Relevant bibliographies by topics / Granirer

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Academic literature on the topic 'Granirer'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 February 2022

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Journal articles on the topic "Granirer"

1

Matzkuhn, B. "Pnina Granirer: a dancing line." Canadian Medical Association Journal 173, no. 11 (November 22, 2005): 1364–65. http://dx.doi.org/10.1503/cmaj.051402.

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Filali, Mahmoud, and Jorge Galindo. "Extreme non-Arens regularity of the group algebra." Forum Mathematicum 30, no. 5 (September 1, 2018): 1193–208. http://dx.doi.org/10.1515/forum-2017-0117.

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AbstractThe Banach algebras of Harmonic Analysis are usually far from being Arens regular and often turn out to be as irregular as possible. This utmost irregularity has been studied by means of two notions: strong Arens irregularity, in the sense of Dales and Lau, and extreme non-Arens regularity, in the sense of Granirer. Lau and Losert proved in 1988 that the convolution algebra {L^{1}(G)} is strongly Arens irregular for any infinite locally compact group. In the present paper, we prove that {L^{1}(G)} is extremely non-Arens regular for any infinite locally compact group. We actually prove the stronger result that for any non-discrete locally compact group G, there is a linear isometry from {L^{\infty}(G)} into the quotient space {L^{\infty}(G)/\mathcal{F}(G)}, with {\mathcal{F}(G)} being any closed subspace of {L^{\infty}(G)} made of continuous bounded functions. This, together with the known fact that {\ell^{\infty}(G)/\mathscr{W\!A\!P}(G)} always contains a linearly isometric copy of {\ell^{\infty}(G)}, proves that {L^{1}(G)} is extremely non-Arens regular for every infinite locally compact group.
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FEELY, MARTIN, DAVID SELBY, JON HUNT, and JAMES CONLIFFE. "Long-lived granite-related molybdenite mineralization at Connemara, western Irish Caledonides." Geological Magazine 147, no. 6 (April 22, 2010): 886–94. http://dx.doi.org/10.1017/s0016756810000324.

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AbstractNew Re–Os age determinations from the Galway Granite (samples: KMG = 402.2 ± 1.1 Ma, LLG = 399.5 ± 1.7 Ma and GBM = 383.3 ± 1.1 Ma) show that in south Connemara, late Caledonian granite-related molybdenite mineralization extended from c. 423 Ma to c. 380 Ma. These events overlap and are in excellent agreement with the published granite emplacement history determined by U–Pb zircon geochronology. The spatial distribution of the late-Caledonian Connemara granites indicates that initial emplacement and molybdenite mineralization occurred at c. 420 Ma (that is, the Omey Granite and probably the Inish, Leterfrack and Roundstone granites) to the N and NW of the Skird Rocks Fault, an extension of the orogen-parallel Southern Uplands Fault in western Ireland. A generally southern and eastward progression of granite emplacement (and molybdenite mineralization) sited along the Skird Rocks Fault then followed, at c. 410 Ma (Roundstone Murvey and Carna granites), at c. 400 Ma (Errisbeg Townland Granite, Megacrystic Granite, Mingling Mixing Zone Granodiorite, Lough Lurgan Granite and Kilkieran Murvey Granite) and at c. 380 Ma (Costelloe Murvey Granite, Shannapheasteen and Knock granites). The duration of granite magmatism and mineralization in Connemara is similar to other sectors of the Appalachian–Caledonian orogeny and several tectonic processes (e.g. slab-breakoff, asthenospheric flow, transtension and decompression) may account for the duration and variety of granite magmatism of the western Irish Caledonides.
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Friend, C. R. L., M. Brown, W. T. Perkins, and A. D. M. Burwell. "The geology of the Qôrqut granite complex north of Qôrqut, Godthåbsfjord, southern West Greenland." Bulletin Grønlands Geologiske Undersøgelse 151 (January 1, 1985): 1–43. http://dx.doi.org/10.34194/bullggu.v151.6693.

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The late Archaean (c. 2550 Ma) Qôrqut granite complex post-dates the major part of the geological evolution of the Godthåbsfjord region of southern West Greenland. The complex is composed of a variety of granites intruded as a multitude of individual sheets. The granites are divided into three groups according to their age relations and overall characteristics: leucocratic granites, grey biotite granites, and composite granites. Moreover, the complex can be divided into three zones: upper, intermediate and lower. These zones have different proportions of the three granite groups and included country rocks. Textures and structures typical of partial melting are found in highly modified gneiss enclaves contained in the leucocratic granites of the lower zone. All stages of the transition from gneiss to granite are present. Field evidence suggests that much of the biotite contained in the granites may be derived from the parent gneiss. Petrographic and mineral data are presented to support this contention. In some parts of the complex in the area studied extensive mineral and lithological layering is present. This most commonly occurs in the leucocratic granites and consists of biotite-rich versus biotite-poor granite. Otherwise seams and thin layers of biotite are found which, in part, may be derived from the partially melted enclaves. Lithological layering may also be produced by intrusive effects of thin sheets of granite of slightly different characteristics. Using mesonormative components the granites approximate to minimum melts in the granite system and appear to have crystallised under conditions where PTotal was less than 5 kbar. The melting zone for the leucocratic granites was not far below the present level of exposure. The grey biotite granites were probably derived from slightly deeper levels. The tectonic regime under which the Archaean crust was partially melted allowed small, discrete batches of magma rapid access to higher levels of the crust. Once at this higher level, emplacement was constrained to a sheet form. The complex was thus built up by successive intrusions of small batches of magma.
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Broska, Igor, and Michal Kubiš. "Accessory minerals and evolution of tin-bearing S-type granites in the western segment of the Gemeric Unit (Western Carpathians)." Geologica Carpathica 69, no. 5 (October 1, 2018): 483–97. http://dx.doi.org/10.1515/geoca-2018-0028.

