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Статті в журналах з теми "REE geochemistry"
Cruz, Armanda, Pedro A. Dinis, Alberto Gomes, and Paula Leite. "Influence of Sediment Cycling on the Rare-Earth Element Geochemistry of Fluvial Deposits (Caculuvar–Mucope, Cunene River Basin, Angola)." Geosciences 11, no. 9 (September 11, 2021): 384. http://dx.doi.org/10.3390/geosciences11090384.
Повний текст джерелаGammons, Christopher H., and Scott A. Wood. "The aqueous geochemistry of REE." Chemical Geology 166, no. 1-2 (May 2000): 103–24. http://dx.doi.org/10.1016/s0009-2541(99)00186-2.
Повний текст джерелаKalender, Leyla, and Gamze Aytimur. "REE Geochemistry of Euphrates River, Turkey." Journal of Chemistry 2016 (2016): 1–13. http://dx.doi.org/10.1155/2016/1012021.
Повний текст джерелаBonev, Nikolay, Petyo Filipov, and Tanya Stoylkova. "Chemical composition of late Eocene–early Oligocene corals in reef buildups from the Thrace basin, Bulgaria–Greece: Paleoenvironmental implications." Geologica Balcanica 51, no. 1 (April 2022): 23–33. http://dx.doi.org/10.52321/geolbalc.51.1.23.
Повний текст джерелаWu, Chengyu, and Shunso Ishihara. "REE geochemistry of the Southern Thailand granites." Journal of Southeast Asian Earth Sciences 10, no. 1-2 (July 1994): 81–94. http://dx.doi.org/10.1016/0743-9547(94)90010-8.
Повний текст джерелаSuhua, Yu, and Wen Qizhong. "REE geochemistry of loess in Xinjiang, China." Chinese Journal of Geochemistry 11, no. 3 (July 1992): 277–87. http://dx.doi.org/10.1007/bf02842272.
Повний текст джерелаSalih, Makki Omer, Bo Wan, and David R. Lentz. "Geochemistry and petrogenesis of anorogenic REE-bearing peralkaline granitoids from Northern Sudan." Neues Jahrbuch für Mineralogie - Abhandlungen 197, no. 2 (October 22, 2021): 185–208. http://dx.doi.org/10.1127/njma/2021/0274.
Повний текст джерелаGreen, T. H., and N. J. Pearson. "High-pressure, synthetic loveringite-davidite and its rare earth element geochemistry." Mineralogical Magazine 51, no. 359 (March 1987): 145–49. http://dx.doi.org/10.1180/minmag.1987.051.359.16.
Повний текст джерелаBowerman, Melissa, Amy Christianson, Robert A. Creaser, and Robert W. Luth. "A petrological and geochemical study of the volcanic rocks of the Crowsnest Formation, southwestern Alberta, and of the Howell Creek suite, British Columbia." Canadian Journal of Earth Sciences 43, no. 11 (November 1, 2006): 1621–37. http://dx.doi.org/10.1139/e06-037.
Повний текст джерелаChen, Wei, Huang Honghui, Tian Bai, and Shaoyong Jiang. "Geochemistry of Monazite within Carbonatite Related REE Deposits." Resources 6, no. 4 (September 27, 2017): 51. http://dx.doi.org/10.3390/resources6040051.
Повний текст джерелаДисертації з теми "REE geochemistry"
Zhong, Shaojun. "Precipitation kinetics and partitioning of rare earth elements (REE) between calcite and seawater." Thesis, McGill University, 1993. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=41198.
Повний текст джерелаAs a consequence of solute interactions in solution and at the growing mineral surface, the calcite precipitation mechanism in seawater is complex. It is dominated by the following reversible overall reaction: $ rm Ca sp{2+}+CO sbsp{3}{2-} rightleftharpoons CaCO sb3.$ A kinetic expression is proposed which describes the precipitation rate according to this reaction. A partial reaction order of 3 with respect to CO$ sb3 sp{2-}$ is obtained.
REE have a strong affinity for calcite and substitute for Ca$ sp{2+}$. REE partition coefficients in calcite overgrowths were calculated from their concentrations in the overgrowths and their parent solutions using a non-thermodynamic homogeneous model. The concentrations were determined by chelation and gradient ion chromatography (CGIC) using a revised procedure. REE partition coefficients decrease gradually with increasing REE atomic number. They are sensitive to changes in (REE): (Ca$ sp{2+}$) and the presence of O$ sb2$ in solution, but unaffected by the precipitation rate, $ rm lbrack CO sb3 sp{2-} rbrack$ or Pco$ sb2$ of the solution. The partitioning behaviour of REE is negatively correlated to the solubility of their respective carbonates and influenced by speciation, adsorption, and subsequent surface reactions (e.g., dehydration).
