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Статті в журналах з теми "Hf isotopes zircon"
Gao, Peng, Chris Yakymchuk, Jian Zhang, Changqing Yin, Jiahui Qian, and Yanguang Li. "Preferential dissolution of uranium-rich zircon can bias the hafnium isotope compositions of granites." Geology 50, no. 3 (December 1, 2021): 336–40. http://dx.doi.org/10.1130/g49656.1.
Повний текст джерелаVezinet, Adrien, Emilie Thomassot, Yan Luo, Chiranjeeb Sarkar, and 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, no. 1 (January 12, 2022): 36. http://dx.doi.org/10.3390/geosciences12010036.
Повний текст джерелаHuang, Chao, Hao Wang, Jin-Hui Yang, Lie-Wen Xie, Yue-Heng Yang, and Shi-Tou Wu. "Further Characterization of the BB Zircon via SIMS and MC-ICP-MS for Li, O, and Hf Isotopic Compositions." Minerals 9, no. 12 (December 11, 2019): 774. http://dx.doi.org/10.3390/min9120774.
Повний текст джерелаViehmann, Sebastian. "Hf-Nd Isotopes in Archean Marine Chemical Sediments: Implications for the Geodynamical History of Early Earth and Its Impact on Earliest Marine Habitats." Geosciences 8, no. 7 (July 16, 2018): 263. http://dx.doi.org/10.3390/geosciences8070263.
Повний текст джерелаDu, Bin, Zian Yang, Lifei Yang, Qi Chen, Jiaxuan Zhu, Kangxing Shi, Gao Li, Lei Wang, and Jia Lu. "Zircon Hf-Isotopic Mapping Applied to the Metal Exploration of the Sanjiang Tethyan Orogenic Belt, Southwestern China." Applied Sciences 12, no. 8 (April 18, 2022): 4081. http://dx.doi.org/10.3390/app12084081.
Повний текст джерелаvan Schijndel, V., G. Stevens, C. Lana, T. Zack, and D. Frei. "De Kraalen and Witrivier Greenstone Belts, Kaapvaal Craton, South Africa: Characterisation of the Palaeo-Mesoarchaean evolution by rutile and zircon U-Pb geochronology combined with Hf isotopes." South African Journal of Geology 124, no. 1 (March 1, 2021): 17–36. http://dx.doi.org/10.25131/sajg.124.0011.
Повний текст джерелаAndersen, T., M. A. Elburg, and J. Lehmann. "Enigmatic provenance signature of sandstone from the Okwa Group, Botswana." South African Journal of Geology 123, no. 3 (September 1, 2020): 331–42. http://dx.doi.org/10.25131/sajg.123.0022.
Повний текст джерелаZhang, Wei, David R. Lentz, and Kathleen G. Thorne. "Petrogenesis of the Nashwaak Granite, West-Central New Brunswick, Canada: Evidence from Trace Elements, O and Hf Isotopes of Zircon, and O Isotopes of Quartz." Minerals 10, no. 7 (July 9, 2020): 614. http://dx.doi.org/10.3390/min10070614.
Повний текст джерелаLIU, YU, KUNGUANG YANG, ALI POLAT, and XIAO MA. "Reconstruction of the Cryogenian palaeogeography in the Yangtze Domain: constraints from detrital age patterns." Geological Magazine 156, no. 07 (August 20, 2018): 1247–64. http://dx.doi.org/10.1017/s0016756818000535.
Повний текст джерелаSun, Xiang, Yongjun Lu, Qiang Li, and Ruyue Li. "A Downgoing Indian Lithosphere Control on Along-Strike Variability of Porphyry Mineralization in the Gangdese Belt of Southern Tibet." Economic Geology 116, no. 1 (November 23, 2020): 29–46. http://dx.doi.org/10.5382/econgeo.4768.
Повний текст джерелаДисертації з теми "Hf isotopes zircon"
Pepper, Martin Bailey. "Magmatic History and Crustal Genesis of South America: Constraints from U-Pb Ages and Hf Isotopes of Detrital Zircons in Modern Rivers." Diss., The University of Arizona, 2014. http://hdl.handle.net/10150/347220.
Повний текст джерелаCouzinié, Simon. "Evolution of the continental crust and significance of the zircon record, a case study from the French Massif Central." Thesis, Lyon, 2017. http://www.theses.fr/2017LYSES035.