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Abstract The S-type accessory mineral assemblage of zircon, monazite-(Ce), fluorapatite and tourmaline in the cupolas of Permian granites of the Gemeric Unit underwent compositional changes and increased variability and volume due to intensive volatile flux. The extended S-type accessory mineral assemblage in the apical parts of the granite resulted in the formation of rare-metal granites from in-situ differentiation and includes abundant tourmaline, zircon, fluorapatite, monazite-(Ce), Nb–Ta–W minerals (Nb–Ta rutile, ferrocolumbite, manganocolumbite, ixiolite, Nb–Ta ferberite, hübnerite), cassiterite, topaz, molybdenite, arsenopyrite and aluminophosphates. The rare-metal granites from cupolas in the western segment of the Gemeric Unit represent the topaz–zinnwaldite granites, albitites and greisens. Zircon in these evolved rare-metal Li–F granite cupolas shows a larger xenotime-(Y) component and heterogeneous morphology compared to zircons from deeper porphyritic biotite granites. The zircon Zr/Hfwt ratio in deeper rooted porphyritic granite varies from 29 to 45, where in the differentiated upper granites an increase in Hf content results in a Zr/Hfwt ratio of 5. The cheralite component in monazite from porphyritic granites usually does not exceed 12 mol. %, however, highly evolved upper rare-metal granites have monazites with 14 to 20 mol. % and sometimes > 40 mol. % of cheralite. In granite cupolas, pure secondary fluorapatite is generated by exsolution of P from P-rich alkali feldspar and high P and F contents may stabilize aluminophosphates. The biotite granites contain scattered schorlitic tourmaline, while textural late-magmatic tourmaline is more alkali deficient with lower Ca content. The differentiated granites contain also nodular and dendritic tourmaline aggregations. The product of crystallization of volatile-enriched granite cupolas are not only variable in their accessory mineral assemblage that captures high field strength elements, but also in numerous veins in country rocks that often contain cassiterite and tourmaline. Volatile flux is documented by the tetrad effect via patterns of chondrite normalized REEs (T1,3 value 1.46). In situ differentiation and tectonic activity caused multiple intrusive events of fluid-rich magmas rich in incompatible elements, resulting in the formation of rare-metal phases in granite roofs. The emplacement of volatile-enriched magmas into upper crustal conditions was followed by deeper rooted porphyritic magma portion undergoing second boiling and re-melting to form porphyritic granite or granite-porphyry during its ascent.
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Wilson, Reginald A., and Sandra L. Kamo. "Geochronology and lithogeochemistry of granitoid rocks from the central part of the Central plutonic belt, New Brunswick, Canada: implications for Sn-W-Mo exploration." Atlantic Geology 52 (April 29, 2016): 125. http://dx.doi.org/10.4138/atlgeol.2016.007.

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The central part of the Central plutonic belt in New Brunswick is underlain by numerous plutons of calc-alkaline, foliated and unfoliated granite that intrude Cambrian to Early Ordovician metasedimentary rocks. U-Pb (zircon) dating demonstrates that granites range in age from Middle Ordovician to Late Devonian, although most are late Silurian to Early Devonian. An age of 467 ± 7 Ma has been obtained on the foliated McKiel Lake Granite, whereas unfoliated intrusions yield ages of 423.2 ± 3.2 Ma (Bogan Brook Granodiorite), 420.7 +1.8/-2.0 Ma (Nashwaak Granite), 419.0 ± 0.5 Ma (Redstone Mountain Granite), 416.1 ± 0.5 Ma (Beadle Mountain Granite), 415.8 ± 0.3 Ma (Juniper Barren Granite), 409.7 ± 0.5 Ma (Lost Lake Granite), and 380.6 ± 0.3 Ma (Burnthill Granite). All plutons exhibit mixed arc-like and within-plate geochemical signatures, although the Redstone Mountain and Burnthill granites are dominantly of within-plate type. Trace element data reveal a close overall geochemical similarity between Ordovician and Silurian – Devonian plutons, indicating that all were generated by partial melting of the same crustal source. Late Silurian to Early Devonian plutons mainly comprise biotite and/or muscovite-bearing, peraluminous granite and are considered prospective for granophile-element mineralization. All plutons contain Sn well in excess of the granite global average abundance, and several contain average tin values comparable to productive stanniferous granites elsewhere. The Burnthill, Lost Lake, Beadle Mountain, and Nashwaak granites are geochemically most evolved and enriched in Sn and W. The Burnthill Granite in particular has experienced late-stage hydrothermal processes that have resulted in local enrichments of these elements.
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Stone, Maurice. "The Tregonning granite: petrogenesis of Li-mica granites in the Cornubian batholith." Mineralogical Magazine 56, no. 383 (June 1992): 141–55. http://dx.doi.org/10.1180/minmag.1992.056.383.01.