Ramirez-Caro, Daniel. "Rare earth elements (REE) as geochemical clues to reconstruct hydrocarbon generation history." Thesis, Kansas State University, 2013. http://hdl.handle.net/2097/16871.
Повний текст джерелаDepartment of Geology
Matthew Totten
The REE distribution patterns and total concentrations of the organic matter of the Woodford shale reveal a potential avenue to investigate hydrocarbon maturation processes in a source rock. Ten samples of the organic matter fraction and 10 samples of the silicate-carbonate fraction of the Woodford shale from north central Oklahoma were analyzed by methods developed at KSU. Thirteen oil samples from Woodford Devonian oil and Mississippian oil samples were analyzed for REE also. REE concentration levels in an average shale range from 170 ppm to 185 ppm, and concentration levels in modern day plants occur in the ppb levels. The REE concentrations in the organic matter of the Woodford Shale samples analyzed ranged from 300 to 800 ppm. The high concentrations of the REEs in the Woodford Shale, as compared to the modern-day plants, are reflections of the transformations of buried Woodford Shale organic materials in post-depositional environmental conditions with potential contributions of exchanges of REE coming from associated sediments. The distribution patterns of REEs in the organic materials normalized to PAAS (post-Archean Australian Shale) had the following significant features: (1) all but two out of the ten samples had a La-Lu trend with HREE enrichment in general, (2) all but two samples showed Ho and Tm positive enrichments, (3) only one sample had positive Eu anomalies, (4) three samples had Ce negative anomalies, although one was with a positive Ce anomaly, (5) all but three out of ten had MREE enrichment by varied degrees. It is hypothesized that Ho and Tm positive anomalies in the organic materials of the Woodford Shale are reflections of enzymic influence related to the plant physiology. Similar arguments may be made for the Eu and the Ce anomalies in the Woodford Shale organic materials. The varied MREE enrichments are likely to have been related to some phosphate mineralization events, as the Woodford Shale is well known for having abundant presence of phosphate nodules. The trend of HREE enrichment in general for the Woodford Shale organic materials can be related to inheritance from sources with REE-complexes stabilized by interaction between the metals and carbonate ligands or carboxylate ligands or both. Therefore, a reasonable suggestion about the history of the REEs in the organic materials would be that both source and burial transformation effects of the deposited organic materials in association with the inorganic constituents had an influence on the general trend and the specific trends in the distribution patterns of the REEs. This study provides a valuable insight into the understandings of the REE landscapes in the organic fraction of the Woodford Shale in northern Oklahoma, linking these understandings to the REE analysis of an oil generated from the same source bed and comparing it to oil produced from younger Mississippian oil. The information gathered from this study may ultimately prove useful to trace the chemical history of oils generated from the Woodford Shale source beds.
Sahlström, Fredrik. "Ore Petrography and Geochemistry of some REE-bearing Fe-oxide Assemblages from the Idkerberget Deposit, Bergslagen, Sweden." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-182875.
Повний текст джерелаVarphögar av apatitjärnmalm av Kirunatyp ifrån järnmalmsbrytning i Bergslagen, Sydcentrala Sverige, innehåller förhöjda halter av sällsynta jordartsmetaller. Ett projekt vid Uppsala Universitet undersöker förekomster av sällsynta jordartsmetaller och andra kritiska element i varphögar bland annat från apatitjärnmalmer. I denna studie har prover från ett av Bergslagens apatitjärnmalmsfält, Idkerberget, undersökts geokemiskt och petrografiskt med fokus på faser som innehåller sällsynta jordartsmetaller. Deras utvinningspotential och deras relation till liknande förekomster såsom Blötberget, Grängesberg samt Kiirunavaara har också tagits i beaktning. Bulkgeokemin i proverna analyserades med ICP-EM och ICP-MS. Polerprov av malmerna undersöktes medelst optisk mikroskopi, SEM-EDS samt med WDS-mikrosondteknik. Resultaten visar att malmerna framförallt består av magnetit och hematit, med mindre mängder silikater, flourapatit, pyrit, kopparkis, monazit-(Ce), allanit-(Ce), thoriumsilikat, titanit och zirkon. Sällsynta jordartsmetaller är i huvudsak bundna i flourapatit, men metamorfa och/eller hydrotermala processer har resulterat i nybildningen av exotiska mineral såsom monazit-(Ce), allanit-(Ce), och sekundär flourapatit. Dessa egenskaper har även observerats i apatitjärnmalmer från andra platser. Proverna från Idkerberget har 1-9 gånger högre koncentration av sällsynta jordartsmetaller än jordskorpan generellt, och lätta sällsynta jordartsmetaller är de mest anrikade. Dessa halter är relativt låga jämfört med sällsynta jordartsmalmer som bryts i dagsläget, men eftersom materialet förekommer i enorma varphögar gör tillgängligheten att metallerna ändå kan utvinnas med vinst om efterfrågan på denna resurs består.