Повний текст джерелаThe formation of the continental crust is a major consequence of Earth differentiation. Understanding how the crust formed and evolved through time is paramount to locate the vast mineral deposits hosted therein and address its influence on the global climate, ultimately affecting the development of terrestrial life. Recent advances on the topic of continental crust evolution benefited from improvements of analytical techniques enabling in situ measurements of U-Pb- Hf-O isotope compositions in zircon, a widespread accessory mineral of continental igneous rocks. The time constrains derived from the U-Pb chronometer coupled with the petrogenetic information retrieved from Hf-O isotope signatures are currently used to unravel the diversity and succession of magmatic events affecting the continental crust at the regional and global scales. This study reconstructs the evolutionary path followed by the crust segment today exposed in the eastern part of the French Massif Central (FMC), a portion of the Variscan belt of Western Europe, with the aim to investigate the potential flaws of the zircon record of crust evolution. In this scope, the origin and geodynamic significance of the constituent FMC lithological units are tackled by combining conventional petrological observations with zircon U-Pb-Hf-O isotope data. The results obtained following this integrated approach are then confronted to the conclusions that would have been drawn solely from zircon isotopic signatures, taken out of their petrological context, as is commonly performed in studies investigating crust evolution. The oldest rocks of the FMC correspond to Ediacaran (590_550 Ma) meta-sediments deposited in back-arc basins along the northern Gondwana margin. Such basins were fed by a mixed detritus originating from the adjacent Cadomian magmatic arc and a distal Gondwana source, presumably the Sahara Metacraton. Partial melting of these meta-sediments at the Ediacaran/Cambrian boundary led to voluminous S-type granitic magmatism, pinpointing a first major crust reworking event in the FMC. The origin of anatexis likely stems from the transient thickening of the hot, back-arc crust caused by the flattening of the Cadomian subduction. Subordinate melting of the depleted backarc mantle at that time is also documented. During the Lower Paleozoic, rifting of the northern Gondwana provoked coeval crust and (limited) mantle melting. Mantle-derived igneous rocks show markedly diverse trace element and isotopic signatures, consistent with a very heterogeneous mantle source pervasively modi_ed by the Cadomian subduction. Finally, the Variscan collision resulted in crustal melting as evidenced by the emplacement of S-type granites and the formation of migmatite domes, the spatial distribution of which being partly controlled by the crustal architecture inherited from pre-orogenic events. Synchronous intrusion of mafic mantle-derived magmas and their differentiates testify for Variscan post-collisional new continental crust production in the FMC. Two major inconsistencies exist between these results and the zircon record. First, zircon Hf model ages would point to substantial Mesoproterozoic crust formation in the FMC whereas more than 60% of the crust is actually Neoproterozoic in age. Second, new additions to the continental crust volume during the Variscan orogeny are not recorded even though 5 to 10% of the exposed crust formed at that time. The origin of both discrepancies inherently lies in the mixed isotopic signature carried by many zircon grains. Such equivocal information can only be detected when additional petrological constrains on the zircon host rocks are available and provide guidance in interpreting the zircon record of crust evolution
Liu, Chaohui, and 刘超辉. "Paleoproterozoic basins in the Trans-North China Orogen: stratigraphic sequences, U-PB ages and HF isotopes of detritalzircons and tectonic implications." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B47163902.
Повний текст джерелаpublished_or_final_version
Earth Sciences
Doctoral
Doctor of Philosophy
Reid, Mattie Morgan. "Forearc basin detrital zircon provenance of Mesozoic terrane accretion and translation, Talkeetna Mountains-Matanuska Valley, south-central Alaska." Thesis, University of Iowa, 2017. https://ir.uiowa.edu/etd/5611.
Повний текст джерелаGudelius, Dominik [Verfasser], and A. [Akademischer Betreuer] Zeh. "Petrogenetic Significance of Zircon in Mafic and Felsic Rocks of the Bushveld Complex: Melt Inclusions, Physicochemical Conditions and Hf Isotopes / Dominik Gudelius ; Betreuer: A. Zeh." Karlsruhe : KIT-Bibliothek, 2020. http://d-nb.info/1223027945/34.
Повний текст джерелаDemouy, Sophie. "La naissance des Andes au Crétacé supérieur : origine et construction du Batholite côtier sud-péruvien (région d'Arequipa)." Toulouse 3, 2012. http://thesesups.ups-tlse.fr/2201/.