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AbstractLi-mica (zinnwaldite and/or lepidolite)—topaz—albite granites in the Tregonning—Godolphin pluton and similar rocks in the St. Austell pluton appear to be petrogenetically unrelated to the spatially associated biotite granites. Evidence is provided by lack of development of Li-mica granites at roof zones of biotite granites and markedly different trends and composition fields in bivariate plots such as Li vs. Cs, Rb vs. Sr and Nb vs. Zr. Thus, differentiation of biotite granite magma is unlikely to have generated Li-mica granite magma, as also, on its own, is partial melting of biotite granite or biotiteabsent residual lower crust. However, partial melting of biotite-rich residual rocks involving biotite breakdown could yield a trace alkali- and F-enriched melt, although this would require marked femic mineral, K-feldspar and anorthite fractionation, and Na-enrichment. It is proposed that volatiles derwed from either a mantle source or the crust/mantle interface have aided metasomatism of either residual S-type crust that earlier provided S-type biotite granite magma, or basic (biotite-rich) granitoid, to produce a low-temperature, low-viscosity Li-mica granite melt that rose rapidly in the crust soon after the emplacement of associated biotite granites.
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Vonopartis, Leonidas, Paul Nex, Judith Kinnaird, and Laurence Robb. "Evaluating the Changes from Endogranitic Magmatic to Magmatic-Hydrothermal Mineralization: The Zaaiplaats Tin Granites, Bushveld Igneous Complex, South Africa." Minerals 10, no. 4 (April 23, 2020): 379. http://dx.doi.org/10.3390/min10040379.

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The stanniferous granites of the Zaaiplaats Tin Field are part of the A-Type Lebowa Granite Suite, within the greater Bushveld Igneous Complex of northeast South Africa. The tin field comprises three granites: (1) the Nebo, a leucocratic, equigranular biotite granite; (2) The brick-red hypidiomorphic Bobbejaankop granite, which is extensively microclinized with chloritized biotite and characteristic synneusis-textured quartz; and (3) The variably altered roof facies of the Bobbejaankop granite known as the Lease microgranite. The Bobbejaankop and Lease granites were both extensively mined for cassiterite until 1989. The cassiterite is hosted in disseminations, miarolitic cavities, and within large hydrothermal, tourmalinized, and greisenized pipes and lenticular ore-bodies. An extensive petrological and whole-rock XRF and ICP-MS geochemical study, has provided new insight into the magmatic and magmatic-hydrothermal mineralization processes in these granites. Trace elements and Rayleigh Fractionation modelling suggest the sequential fractionation of the Nebo granite magma to be the origin of the Bobbejaankop granite. Incompatible elemental ratios, such as Zr/Hf and Nb/Ta, record the influence of internally derived, F-rich, hydrothermal fluid accumulation within the roof of the Bobbejaankop granite. Thus, the Lease granite resulted from alteration of the partially crystallized Bobbejaankop granite, subsequent to fluid saturation, and the accumulation of a magmatic-hydrothermal, volatile-rich fluid in the granite cupola. The ratio of Nb/Ta, proved effective in distinguishing the magmatic and magmatic-hydrothermal transition within the Bobbejaankop granite. Elemental ratios reveal the differences between pre- and post-fluid saturation in the mineralizing regimes within the same pluton. Thus highlighting the effect that the location and degree of hydrothermal alteration have had on the distribution of endogranitic tin mineralization.
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Grantham, G. H., A. B. Moyes, and D. R. Hunter. "The age, petrogenesis and emplacement of the Dalmatian Granite, H.U. Sverdrupfjella, Dronning Maud Land, Antarctica." Antarctic Science 3, no. 2 (June 1991): 197–204. http://dx.doi.org/10.1017/s0954102091000238.

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The ∼470 Ma Dalmatian Granite forms sheet-like bodies intruded discordantly into orthogneisses, paragneisses and calcareous rocks belonging to the ∼1000 Ma Jutulrora, Sveabreen and Fuglefjellet formations respectively. The Dalmatian Granite is muscovite + biotite bearing. Two varieties are recognized, one that is magnetite-bearing and another that is characterized by tourmaline nodules. At some localities, development of the tourmaline-bearing variety is spatially associated with the presence of carbonates. Physical conditions of emplacement for the Dalmatian Granite are estimated to be approximately 700°C and 6kbar with pH2O = Pload. The emplacement of the granite is considered to have occurred syntectonically during D3 approximately 470 Ma ago. The granites are therefore similar in age to Pan African age granites in Mozambique as well as Ross Orogeny age granites in the Transantarctic Mountains.
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Imeokparia, E. G. "Geochemical evolution of the Jarawa Younger Granite complex and its related mineralization, northern Nigeria." Geological Magazine 122, no. 2 (March 1985): 163–73. http://dx.doi.org/10.1017/s0016756800031071.