Aiglsperger, Thomas Hans. "Mineralogy and geochemistry of the platinum group elements (PGE), rare earth elements (REE) and scandium in nickel laterites." Doctoral thesis, Universitat de Barcelona, 2015. http://hdl.handle.net/10803/396340.
Повний текст джерелаInguaggiato, Claudio. "Geochemistry of Zr, Hf and REE in extreme water environments : hyperacid, hypersaline and lake waters in hydrothermal systems." Thesis, Paris 6, 2016. http://www.theses.fr/2016PA066007/document.
Повний текст джерелаThis thesis concerns the geochemistry of Zr, Hf and REE (Rare Earth Elements) in extreme water environments. The investigations were carried out in hypersaline waters covering a wide range of Eh values along Dead Sea Fault (Israel), in hyperacid waters circulating in Nevado del Ruiz volcano-hydrothermal system (Colombia) and in CO2-rich waters in Pantelleria volcano-hydrothermal system (Italy), including the alkaline lake “Specchio di Venere” within a calderic depression. The acidic sulphates waters characterized by the precipitation of alunite and jarosite show a strong LREE depletion. The REE in waters along Dead Sea Fault show MREE enrichments in waters with relative high Ca and SO4 concentrations due to the water interaction with MREE-enriched salt minerals. In the natural waters, changing of pH and Eh induce variations of Ce and Eu anomalies, due to the different behaviour of these elements with respect to the neighbours REE. In sulphate acidic waters, Zr/Hf ratios are very low down to 4.7, while quite constant Y/Ho ratio (close to the local rock value) indicates the lack of decoupling. Zr/Hf ratio increases as Cl/SO4 ratio increases. On the contrary, Zr/Hf and Y/Ho ratios in near-neutral pH waters with positive Eh values change from near-chondritic to super-chondritic. The precipitation of Fe-oxyhydroxides removes preferentially Hf and Ho with respect to Zr and Y. The interaction of atmospheric fallout from the nearby Sahara Desert with the water of the lake “Specchio di Venere” was recognized by the Zr, Hf and REE distribution. Zr, Hf and REE show the capability to trace the interaction process between open water bodies and atmospheric fallout
Baldwin, Geoffrey James. "THE STRATIGRAPHY AND GEOCHEMISTRY OF THE RAPITAN IRON FORMATION, NORTHWEST TERRITORIES AND YUKON, CANADA." Thesis, Laurentian University of Sudbury, 2014. https://zone.biblio.laurentian.ca/dspace/handle/10219/2194.
Повний текст джерелаVanderstraeten, Aubry. "Advances in geochemical tracing of atmospheric dust in Antarctica." Doctoral thesis, Universite Libre de Bruxelles, 2020. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/312773.
