle-Derived Rocks from the Saglek-Hebron Gneiss Complex, Northern Labrador“. Thesis, Université d'Ottawa / University of Ottawa, 2019. http://hdl.handle.net/10393/39208.
Der volle Inhalt der QuelleLinkermann, Sean Aaron. „Emplacement of the 2.44 Ga ultramafic layered Kemi intrusion, Finland PGE, geochemical and Sm-Nd isotopic implications“. Thesis, Rhodes University, 2011. http://hdl.handle.net/10962/d1005552.
Der volle Inhalt der QuelleSchmitt, Wolfgang. „Application of the Sm-Nd Isotope System to the Late Quaternary Paleoceanography of the Yermak Plateau (Arctic Ocean)“. Diss., lmu, 2007. http://nbn-resolving.de/urn:nbn:de:bvb:19-71834.
Der volle Inhalt der QuelleBücher zum Thema "Isotopie Sm-Nd"
Survey, Ontario Geological. Geochronology Compilation Map For Ontario : Sheet 2: Southern Ontario: Grenville : Province and Environs : rb-sr, nd-sm, U-pb, and Other Isotopic Systems. S.l: s.n, 1986.
Den vollen Inhalt der Quelle findenBuchteile zum Thema "Isotopie Sm-Nd"
Champion, David C., und David L. Huston. „Applications of Neodymium Isotopes to Ore Deposits and Metallogenic Terranes; Using Regional Isotopic Maps and the Mineral Systems Concept“. In Isotopes in Economic Geology, Metallogenesis and Exploration, 123–54. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_5.
Der volle Inhalt der QuelleWaltenberg, Kathryn. „Application of the Lu–Hf Isotopic System to Ore Geology, Metallogenesis and Mineral Exploration“. In Isotopes in Economic Geology, Metallogenesis and Exploration, 189–208. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-27897-6_7.
Der volle Inhalt der QuelleAshwal, Lewis D., und Joseph L. Wooden. „Sm-Nd Isotopic Studies of Proterozoic Anorthosites: Systematics and Implications“. In The Deep Proterozoic Crust in the North Atlantic Provinces, 61–73. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_5.
Der volle Inhalt der QuelleKinny, Peter D., und Roland Maas. „12. Lu-Hf and Sm-Nd isotope systems in zircon“. In Zircon, herausgegeben von John M. Hanchar und Paul W. O. Hoskin, 327–42. Berlin, Boston: De Gruyter, 2003. http://dx.doi.org/10.1515/9781501509322-015.
Der volle Inhalt der QuelleMcCulloch, M. T. „Sm-Nd isotopic constraints on the evolution of Precambrian crust in the Australian continent“. In Proterozic Lithospheric Evolution, 115–30. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0115.
Der volle Inhalt der QuelleFan, Y., T. F. Zhou, F. Yuan, M. A. Wu, M. J. Hou, G. Voicu, Q. H. Hu und Q. M. Zhang. „Sm-Nd isotope dating of fluorites from the Xiangquan thallium deposit, Anhui Province, East China“. In Mineral Deposit Research: Meeting the Global Challenge, 381–83. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_100.
Der volle Inhalt der QuelleSoroka, Elena I., Oksana B. Azovskova, Mikhail Yu Rovnushkin, Mikhail E. Pritchin, Irina V. Smoleva, Natalia G. Soloshenko, Maria V. Streletskaya und Maria V. Zaitceva. „Isotopic (δ13C, δ18O, Rb-Sr and Sm-Nd) Studies of Carbonates from the Vorontsovskoe Gold Deposit (Northern Urals)“. In Springer Proceedings in Earth and Environmental Sciences, 245–52. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-00925-0_36.
Der volle Inhalt der QuelleKrymsky, R. S., B. V. Belyatsky, A. K. Rub und M. G. Rub. „The genesis of the rare-metal greisen Tigrinoe ore-deposit (Sikhote-Alin, Russia): Sm-Nd and Rb-Sr isotope constraints“. In Mineral Deposits at the Beginning of the 21st Century, 433–36. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003077503-110.
Der volle Inhalt der QuelleBen-Tami, Abdelhay, Said Belkacim, Bouchra Baidada, Jamal El Kabouri, Mohamed Assalmi, Mohamed Bhilisse und Mohammed Bouabdellah. „Lithostratigraphy, Whole-Rock, and Sm–Nd Isotopic Data of the Ediacaran Magmatic Rocks from the Zgounder Ag–Hg Deposit (Siroua Massif, Central Anti-Atlas, Morocco)“. In Advances in Science, Technology & Innovation, 167–71. Cham: Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-48758-3_38.
Der volle Inhalt der Quelle„The Sm–Nd method“. In Radiogenic Isotope Geology, 70–100. Cambridge University Press, 2005. http://dx.doi.org/10.1017/cbo9781139165150.005.
Der volle Inhalt der QuelleKonferenzberichte zum Thema "Isotopie Sm-Nd"
Frossard, Paul, Maud Boyet, Audrey Bouvier, Pierre Bonnand und Delphine Auclair. „Deciphering Nd and Sm Isotope Composition in Chondrites“. In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.755.
Der volle Inhalt der QuelleRay, Esha, Debajyoti Paul, Rajneesh Bhutani, Ramananda Chakrabarti und Shouye Yang. „Sm-Nd isotope systematics of Indian shales constrain the growth of Indian continental crust“. In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.14275.