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AbstractThe Jarawa Younger Granite complex is composed of high silica alkali granites that were emplaced 161 Ma ago. The granites are characterized by high contents of Rb, Li, F, Sn, Nb, W above normal low-Ca granitic rocks and have typical S-type characteristics that are indicative of a substantial component of crustal melt.Mineralization in the complex is associated with the biotite granite which was emplaced as a sheet-like body at relatively shallow depth and occurs as disseminations and as greisen lodes and veins.Chemical studies of the granites have shown that the biotite granite represents a highly fractionated rock that crystallized from a residual magma from which the hornblende-biotite granite had previously crystallized. However the biotite granite is characterized by steep gradients in some minor and trace elements that apparently indicate that liquid-state differentiation and/or volatile complexing processes made significant contributions to their differentiation. Enrichment of Th, Li, Rb, Sn, W and Nb may be more closely linked to roofward migration of F.
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Dissertations / Theses on the topic "Granirer"

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Villaros, Arnaud. "Petrogenesis of S-type granites : the example of the Cape Granite Suite." Thesis, Stellenbosch : University of Stellenbosch, 2010. http://hdl.handle.net/10019.1/4015.

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Thesis (PhD (Earth Sciences))--University of Stellenbosch, 2010.
ENGLISH SUMMARY: S-type granite intrusions are extremely common in the continental crust and form from the partial melting of metasediments. Compositions of S-type granite range from leucogranite to granodiorite and have trace element contents that globally increase with increasing maficity (Fe + Mg). Models proposed for the formation of S-type granite do not answer satisfactorily all petrological and compositional requirements. In this study, S-type granite of the Cape Granite Suite (CGS), South Africa is used to discriminate between potential sources of compositional variation. Experimental studies show that melt produced from the partial melting of sediment is exclusively leucocratic. On this basis, the entrainment of up to 20 wt.% of peritectic garnet within S-type melt can be established to produce the observed major element variations. S-type CGS locally contains garnet. This garnet is in equilibrium with granite composition at P-T conditions (5kb and 750 C for the core of the garnet and 3kb and 720 C for the rim) well below conditions recorded by xenoliths from the same granite (10 kb and 850 C from a metabasite). From this result it seems that the originally entrained garnet no longer exists in the Stype CGS and it have been replaced by newly formed minerals (garnet, cordierite and biotite). Considering the short time necessary to emplace granites (about 100 000 years), it appears that garnet has been compositionnally re-equilibrated through a dissolution-precipitation process. The study of trace element variations in S-type CGS shows that most leucocratic compositions are undersaturated in Zr and Ce compared to predictions from experimental models for dissolution of accessory zircon and monazite in their source regions. Thus, S-type melts are likely to be formed in disequilibrium with respect to accessory phase stability. As a result the observed increase in trace element content with increasing maficity indicates that accessory minerals such as zircon and monazite are co-entrained with peritectic garnet in melt to produce the observed trace element variation in S-type granite. Trace element disequilibrium in the CGS S-type granitoids requires particularly short times of residence of melt within the source region. Together, these results provide for the first time, a fully comprehensive model for major and trace elements variations. Compositional variation in CGS S-type granite results from source processes by a selective entrainment of peritectic and accessory minerals. After entrainment, these minerals are likely to be re-equilibrated within the magma, through a dissolution-reprecipitation process. In addition, it appears that the construction of large S-type granitic bodies occurs through successive addition of magma batches of different composition that originates directly from the source region.
AFRIKAANSE OPSOMMING: S-tipe granietinstrusies is baie algemeen in die kontinentale kors en vorm deur die gedeeltelike smelting van metasedimente. Samestellings van S-tipe graniete strek vanaf leukograniet tot granodioriet en het spoorelementsamestellings wat global toeneem met ’n toenemende mafiese component (Fe + Mg). Modelle wat voorgestel is vir die formasie van S-tipe graniete beantwoord nie bevredigend al die petrologiese en komposisionele benodigdhede nie. In hierdie studie word S-tipe graniete van die Kaapse Graniet Suite (CGS), Suid Afrika, gebruik om te diskrimineer tussen potensiele bronne van komposisionele variasie. Eksperimentele studies wys dat smelt, geproduseer van die gedeeltelike smelting van sedimente, uitsluitlik leukokraties is. Op hierdie basis kan bewys word, dat die optel-en-meevoering van tot 20 wt% van peritektiese granaat in S-tipe smelt, die waargeneemde hoofelement variasies kan produseer. S-tipe CGS bevat lokale granaat. Hierdie granaat is in ekwilibrium met die graniet samestelling by P-T kondisies (5kb en 750circC vir die kern van die granaat en 3kb en 720circC vir die rand) ver onder kondisies waargeneem by xenoliete van dieselfde granite (10kb en 850circC van ’n metabasiet). Van hierdie resultaat kan afgelei word dat die oorspronklike opgetel-en-meegevoerde graniet bestaan nie meer in die S-tipe CGS en dat dit vervang is deur nuutgevormde minerale (granaat, kordieriet en biotiet). As in ag geneem word die kort tyd wat nodig is om graniete in te plaas (omtrent 100 000 jaar), wil dit voorkom dat granaat se samestelling geherekwilibreer word deur ’n oplossings-presipitasie proses. Die studie van spoorelement variasies in S-tipe CGS wys dat meeste leukokratiese samestellings is onderversadig in Zr en Ce in vergelyking met voorspellings deur eksperimentele modelle vir die oplossing van bykomstige zircon en monasiet in hulle brongebiede. Dus is S-tipe smelte meer geneig om gevorm te word in disekwilibrium in verhouding tot bykomstige mineraalstabilileit. Met die gevolg is dat die waargenome toename in spoorelementinhoud met toename in mafiese component wys dat bykomstige minerale, soos zirkoon en monasiet, word saam opgetel-enmeegevoer met peritektiese granaat in smelt om die waargenome spoorelement variasie in S-tipe graniete te verklaar. Spoorelement disekwilibrium in die CGS S-tipe granitoide benodig veral kort tye van residensie van die smelt binne die brongebied. Saam gee hierdie resultate vir die eerste keer ’n algehele antwoord vir hoof- en spoorelement variasies. Variasie in samestelling in CGS S-tipe graniete is die resultaat van bronprosesse deur ’n selektiewe optel-en-meevoer van peritektiese en bykomstige minerale. Na die optel-en-meevoer van hierdie minerale word hulle geherekwilibreer binne die magma deur ’n oplossings-presipitasie proses. Addisioneel wil dit voorkom of die konstruksie van groot S-tipe granietliggame plaasvind deur opeenvolgende toevoegings van magma lotte van verskillende samestellings wat direk uit die brongebied kom.
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Bland, A. M. "The geology of the granites of Western Jersey, with particular reference to the south-west granite complex." Thesis, Oxford Brookes University, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.355623.