Повний текст джерелаRésuméLes particules atmosphériques (PA) sont un composant majeur du système Terre. Leurs propriétés optiques ainsi que leur rôle au sein des processus de nucléation des nuages ont des impacts majeurs sur le budget radiatif et hydrologique de la terre. Les PA interviennent aussi dans de nombreux cycles biogéochimiques à la surface des océans ou sur terre grâce à leur capacité à fournir des nutriments clés (e.g. Fe, P) soutenant la production primaire. Le but de ce doctorat est d’améliorer la compréhension du cycle des PA en créant de nouvelles méthodes innovatrices permettant de tracer leurs origines et quantifier leurs contributions. Nous avons développé une nouvelle méthode chromatographique optimisée pour les PA afin d’analyser six systèmes isotopiques (i.e. Pb, Nd, Sr, Zn, Cu, Fe) largement utilisés pour tracer l’origine des PA. Afin de combler un manque crucial en terme de matériaux de référence (MR), nous avons quantifié deux nouveaux MR de PA, ATD et BCR-723 (représentatifs des milieux naturels et urbains) et nous les proposons pour toutes les futures études géochimiques de PA. Nous avons aussi étudié les dépositions atmosphériques le long d’un ‘transect’ de 250 km depuis la côte Antarctique jusqu’à la station Belge Princesse Elisabeth. Premièrement, nous avons réalisé des analyses morphologiques et chimiques à l’échelle de la particule à l’aide d’un Microscope Electronique à Balayage à dispersion d’énergie (MEB-EDS). Les analyses ont montré une distribution granulométrique <5 μm ainsi qu’une variation de composition chimique (i.e. minéralogie) depuis la côte jusqu’aux Sør Rondane. Deuxièmement, afin de mieux identifier l’origine de ces PA, nous avons analysé les terres rares (REE) et développé dans son intégralité une nouvelle approche statistique permettant d’identifier les sources ainsi que leurs contributions relatives. Grâce à cela, nous avons déterminé que les échantillons à la côte proviennent du Puna-Altiplano, de Patagonie et du Sud de l’Afrique (SAF). C’est la première fois que des apports du SAF sont formellement identifiés en Antarctique. Finalement, nous avons revisité les data-set de REE des carottes de glace du projet EPICA (EDC et EDML) afin de reconstruire les apports de PA durant la dernière transition glacière/interglaciaire. Nos résultats ont montré que durant la dernière période glaciaire les PA proviennent principalement de Nouvelle-Zélande (NZ) avec des apports secondaires provenant de la partie Sud du centre de l’Ouest Argentin ainsi que de Patagonie. Une transition est marquée entre 18 et 11.6 ka BP jusqu’à un équilibre dès l’Holocène (après 11.7 ka BP) marqué par des apports de sources variées venant de Patagonie, SAF, Puna-Altiplano et NZ. Nous avons aussi démontré que les variations des contributions relatives de sources enregistrées dans les carottes de glaces sont toutes en relation avec des changements climatiques importants au niveau des régions sources impactant leur capacité à générer des PA. Notre approche statistique exploitant les REE apporte une méthode sans précédent pour identifier et quantifier les sources de PA des carottes de glace d’Antarctique et ouvre de nouvelles opportunités sur ces archives du climat et de la circulation atmosphérique de la Terre.
Doctorat en Sciences
info:eu-repo/semantics/nonPublished
Tourpin, Sylvie. "Perte des mémoires isotopiques (Nd, Sr, 0) et géochimiques (REE) primaires des komatiites au cours du métamorphisme : Exemple de la Finlande Orientale." Phd thesis, Université Rennes 1, 1991. http://tel.archives-ouvertes.fr/tel-00675899.
Повний текст джерелаPaquette, Jean-Louis. "Comportement des systèmes isotopiques U-Pb et Sm-Nd dans le métamorphisme éclogitique. Chaîne Hercynienne et chaîne Alpine." Phd thesis, Université Rennes 1, 1987. http://tel.archives-ouvertes.fr/tel-00675107.
Повний текст джерелаMartin, Hervé. "Nature, origine et évolution d'un segment de croûte continentale archéenne : contraintes chimiques et isotopiques. Exemple de la Finlande orientale." Phd thesis, Université Rennes 1, 1985. http://tel.archives-ouvertes.fr/tel-00655973.
Повний текст джерелаКниги з теми "REE geochemistry"
Bove, Dana. Compositional changes induced by hydrothermal alteration at the Red Mountain alunite deposit, Lake City, Colorado. Washington, D.C: U.S. G.P.O., 1990.
Знайти повний текст джерелаKlika, Zdeněk. Geochemistry of coal from region of the red beds bodies of the Upper Silesian Coal Basin. [Ostrava]: VŠB-Technical University Ostrava, Faculty of Mining and Geology, 1998.
Знайти повний текст джерелаShen, Glen T. Lead and cadmium geochemistry of corals: Reconstruction of historic perturbations in the upper ocean. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1986.
Знайти повний текст джерелаNordstrom, Darrell Kirk. Questa baseline and pre-mining ground-water quality investigation 25. Summary of results and baseline and pre-mining ground-water geochemistry, Red River Valley, Taos County, New Mexico, 2001-2005. Reston, Va: U.S. Geological Survey, 2008.