Der volle Inhalt der QuelleYermakov, Y., M. Spasennykh, E. Leushina, E. Kozlova, N. Bogdanovich, A. Voropaev und Y. Kostitsyn. „Application of Sm-Nd Isotope Geochemistry for Unconventional Reservoir Characterization (On The Example of Bazhenov Formation)“. In EAGE/SPE Workshop on Shale Science 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202151022.
Der volle Inhalt der QuelleApen, Francisco, Corey J. Wall, John Cottle, Mark D. Schmitz, Andrew R. C. Kylander-Clark und Gareth G. E. Seward. „APATITES FOR DESTRUCTION: NEW REFERENCE APATITES FOR U-PB PETROCHRONOLOGY AND SM-ND AND SR ISOTOPE GEOCHEMISTRY“. In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-365621.
Der volle Inhalt der QuelleKuper, Kathy, Christopher Kirkland, Hugo Olierook, Massimo Chiaradia und Katy Evans. „Apatite Sm-Nd and U-Pb isotopes unravel crust-mantle interactions in the Fraser Zone, Western Australia“. In Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.19088.
Der volle Inhalt der QuelleAlam, Meraj ALam, Md Naushad Naushad und Talat Ahmad Ahmad. „Geochemical and Sm-Nd Isotopic Constraints on the Petrogenesis and Tectonic Significance of Magmatism in Mahakoshal Belt, Central India“. In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.32.
Der volle Inhalt der QuelleMarshall, Edward W., John C. Lassiter und Jaime D. Barnes. „NEW RE-OS AND SM-ND ISOTOPIC CONSTRAINTS ON THE TECTONIC SETTING OF THE 1.4 GA LAURENTIAN MAGMATIC EVENT“. In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298860.
Der volle Inhalt der QuelleHammerli, Johannes, und Tony I. S. Kemp. „DECOUPLING OF LU-HF AND SM-ND ISOTOPE SYSTEMS DURING CRUSTAL MELTING: AN EXAMPLE FROM THE HIDAKA METAMORPHIC BELT, JAPAN“. In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282915.
Der volle Inhalt der QuelleJabbour, Marieme, Moha Ikenne, Brian Cousens, Richard Ernst, Mustapha Souhassou, Abdelilah Benhammou und Amine Bajaddi. „A revised geodynamic significance of the Tachdamt Bleida series (Bou Azzer El Graara, central Anti-Atlas, Morocco): geochemistry and Sm-Nd isotopes“. In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12204.
Der volle Inhalt der QuelleD, Kamalakannan, und Balakrishnan S. „Mesoarchean Mafic Magmatism from Two Distinct Mantle Sources: Evidence from Sm-Nd Isotopic Studies on Metabasalts of the Gadag Greenstone Belt, Dharwar Craton, India“. In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.505.
Der volle Inhalt der QuelleBerichte der Organisationen zum Thema "Isotopie Sm-Nd"
Piercey, S. J., und J. L. Pilote. Nd-Hf isotope geochemistry and lithogeochemistry of the Rambler Rhyolite, Ming VMS deposit, Baie Verte Peninsula, Newfoundland: evidence for slab melting and implications for VMS localization. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328988.
Der volle Inhalt der QuelleBerman, R. G., B. E. Taylor, W. J. Davis, M. Sanborn-Barrie und J B Whalen. Crustal architecture and evolution of the central Thelon tectonic zone, Nunavut: insights from Sm-Nd and O isotope analysis, U-Pb zircon geochronology, and targeted bedrock mapping. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332497.
Der volle Inhalt der QuelleRoddick, J. C., R. W. Sullivan und F. O. Dudas. Precise Calibration of Tracer Compositions For Sm - Nd Isotopic Studies. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132926.
Der volle Inhalt der QuellePeterson, T. D., S. Pehrsson, T. Skulski und H. Sandeman. Compilation of Sm-Nd isotope analyses of igneous suites, western Churchill Province. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/285360.
Der volle Inhalt der QuelleAnglin, C. D. Preliminary Sm - Nd Isotopic Analyses of Scheelites From Val D'or Gold Deposits, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131262.
Der volle Inhalt der QuelleMitchell, R. K., O. van Breemen, W. J. Davis und R. Buenviaje. Sm-Nd isotopic data from the Canadian Shield north of 60 degrees latitude, northern Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2010. http://dx.doi.org/10.4095/287188.
Der volle Inhalt der QuelleTheriault, R. J. Methods for Rb-Sr and Sm-Nd isotopic analyses at the geochronology laboratory, Geological Survey of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/129062.
Der volle Inhalt der QuelleThériault, R. J., und S. Tella. Sm-Nd isotopic study on mafic volcanic rocks from the Rankin Inlet and Tavani regions, District of Keewatin, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209092.
Der volle Inhalt der Quellevan Breemen, O., S. Pehrsson und T. D. Peterson. Reconnaissance U-Pb SHRIMP geochronology and Sm-Nd isotope analyses from the Tehery-Wager Bay gneiss domain, western Churchill Province, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/224019.
Der volle Inhalt der Quellevan Breemen, O., J. R. Henderson, C. W. Jefferson, R. M. Johnstone und R. Stern. U-Pb age and Sm-Nd isotopic studies in Archean Hood River and Torp Lake supracrustal belts, northern Slave Province, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/195167.
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