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Riley, Dean Nolan. "Granites, orogeny, and the deblois pluton complex in Eastern Maine, USA." Connect to this title online, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1087232113.

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Thesis (Ph. D.)--Ohio State University, 2004.
Title from first page of PDF file. Document formatted into pages; contains xliv, 546 p.; also includes graphics. Includes bibliographical references (p. 517-546).
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Klimm, Kevin. "Differentiation and crystallisation processes in A-type granites an experimental study of the Wangrah Suite, Australia = Differenzierungs- und Kristallisationsprozesse in A-Typ-Graniten /." [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=972117229.

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Griffault, Lise. "Bilan des transferts de matière (majeurs et terres rares) dans les altérations hydrothermales des granites : exemple du granite du ballon d'alsace (vosges méridionales)." Poitiers, 1987. http://www.theses.fr/1987POIT2302.

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Etude de deux systemes d'alteration hydrothermale: - une alteration pervasive, se manifestant par la chloritisation des ferromagnesiens, le formation d'illite dans les plagioclases et la cristallisation de calcite; - une alteration a illite dans les epontes de veines liees a la mise en place de filins de fluorine. Cette etude montre que le comportement geochimique des terres rares ne peut etre assimile au comportement des elements majeurs au cours des processus hydrothermaux ou des mineraux argileux sont formes. Les mecanismes de fixation des terres rares correspondent a des phenomenes de sorption des elements sur les surfaces des particules argileuses et non a des substitutions
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Mouraouah, Az-El-Arab el. "Palingenèse du granite du Velay autour de la diorite du Peyron (Burzet, Ardèche, M.C.F.) approche pétrographique et géochimique de la genèse des granites tardimigmatitiques." Grenoble 2 : ANRT, 1986. http://catalogue.bnf.fr/ark:/12148/cb375999372.

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Griffault, Lise. "Bilan des transferts de matière (majeurs et terres rares) au cours des altérations hydrothermales des granites exemple du granite du Ballon d'Alsace, Vosges méridionales /." Grenoble 2 : ANRT, 1987. http://catalogue.bnf.fr/ark:/12148/cb37605587v.

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Flatley, Kerin. "Granite Butterfly." Digital Archive @ GSU, 2009. http://digitalarchive.gsu.edu/english_diss/45.

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ABSTRACT Granite Butterfly is a novel about three women—grandmother, mother, and daughter—and the unusual attachments that break apart their family. Tuula Laine is a Rockport, Massachusetts, native of Finnish descent, whose parents moved to Cape Ann for work in the area’s granite quarries. Her life changes one afternoon when her son Henri, a brilliant surgeon who has never seriously dated anyone before, visits with his pregnant girlfriend, Coreen. Tuula immediately senses that Coreen not the right match for him in terms of age, education, or temperament, and as the couple separates and unites over the course of one summer, Tuula witnesses, for the first time, the pattern of desire and abandonment that will define their relationship. By the time Tuula’s granddaughter, Suvi, is fourteen years old, she, too, has established a destructive relationship pattern with Coreen: whenever Coreen and Henri separate, Suvi’s mother clings to her until they develop a bond closer to that of sisters than a mother and child. In the final movement of the novel, this bond, and the bond between Suvi’s parents, is finally put to the test. Granite is cut into precise blocks—dynamite is never used, lest it shatter the stone. In a few short weeks, the Laine family is pulled apart, but unlike with quarrying, there is no way to divide them in a careful manner, no way to detach them that isn’t violent and abrupt, no way to predict, or guide, where they will split.
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El, Mouraouah Az El Arab. "Palingenèse du granite du Velay autour de la diorite du Peyron (Burzet, Ardèche, M. C. F. ) : approche pétrographique et géochimique de la genèse des granites tardimigmatitiques." Clermont-Ferrand 2, 1986. http://www.theses.fr/1986CLF21030.

