Добірка наукової літератури з теми "REE-U enrichment"
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Статті в журналах з теми "REE-U enrichment"
Lentz, David. "Radioelement distribution in U, Th, Mo, and rare-earth-element pegmatites, skarns, and veins in a portion of the Grenville Province, Ontario and Quebec." Canadian Journal of Earth Sciences 28, no. 1 (January 1, 1991): 1–12. http://dx.doi.org/10.1139/e91-001.
Повний текст джерелаMcLeod, Claire, and Barry Shaulis. "Rare Earth Elements in Planetary Crusts: Insights from Chemically Evolved Igneous Suites on Earth and the Moon." Minerals 8, no. 10 (October 16, 2018): 455. http://dx.doi.org/10.3390/min8100455.
Повний текст джерелаDubyna, O. V., S. G. Kryvdik, I. A. Shvaika, I. D. Shvaika, and L. I. Proskurka. "APATITE GEOCHEMISTRY IN ROCKS OF KORSUN-NOVOMYRHOROD ANORTOSITE-RAPAKIVI GRANITE PLUTON." Mineralogical Journal 44, no. 3 (2022): 48–66. http://dx.doi.org/10.15407/mineraljournal.44.03.048.
Повний текст джерелаMcCafferty, Anne E., Douglas B. Stoeser, and Bradley S. Van Gosen. "Geophysical interpretation of U, Th, and rare earth element mineralization of the Bokan Mountain peralkaline granite complex, Prince of Wales Island, southeast Alaska." Interpretation 2, no. 4 (November 1, 2014): SJ47—SJ63. http://dx.doi.org/10.1190/int-2014-0010.1.
Повний текст джерелаMolnár, Zsuzsa, Gabriella B. Kiss, István Dunkl, György Czuppon, Federica Zaccarini, and István Dódony. "Geochemical characteristics of Triassic and Cretaceous phosphorite horizons from the Transdanubian Mountain Range (western Hungary): genetic implications." Mineralogical Magazine 82, S1 (March 21, 2018): S147—S171. http://dx.doi.org/10.1180/minmag.2017.081.103.
Повний текст джерелаΠΕΡΓΑΜΑΛΗΣ, Φ., Δ. Ε. ΚΑΡΑΓΕΩΡΓΙΟΥ та Α. ΚΟΥΚΟΥΛΗΣ. "Συμβολή της ακτινοβολίας γ στον εντοπισμό αποθεματικού δυναμικού Ti, σπάνιων γαιών Th, U, Au παράκτιας ζώνης Νέας Περά- μου - Λουτρών Ελευθέρων, Ν. Καβάλας". Bulletin of the Geological Society of Greece 34, № 3 (1 січня 2001): 1023. http://dx.doi.org/10.12681/bgsg.17707.
Повний текст джерелаHassan, Kamaleldin M. "Trace elements and REE enrichment at Seboah Hill, SW Egypt." Mineralogia 49, no. 1-4 (December 1, 2018): 47–65. http://dx.doi.org/10.2478/mipo-2018-0007.
Повний текст джерелаDupuy, C., J. Dostal, and J. L. Bodinier. "Geochemistry of spinel peridotite inclusions in basalts from Sardinia." Mineralogical Magazine 51, no. 362 (October 1987): 561–68. http://dx.doi.org/10.1180/minmag.1987.051.362.10.
Повний текст джерелаSchneider, Petra, Dražen Balen, Joachim Opitz, and Hans-Joachim Massonne. "Dating and geochemistry of zircon and apatite from rhyolite at the UNESCO geosite Rupnica (Mt. Papuk, northern Croatia) and the relationship to the Sava Zone." Geologia Croatica 75, no. 2 (June 23, 2022): 249–67. http://dx.doi.org/10.4154/gc.2022.19.
Повний текст джерелаPlatt, R. G., F. Wall, C. T. Williams, and A. R. Woolley. "Zirconolite, chevkinite and other rare earth minerals from nepheline syenites and peralkaline granites and syenites of the Chilwa Alkaline Province, Malawi." Mineralogical Magazine 51, no. 360 (June 1987): 253–63. http://dx.doi.org/10.1180/minmag.1987.051.360.07.
Повний текст джерелаДисертації з теми "REE-U enrichment"
Kontonikas-Charos, A. "Albitization and REE-U-enrichment in IOCG systems: insights from Moonta-Wallaroo, Yorke Peninsula, South Australia." Thesis, 2013. http://hdl.handle.net/2440/106289.
Повний текст джерелаIron Oxide Copper Gold (IOCG) deposits are the products of crustal-scale metasomatic alteration, generally considered to be associated with the emplacement of large felsic intrusions. These systems are typified by zoned, broad alteration haloes comprising the products of an early, barren albitization event, and late, ore-hosting potassic/calcic (skarn) alteration associated with mineralization. Yttrium and rare earth elements (REY), and also uranium, are prominent components of most IOCG systems. The REY-signatures of feldspars and accessory apatite, Fe-(Ti)-oxides and other minerals are geochemical tracers of alteration stages within a magmatic-hydrothermal system. This study sets out to identify links between magmatism and initiation of hydrothermal activity, and to test the hypothesis that albitization is a pre-requisite stage for REE-U enrichment in magmatically-derived IOCG systems. The compositions and trace element concentrations in key minerals have been analysed using scanning electron microscopy, electron probe microanalysis and laser-ablation inductively-coupled plasma mass spectrometry in a varied range of magmatic to metasedimentary lithologies from the Moonta-Wallaroo region, an area in which broad regional-scale alkali alteration is recognised. Results confirm a strong link between albitization and REE-U-enrichment. The process of albitization is seen to consume, redistribute and lock-in REY, LILE and HFSE via complex fluid-rock reactions dependent on the pre-existing mineral assemblages and fluid characteristics, providing a holistic model for IOCG-driven alkali metasomatism. The trace element signatures recorded by K-feldspar reflect a transition from magmatic to hydrothermal stages within an evolving IOCG system. Although further constraints on these signatures are required, they could prove invaluable in mineral exploration as they suggest a quantifiable distinction between alteration associated with mineralization, and regional background. This hypothesis requires testing elsewhere in the Olympic Province and in analogous terranes.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Тези доповідей конференцій з теми "REE-U enrichment"
Karl, Susan M., George Case, Elizabeth Drewes-Todd, Douglas C. Kreiner, Thomas P. Miller, and Alan Pongratz. "MINERALOGIC AND GEOCHEMICAL IMPLICATIONS FOR ENRICHMENT OF U-TH-REE IN SYENITE DIKES ON THE EASTERN SEWARD PENINSULA, ALASKA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335299.
Повний текст джерелаЗвіти організацій з теми "REE-U enrichment"
Gadd, M. G., J. M. Peter, T A Fraser, and D. Layton-Matthews. Paleoredox and lithogeochemical indicators of the environment of formation and genesis of the Monster River hyper-enriched black shale showing, Yukon. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328004.
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