Повний текст джерелаDuring the Late Cretaceous and Paleocene, intense magmatic arc activity resulted in the building of a continuous relief along the Peruvian margin. This arc growth coincided with the only known significant uplift along the coastal southern Peru. Our study has focused in the Arequipa area, on a batholith segment extending 80x60 km for a thickness bigger than 7 km. The structural study describes an object that is complex and consists of different plutonic units, that for some underwent extensive deformation syn to post emplacement. Major faults affect the batholith as a consequence of tectonic strains and exaggerate growth of the arc. The geochronological study indicates a discontinuous construction of the batholith, during the Jurassic (200-175 Ma) and the Late Cretaceous-Paleocene (90-60 Ma). Exploitation of the geochemistry and isotopic data (Hf, Sr, Nd) allows to identify an initiation stage of the arc during which fractional crystallization and mixing are predominant, and a thermal maturation stage during which magmas are homogenized in the deep crust, and evolve by fractional crystallization until the batholith level. This period leads to the construction of more than 70 % of the batholith and can thus be considered as a flare-up event. This event is characterized by juvenile signatures and also contributes significantly to the growth of the continental crust
Canile, Fernanda Maciel. "Geologia isotópica em zircões detríticos (U-Pb, Hf e O) e em rocha total (Sm-Nd e Pb-Pb) das rochas da Bacia do Paraná em Santa Catarina." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-24022016-140417/.
Повний текст джерелаU-Pb, Hf and O isotope data were obtained from detrital zircons from late Paleozoic-early Mesozoic units from Paraná Basin, southeastern Brazil, in order to constain the provenance of the sediments, as well as to contribute to the understanding of the tectonic evolution of the basin. Whole rock Sm-Nd and Pb-Pb isotopic signatures were also taken in order to help the interpretation. The studied section, White Column in Santa Catarina state, includes rocks from 11 stratigraphic units (from base to top): Rio do Sul Formation, Rio Bonito Formation (Triunfo, Paraguaçu and Siderópolis members), Palermo Formation, Irati Formation, Serra Alta Formation, Teresina Formation, and Rio do Rasto Formation (Serrinha and Morro Pelado members) and Botucatu Formation. U-Pb ages were obtained on 1941 detrital zircons and range from 242 Ma to 3400 Ma. All sedimentary units show four main detrital age groups, Neoarchean (2700-2500 Ma), mid-Paleoproterozoic (2000-1800 Ma), Grenvillian (1100-900 Ma) and Brasiliano (850-490 Ma), reflecting the importance of the Precambrian basement bordering the east side of the basin, such as Dom Feliciano, Kaoko and Namaque-Natal Belts as source areas, including the local basement that was dated at 584 Ma. The Siderópolis Member shows an important change in the source of sediments with a Permian age-peak (266 to 290 Ma). This age-peak persists towards the top of the section until the Botucatu Formation. O and Hf isotopic signatures from the detrital zircons show that a portion of the mid-Paleoproterozoic grains is probably from rocks of the presently covered basement, which was exposed until the deposition of the Rio Bonito Formation. O and Hf isotopes also show that some Grenvillian aged zircons are from Argentinian rocks, which implies a long transport distance. Isotopic signatures of part of the Permian grains also link them to sources from Argentina and Chile, and part of these grains has more rounded shapes, suggesting that they reached the basin after long distance traveling on subaquatic environment and nor only through the air (ash falls) as it is commonly accepted. Other younger age peaks (Ordovician to Carboniferous) found from Palermo Formation upsection are also linked to Argentinian and Chilean sources, showing the importance of distant sources during the filling of the basin. The Sm-Nd and Pb-Pb data on whole rocks show that the sediments from the Paraná Basin present predominance of sources with crustal origin. Osotopic signatures are similar to granitoid rocks from Santa Catarina, Ribeira Belt, Brazilian Shield, Namaqua-Natal and Kaoko Belts, as well as the Arequipa-Antofalla terranes (Andes basement) and granitoids from North Patagonia. These data corroborate the observed detrital zircon patterns thar point to both proximal and distal source areas. \'T IND.DM\' model ages older than 1.4 Ga and more negative (-10 to -15) epsilon values were observed in the lower units (Rio do Sul Formation to Paraguaçu Member), while the upper units show \'\'épsilos\' IND.Nd(0)\' values ranging from -6 to -12 and \'T IND. DM\' model ages younger than 1.5 Ga, corroborating the addition of a younger source starting from the Siderópolis Member deposition upwards, as noted by detrital zircon data (Permian age-peak).
Guitreau, Martin. "Les isotopes de l'hafnium dans les TTG et leurs zircons : témoins de la croissance des premiers continents." Phd thesis, Ecole normale supérieure de lyon - ENS LYON, 2012. http://tel.archives-ouvertes.fr/tel-00713096.
Повний текст джерелаLuo, Yan. "U-Pb age and Hf isotopic study of detrital zircons from the Liaohe Group constraints on the evolution of the Jiao-Liao-Ji Belt, North China craton /." Click to view the E-thesis via HKUTO, 2005. http://sunzi.lib.hku.hk/hkuto/record/B36639242.