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Le massif dioritique du Peyron s'est mis en place à l'état magmatique dans le granite du Velay. L'intrusion basique a induit une fusion partielle du granite du Velay. Interactions chimiques a l'interface granite-diorite par thermodiffusion. Les enclaves microgrenues sombres de taille importante résultent d'un vrai mélange avec proportion variable de granite et de diorite. Les granites tardimigmatitiques liés au granite du Velay présentent des analogies pétrographiques et géochimiques avec le granite refondu du Peyron.
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Sérvulo, Ana Cláudia Oliveira. "Método de Granier e transpiração do mogno africano." Universidade Federal de Goiás, 2016. http://repositorio.bc.ufg.br/tede/handle/tede/6222.

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The African Mahogany’s commercial exploitation in the Brazilian Midwest lacks information to assist management strategies of the specie and natural resources, specially water. The transpiration and growth analysis are useful, not just for water management, but also to support physiological studies. The Granier method (thermal dissipation probe – TDP) uses sap flow measurements to estimate transpiration in woody species, however it requires validate for each new specie. This paper aimed to study the African Mahogany’s water consumption and growth in the Cerrado bioma. The main activities aimed to: a) Adjust the Granier’s sap flux method to African Mahogany; b) Quantify water consumption and vegetative growth on a 2.5 years old African Mahogany’s forest, under two water regimes; c) Establish relations between tree transpiration and atmospheric water demand. This research consisted of two experiments. The first one, happened in oct-nov/2014 and feb-may/2015, consisted of the Granier’s model adjustment with aid of the lysimetry, for use in African Mahogany’s transpiration measurements. The second experiment, happened between oct/2014 and oct/2015, on a commercial forest up to 2.5 years old, evaluated water consumption (transpiration by leaf area – T) using integrated sap flux measurements by TDP, and vegetative growth [leaf area (AF), diameter at breast height (DAP), tree height (Alt), trunk volume (VTR) and leaf dry biomass (BMF)], treatments were defined as: T1 – forest with irrigation interrupted at two years old; T2 – forest without irrigation. The adjusted sap flux model to African mahogany is F    k  AS 6 1,231 268,25 10 , and the original Granier’s model underestimates the transpiration in 39.1%. The average potential transpiration was between 2.1 and 34.8 L day-1. In field conditions, the growth benefits from the T1 are seen in highest values for AF, DAP and BMF. However, the Alt and VTR are not significant different. The monthly T under field conditions varied between 10.2 and 24.2 L m-2, except for jul-aug/2015, when T2 transpiration was higher. The combination of bigger leaf area and low soil water content led to T1’s water deficit scenario.
A exploração comercial do Mogno Africano (Khaya ivorensis) no Centro- Oeste brasileiro carece de informações sobre a espécie para auxiliar no desenvolvimento de estratégias de ações no manejo da espécie e dos recursos naturais, em especial a água. Para tal, os estudos do processo transpiratório e de análise de crescimento são úteis, não só para o manejo da água no processo produtivo, como também para sustentar estudos fisiológicos. O método de Granier (sonda de dissipação térmica – SDT) utiliza a medida do fluxo de seiva como base para estimativa da transpiração em espécies lenhosas, todavia seu uso requer validação do modelo para cada nova espécie. Este trabalho tem como objetivo determinar consumo hídrico e o crescimento do Mogno Africano no bioma Cerrado. As atividades envolvidas visaram: a) Ajustar o modelo de Granier para estimativa da transpiração em Mogno Africano; b) Quantificar o consumo de água e o crescimento vegetativo em uma floresta a partir dos 2,5 anos de idade em dois regimes hídricos; c) Estabelecer a relação entre a transpiração das árvores e a demanda hídrica da atmosfera em condições naturais de disponibilidade de água no solo. A pesquisa constituiu de dois experimentos. O primeiro experimento foi realizado entre out-nov/2014 e fev-mai/2015 e objetivou o ajuste do modelo de Granier a partir da lisimetria na medida da transpiração do Mogno Africano. O segundo experimento foi realizado a campo entre out/2014 e out/2015, em um plantio comercial a partir de 2,5 anos de idade, avaliou-se o consumo hídrico (transpiração por unidade de área foliar – T), por meio da integração do fluxo de seiva medido com a SDT, e o crescimento vegetativo [área foliar (AF), diâmetro à altura do peito (DAP), altura (Alt), volume de tronco (VTR) e biomassa seca de folhas (BMF)]; os tratamentos foram definidos como: T1 – floresta com irrigação interrompida aos dois anos; T2 – floresta não irrigada. O modelo ajustado para o Mogno Africano é F    k  AS 6 1,231 268,25 10 . O modelo original de Granier subestima em 39,1% a transpiração do Mogno Africano. A transpiração potencial média foi de 13,0 L dia-1. Em campo, a superioridade do crescimento em AF, DAP e BMF prevaleceu para o tratamento T1. Porém o incremento em Alt e VTR foi similar nos dois grupos avaliados. A T em campo variou entre 10,2 e 24,2 L m-2 mês-1, respondendo diretamente à demanda evaporativa atmosférica, exceto em jul e ago/2015, nos quais T2 apresentou maior T. A combinação entre maior área foliar e baixo armazenamento de água no solo (a partir de 33,6 mm) promoveu menor transpiração à T1 devido ao esgotamento precoce da água do solo.
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Books on the topic "Granirer"