Знайти повний текст джерелаLucey, Keith J. Analysis of the ground-water flow system, geochemistry, and underseepage in the vicinity of the Red Rock Dam near Pella, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Знайти повний текст джерелаLucey, Keith J. Analysis of the ground-water flow system, geochemistry, and underseepage in the vicinity of the Red Rock Dam near Pella, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Знайти повний текст джерелаLucey, Keith J. Analysis of the ground-water flow system, geochemistry, and underseepage in the vicinity of the Red Rock Dam near Pella, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Знайти повний текст джерелаLucey, Keith J. Analysis of the ground-water flow system, geochemistry, and underseepage in the vicinity of the Red Rock Dam near Pella, Iowa. Iowa City, Iowa: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Знайти повний текст джерелаNordstrom, Darrell Kirk. Questa baseline and pre-mining ground-water quality investigation: Interpretation of ground-water geochemistry in catchments other than the Straight Creek catchment, Red River Valley, Taos County, New Mexico, 2002-2003. Boulder, Colo: U.S. Geological Survey, 2005.
Знайти повний текст джерелаHeggie, D. T. Continental margin transects: Geochemistry of sediments from the north east Australian continental margin, including the Great Barrier Reef slope, Queensland Plateau and Trough and the Osprey Embayment : AGSO project 121.11 and 121.38. Canberra: Australian Geological Survey Organisation, 1993.
Знайти повний текст джерелаЧастини книг з теми "REE geochemistry"
Brookins, Douglas G. "Yttrium and the Rare Earth Elements (REE)." In Eh-pH Diagrams for Geochemistry, 122–40. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73093-1_50.
Повний текст джерелаAntoniassi, Juliana Lívi, Daniel Uliana, Henrique Kahn, M. Manuela M. Lé Tassinari, and Carina Ulsen. "Assessment and Characterization of REE Minerals from an Alkali-Carbonatitic Complex." In Springer Geochemistry/Mineralogy, 173–86. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_18.
Повний текст джерелаYang, Yuangen, Congqiang Liu, Zhenli He, and Keneng Yuan. "Rare Earth Element (REE) Geochemistry During Red Soil Formation in Southern China." In The Red Soils of China, 89–100. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-1-4020-2138-1_6.
Повний текст джерелаXueyuan, Yu. "Geochemistry of Rb, Sr and REE in Niutoushan basalts in the coastal area of Fujian Province, China." In Properties and Processes of Earth' Lower Crust, 331–38. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/gm051p0331.
Повний текст джерелаWagner, Thomas, and Jörg Erzinger. "REE geochemistry of fluid-rock interaction processes related to Alpine-type fissure vein mineralisation, Rheinisches Schiefergebirge, Germany." In Mineral Deposits at the Beginning of the 21st Century, 929–32. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003077503-236.
Повний текст джерелаXie, Qiaoqin, Gao Qiu, Tianhu Chen, Xiaochun Xu, Xiaoyong Wang, Huayu Lu, Huifang Xu, and Junfeng Ji. "Palygorskite in the Late Miocene Red Clay Sediment from the Chinese Loess Plateau and Its Paleoclimatic Implications." In Springer Geochemistry/Mineralogy, 425–40. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-13948-7_42.
Повний текст джерелаStoffers, P., R. Botz, and J. Scholten. "Isotope Geochemistry of Primary and Secondary Carbonate Minerals in the Shaban-Deep (Red Sea)." In Sediments and Environmental Geochemistry, 83–94. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75097-7_5.
Повний текст джерелаBuddemeier, R. W., and J. A. Oberdorfer. "Internal Hydrology and Geochemistry of Coral Reefs and Atoll Islands: Key to Diagenetic Variations." In Reef Diagenesis, 91–111. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-82812-6_6.
Повний текст джерелаStoffers, P., and R. Botz. "Carbonate Crusts in the Red Sea: Their Composition and Isotope Geochemistry." In Facets of Modern Biogeochemistry, 242–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-73978-1_20.
Повний текст джерелаZanoni, Davide, Najeeb M. A. Rasul, Antonio Langone, and Moustafa Khorshid. "Microstructure and Geochemistry of Magmatic Dykes from the Arabian Margin, Red Sea." In Geological Setting, Palaeoenvironment and Archaeology of the Red Sea, 437–71. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99408-6_20.
Повний текст джерелаТези доповідей конференцій з теми "REE geochemistry"
Lee, Seung-Gu, and Young-Rok Park. "REE, Nd, Sr and Eu Isotope Geochemistry of Anorthosite at Sancheong Area, Korea." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1443.
Повний текст джерелаDietz, Haley, and Virginia T. McLemore. "Geochemistry of the U-Th-REE mineralized Tajo granite, Socorro County, New Mexico." In 2021 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2021. http://dx.doi.org/10.56577/sm-2021.2756.