Повний текст джерелаXia, Xiaoping. "Spot U-Pband Hf isotope analyses of detrital zircons from the khondalites in the western block of the North China craton." Click to view the E-thesis via HKUTO, 2005. http://sunzi.lib.hku.hk/hkuto/record/B35773698.
Повний текст джерелаЧастини книг з теми "Hf isotopes zircon"
Su, Ben-Xun. "Zircon U–Pb Geochronlogy and Hf–O Isotopes." In Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication, 69–106. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-54262-6_5.
Повний текст джерелаWu, Meiling. "Zircon U–Pb Geochronology and Hf Isotopes of Major Lithologies from the Jiaodong Terrane." In Ages, Geochemistry and Metamorphism of Neoarchean Basement in Shandong Province, 49–78. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-662-45343-8_4.
Повний текст джерелаWu, Meiling. "Zircon U–Pb Geochronology and Hf Isotopes of Major Lithologies from the Yishui Terrane." In Ages, Geochemistry and Metamorphism of Neoarchean Basement in Shandong Province, 79–108. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-662-45343-8_5.
Повний текст джерелаKinny, Peter D., and Roland Maas. "12. Lu-Hf and Sm-Nd isotope systems in zircon." In Zircon, edited by John M. Hanchar and Paul W. O. Hoskin, 327–42. Berlin, Boston: De Gruyter, 2003. http://dx.doi.org/10.1515/9781501509322-015.
Повний текст джерелаOsipova, Tatyana A., Maria V. Zaitceva, and Sergei Votyakov. "U–Pb Age and Analysis of the Lu–Hf Isotope System of Zircon from Granitoids of the Final Phases of the Nepluyevsky Pluton (The Southern Urals)." In Springer Proceedings in Earth and Environmental Sciences, 153–60. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-00925-0_24.
Повний текст джерелаSavko, Konstantin A., Maria V. Zaitceva, Sergei Votyakov, and Sergey V. Tsybulyaev. "Hf Isotopic Composition of Zircons from the Granodiorites of the Talovsky Intrusion as the Evidence for the Juvenile Paleoproterozoic Crust of the Vorontsovsky Terrane, Eastern Sarmatia." In Springer Proceedings in Earth and Environmental Sciences, 215–20. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-00925-0_32.
Повний текст джерелаGottlieb, Eric S., Elizabeth L. Miller, John W. Valley, Christopher M. Fisher, Jeffrey D. Vervoort, and Kouki Kitajima. "Zircon petrochronology of Cretaceous Cordilleran interior granites of the Snake Range and Kern Mountains, Nevada, USA." In Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma). Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2555(02).
Повний текст джерелаPollock, Jeffrey C., Sandra M. Barr, Deanne van Rooyen, and Chris E. White. "Insights from Lu-Hf zircon isotopic data on the crustal evolution of Avalonia and Ganderia in the northern Appalachian orogen." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(08).
Повний текст джерелаThompson, M. D., S. M. Barr, and J. C. Pollock. "Evolving views of West Avalonia: Perspectives from southeastern New England, USA." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2554(03).
Повний текст джерелаOrtega-Flores, Berlaine, Luigi A. Solari, Michelangelo Martini, and Carlos Ortega-Obregón. "The Guerrero terrane, a para-autochthonous block on the paleo-Pacific continental margin of North America: Evidence from zircon U-Pb dating and Hf isotopes." In Southern and Central Mexico: Basement Framework, Tectonic Evolution, and Provenance of Mesozoic–Cenozoic Basins. Geological Society of America, 2020. http://dx.doi.org/10.1130/2020.2546(08).
Повний текст джерелаТези доповідей конференцій з теми "Hf isotopes zircon"
Tomson, J. K., and J. Amal Dev. "Crustal evolution of south Indian granulites: Insights from zircon Hf isotopes." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10115.
Повний текст джерелаYang, Jin-Hui, Ji-Heng Zhang, Jing-Yuan Chen, and Jin-Feng Sun. "Mesozoic Lithospheric Rejuvenation of South China: Evidence from Magmatic Zircon Hf-O Isotopes." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2989.
Повний текст джерелаTurnbull, Rose, Joshua Schwartz, Marco Fiorentini, Richard Jongens, Thomas Ludwig, Noreen Evans, Brad McDonald, and Keith Klepeis. "Mapping the 4D Lithospheric Architecture of Zealandia Using Zircon O and Hf Isotopes in Plutonic Rocks." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2637.