1

Lindberg, E. Theodore. Pnina Granirer: Portrait of an artist. Vancouver, B.C: Ronsdale, 1998.

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Granice, granice: Studije i ogledi. Pula: Istarski ogranak Društva Hrvatskih Književnika, 2007.

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Pužar, Aljoša. Granice, granice: Studije i ogledi. Pula: Istarski ogranak Društva Hrvatskih Književnika, 2007.

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Bray, E. A. Du. Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia. Washington: U.S. G.P.O., 1988.

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Bray, E. A. Du. Geology of the Silsilah ring complex and associated tin mineralization, Kingdom of Saudi Arabia. Washington, DC: Dept. of the Interior, 1988.

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Barbara, Korzon, ed. Granice uczuć. Katowice: Ksia̜żnica, 2004.

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Mitchell, James Leslie. Grey granite. Edinburgh: Canongate Pub., 1990.

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Archer, Michael. Granite sculpture. Nottingham: Nottingham Castle Museum, 1990.

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Skarga, Barbara. Granice historycznosci. Warszawa: Państwowy Instytut Wydawniczy, 1989.

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ill, Hawkes Kevin, ed. Granite baby. New York: Farrar, Straus and Giroux, 2005.

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Book chapters on the topic "Granirer"

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Stevenson, David S. "Our Planet’s Torrid Heart." In Granite Skyscrapers, 1–31. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_1.

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Stevenson, David S. "The Formation of Granites & Plate Tectonics." In Granite Skyscrapers, 32–82. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_2.

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Stevenson, David S. "The Evolution of Modern Continents." In Granite Skyscrapers, 83–154. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_3.

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Stevenson, David S. "Plate Tectonics, Planetary Magnetism and Life." In Granite Skyscrapers, 155–92. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_4.

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Stevenson, David S. "Jotunheim –In the Realm of Giants." In Granite Skyscrapers, 193–250. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_5.

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Stevenson, David S. "Mountains, Atmosphere and Long-Term Habitability." In Granite Skyscrapers, 251–86. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_6.

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Stevenson, David S. "Our Island Earth: Granite Here, Granite Everywhere?" In Granite Skyscrapers, 287–337. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_7.

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Stevenson, David S. "Exoplanets, Granitoids and Evolutionary Potential." In Granite Skyscrapers, 338–64. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-91503-6_8.

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Arndt, Nicholas. "Granite." In Encyclopedia of Astrobiology, 999. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_665.

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Arndt, Nicholas. "Granite." In Encyclopedia of Astrobiology, 1. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_665-3.

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Conference papers on the topic "Granirer"

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Mouroux, B., T. Merceron, D. Vilogeux, and J. de Me`redieu. "The Disposal of HLLL Waste in a Granitic Formation: The Status of Research in France." In ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4818.

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In accordance with the French Law of 1991 December 30, Andra is preparing a report on the possibilities of geological disposal to be submitted in 2005. For that purpose, a research programme has been launched to assess the suitability of granite geological formations for the implementation of a high-level long-lived radioactive waste repository. The programme relies mainly on Andra’s participation in experiments in Swedish, Swiss and Canadian underground research laboratories. The main issues under investigation include granite fracturing and the behaviour of engineered barriers. Furthermore, a typological analysis of French granites provides an opportunity to apply results to the French geological context. Advances in knowledge afford a better understanding of the phenomena relating to granite and preliminary repository designs. They constitute the basis for design studies and safety analyses to be conducted before 2005.
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Stevenson, Alexandria M., and Jonathan D. Price. "ANOMALOUS GRANITES WITHIN THE QUANAH GRANITE PLUTON, WICHITA MOUNTAINS, OKLAHOMA." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343875.

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René, Miloš. "Nb-Ta-Ti oxides in topaz granites of the Geyer granite stock (Erzgebirge Mts., Germany)." In The 1st International Electronic Conference on Mineral Science. Basel, Switzerland: MDPI, 2018. http://dx.doi.org/10.3390/iecms2018-05448.

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Stevenson, Alexandria M., and Jonathan D. Price. "IT’S COMPLICATED: FINE AND PORPHYRITIC GRANITES ASSOCIATED WITH THE COARSE-GRAINED QUANAH GRANITE, SOUTHWESTERN OKLAHOMA, USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-322860.