Повний текст джерелаRiggins, Annelise M., Nelia Dunbar, Virginia McLemore, Matthew Heizler, William McIntosh, and Kwame Frempong. "Mineralogy, Geochemistry, and Chronology of the Caballo and Burro Mountains REE-Bearing Episyenites." In 2014 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2014. http://dx.doi.org/10.56577/sm-2014.269.
Повний текст джерелаVillanova-De-Benavent, Cristina, Thomas Aiglsperger, and Joaquín Proenza. "Geochemistry and mineralogy of critical metals (PGE, Co, REE, Sc) in supergene deposits." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.7888.
Повний текст джерелаOksuz, Nursel. "REE GEOCHEMISTRY, MINERALOGY AND ORIGIN OF MANGANESE IN THE ARTOVA OPHIOLITE COMPLEX, YOZGAT (TURKEY)." In SGEM2011 11th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2011. http://dx.doi.org/10.5593/sgem2011/s01.130.
Повний текст джерелаGonzález-Nistal, Santiago, Rodrigo Álvarez, Almudena Ordóñez, and Jorge Loredo. "Occurrence of Detrital Monazite within the Esva Watershed (NW Spain): EPMA Dating and REE Geochemistry." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.860.
Повний текст джерелаObregón, Cynthia, Rosa Marques, Maria Isabel Prudêncio, João Carlos Waerenborgh, Bruno Vieira, Catarina Diamantino, and Edgar Carvalho. "REE GEOCHEMISTRY AND EVALUATION OF EFFECTIVENESS OF THE PASSIVE REMEDIATION SYSTEM AT LOUSAL MINE, PORTUGAL." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6246.
Повний текст джерелаLu, Jue, Wei Chen, Yuancan Ying, and Shao-Yong Jiang. "Texture and Trace Element Geochemistry of Apatite in Carbonatite Related REE Deposits: Fingerprinting Magmatic-Hydrothermal Processes." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1641.
Повний текст джерелаYoshiya, Kazumi, Keita Itano, and Tsuyoshi Iizuka. "U-Pb chronology, REE geochemistry, and Nd isotope ratios of detrital monazites from major North and South American rivers." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12006.
Повний текст джерелаWang, Chunzeng, John F. Slack, Martin Yates, David R. Lentz, Anjana Shah, Amber H. Whittaker, and Robert Marvinney. "THE NEWLY DISCOVERED TRACHYTE-HOSTED PENNINGTON MOUNTAIN REE-NB-ZR DEPOSIT IN NORTHERN MAINE: PRELIMINARY GEOLOGY, MINERALOGY, AND GEOCHEMISTRY." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379619.
Повний текст джерелаЗвіти організацій з теми "REE geochemistry"
Grunsky, E. C., P. W. B. Friske, and R. McNeil. A re-evaluation of lake sediment geochemistry from the Bancroft region of Ontario; recognizing geochemical background and sources of uranium and REE mineralization. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2014. http://dx.doi.org/10.4095/294924.
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 джерелаManor, 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 джерелаMueller, C., S. J. Piercey, M. G. Babechuk, and D. Copeland. Stratigraphy and lithogeochemistry of the Goldenville horizon and associated rocks, Baie Verte Peninsula, Newfoundland. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328990.
Повний текст джерелаMowbray, B., and S. J. Pehrsson. Geochemistry, petrology, and aeromagnetic mapping of the Orpheus dykes, south Rae Craton, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/311306.
Повний текст джерелаAcosta-Góngora, P., E. Martel, and S. J. Pehrsson. Geochemistry results from the south Rae mapping project, Northwest Territories, 2015 and 2016 field seasons. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2018. http://dx.doi.org/10.4095/306501.
Повний текст джерелаEvans, Carol. The Geology, Geochemistry, and Alteration of Red Butte, Oregon: A Precious Metal-Bearing Paleo Hot Spring System. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.5328.
Повний текст джерелаZagorevski, A., C. R. van Staal, J. H. Bédard, A. Bogatu, D. Canil, M. Coleman, M. Golding, et al. Overview of Cordilleran oceanic terranes and their significance for the tectonic evolution of the northern Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326053.
Повний текст джерелаZhang, S. Geochemistry data from three oil shale intervals in unit 1, Red Head Rapids Formation (Upper Ordovician) on Southampton Island. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/288109.
Повний текст джерелаRegis, D., and M. Sanborn-Barrie. Delimiting the extent of 'Boothia terrane' crust, Nunavut: new U-Pb geochronological results. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330703.
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