Повний текст джерелаLi, Shan, Sun-Lin Chung, Yu-Ming Lai, Azman Ghani, Hao-Yang Lee, and Sayed Murtadha. "Mesozoic Juvenile Crustal Growth in the Easternmost Tethys: New Evidence from Zircon Hf Isotopes in Sumatran Granitoids, Indonesia." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1511.
Повний текст джерелаLiu, Hangyu, Ryan McKenzie, Cody Colleps, Wei Chen, Yuan-Can Ying, Lisa Stockli, Apsorn Sardsud, and Danny Stockli. "Tracking Permian–Triassic tectonic transitions in Thailand via detrital zircon U-Pb ages, Hf isotopes and trace elements." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6582.
Повний текст джерелаQin, Zhengwei, and Wolfgang Siebel. "The source nature, magma evolution of I-type granites revealed by zircon morphology and grain-scale Hf-O isotopes." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.13180.
Повний текст джерелаJohnston, Scott, Andrew Kylander-Clark, and Andrew P. Barth. "TRACKING CRETACEOUS CORDILLERAN MAGMATIC ARC PETROGENESIS USING COUPLED DETRITAL ZIRCON GEOCHRONOLOGY, HF ISOTOPES, AND GEOCHEMISTRY FROM MODERN SIERRA NEVADA SAND." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370238.
Повний текст джерелаKumar, Santosh, Kapil Panwar, Keewook Yi, Youn-Joong Jeong, Subhransu Pani, and Umesh Sharma. "Petrology and U-Pb-Lu-Hf zircon isotopes of mafic to hybrid synplutonic dykes from Ladakh Batholith, Trans Himalaya, India." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7472.
Повний текст джерелаCouper, Samantha, Barbara P. Nash, Michael Stearns, and Diego P. Fernandez. "DUAL MULTICOLLECTOR LASS-ICP-MS FOR LU-HF AND U-PB ISOTOPES: APPLICATION TO ZIRCON IN RHYOLITE FROM THE YELLOWSTONE HOTSPOT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285448.
Повний текст джерелаXue, Yiting, Jie Tang, Wenliang Xu, and Jinpeng Luan. "Detrital zircon U–Pb ages and Hf isotopes of Neoproterozoic strata in the Songnen Massif: Implications for basement composition and tectonic affinity." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12990.
Повний текст джерелаЗвіти організацій з теми "Hf isotopes zircon"
Manor, M. J., and S. J. Piercey. Whole-rock lithogeochemistry, Nd-Hf isotopes, and in situ zircon geochemistry of VMS-related felsic rocks, Finlayson Lake VMS district, Yukon. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328992.
Повний текст джерелаDe Matheus Marques Dos Santos, Mariana, Cláudia Regina Passarelli, Miguel Angelo Stipp Basei, Antonio Roberto Saad, Paulo Roberto Dos Santos, and Oswaldo Siga Júnior. Zircon U Pb ages and Hf isotopes tracking the origin of Permian Paraná Basin ash fall layers: are they coming from Choiyoi formation? Peeref, October 2022. http://dx.doi.org/10.54985/peeref.2210p5895640.
Повний текст джерелаMatte, S., M. Constantin, and R. Stevenson. Mineralogical and geochemical characterisation of the Kipawa syenite complex, Quebec: implications for rare-earth element deposits. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329212.
Повний текст джерелаPeytcheva, Irena, Albrecht von Quadt, Lubomira Macheva, Krastina Kolcheva, and Stoyan Sarov. Relics of Devonian Oceanic Lithosphere in Byala Reka Dome, Eastern Rhodopes: Evidence from Zircon U‑Pb Dating and Hf‑isotope Tracing. "Prof. Marin Drinov" Publishing House of Bulgarian Academy of Sciences, December 2018. http://dx.doi.org/10.7546/crabs.2018.12.10.
Повний текст джерелаTodd, Erin, Andrew Kylander-Clark, Alicja Wypych, Evan Twelker, and K. R. Sicard. U-Pb and Lu-Hf isotope, age, and trace-element data from zircons at four sites in the western Alaska Range and Talkeetna Mountains, Alaska. Alaska Division of Geological & Geophysical Surveys, April 2017. http://dx.doi.org/10.14509/29717.
Повний текст джерелаTodd, Erin, Alicja Wypych, and Andrew Kylander-Clark. U-Pb and Lu-Hf isotope, age, and trace element data from zircon separates from the Tanacross D-1, and parts of D-2, C-1, and C-2 quadrangles. Alaska Division of Geological & Geophysical Surveys, July 2019. http://dx.doi.org/10.14509/30198.
Повний текст джерела