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Moecher, David P., Samantha R. Burk, and Scott D. Samson. "TESTING THE “HOT GRANITE” HYPOTHESIS FOR HIGH-ZR GRENVILLE GRANITES FROM EASTERN LAURENTIA USING ZIRCON THERMOMETERS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305927.

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RAVICHANDRAN, Lenin, Dmitrijs RUSOVS, Thottipalayam Vellingri ARJUNAN, Selvaraj VIJAYAN, and Murugesan MATHESWARAN. "EXPERIMENTAL STUDY OF BRACKISH WATER DISTILLATION IN SINGLE SLOPE SOLAR STILL USING SENSIBLE HEAT STORAGE MATERIALS." In RURAL DEVELOPMENT. Aleksandras Stulginskis University, 2018. http://dx.doi.org/10.15544/rd.2017.086.

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Solar distillation is one of the important methods of getting clean water from brackish and seawater using the renewable energy of the sun. The passive type solar still represent most economical method to supply drinking water for domestic applications for decentralized level. Experimental measurements of solar distillation productivity for single slope still were conducted at the testing field of the Mechanical Engineering department, Coimbatore Institute of Engineering and Technology, Coimbatore, Tamilnadu, India. The influence of basin water quantity and amount of energy storage materials are examined and the performance is compared. The target of this research is to find best way to keep the excess heat by energy storage materials and release it during off-sunshine hours for increment in distillate output and efficiency. Various sensible heat energy storage materials like pebbles, blue metal stone, red brick, granites and white marbles were used as energy storage medium. The daily yield of black granite still is higher than other energy storage material stills and is equal to 3.216 kg/day/m2, which is 29% higher than that of the still without energy storage materials.
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Arbain, Azizi, Mohd Hafiz Zawawi, Mohd Rashid Mohd Radzi, Nurul Husna Hassan, and Ahmad Zhafran Ahmad Mazlan. "Natural frequencies comparison between the pure granite and bonded granite-concrete." In PROCEEDINGS OF GREEN DESIGN AND MANUFACTURE 2020. AIP Publishing, 2021. http://dx.doi.org/10.1063/5.0044239.

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Sun, Weizhao, Zhongfan Wang, Yaliang Xia, Gang Chen, and Suhong Zhang. "Application of Fracture Prediction Research Based on OVT Gather in Granite Buried Hills." In International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21500-ms.

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Abstract The space of fracture reservoir in granite buried hills varies sharply with strong heterogeneity and very difficult to predict. Conventional fracture prediction methods based on narrow-azimuth post-stack seismic data have low prediction accuracy. OVT pre-stack gather retains the information of offset and azimuth, reflects the anisotropic characteristics of fractures and can be effectively used to predict the strength and strike of fracture in granite buried hills. In this paper, based on the analysis of anisotropy of OVT gather data, according to the geological characteristics of granite fractures, optimizes the sensitive offset and azimuth OVT gather data, uses the P-wave azimuth anisotropy technique to predict the strength and strike of fractures. The prediction coincides well with the drilling results, which can provide an important guidance for the exploration and development of granite buried hill in the research area.
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Newcomb, Sally. "THE CONTROVERSIAL GRANITE CONTROVERSY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334628.

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Kirkpatrick, Heather, Mark Harrison, Ming-Chang Liu, Elizabeth Bell, Francois L. H. Tissot, and Mauricio Ibañez-Mejia. "δ94/90Zr Variations in Granites." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1325.

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Reports on the topic "Granirer"

1

Burns, L. E., K. J. Johnson, and R. J. Newberry. Discriminant function for separating tin from non-tin granites: application to the Hope Granite Suite, eastern interior Alaska. Alaska Division of Geological & Geophysical Surveys, 1988. http://dx.doi.org/10.14509/1361.

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Susskind, Lawrence E., Susan L. Podziba, and Eileen Babbitt. Granite Construction Co. Fort Belvoir, VA: Defense Technical Information Center, August 1989. http://dx.doi.org/10.21236/ada225177.

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Petkovic, Peter. Gravity and granites : technical notes on mapping relationships of known granites and gravity. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.012.

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Whalen, J. B. A-Type Granites in New Brunswick. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120384.

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Swaja, R. E., and W. D. Cottrell. Results of the radiological survey at the Granite City Steel facility, Granite City, Illinois. Office of Scientific and Technical Information (OSTI), July 1990. http://dx.doi.org/10.2172/6605990.

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Buettner, Edwin W., and V. Lance Nelson. Smolt Monitoring at the Head of Granite Reservoir and Lower Granite Dam, 1989 Annual Report. Office of Scientific and Technical Information (OSTI), April 1990. http://dx.doi.org/10.2172/6854896.

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Whalen, J. B., K. L. Currie, and B. W. Chappell. A-Type Granites: Descriptive and Geochemical Data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/130214.

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Bedrossian, P. Neutrons and Granite: Transport and Activation. Office of Scientific and Technical Information (OSTI), April 2004. http://dx.doi.org/10.2172/15009828.

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Jackson, L. E. Surficial geology, Granite Canyon, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208953.

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Buettner, Edwin W., and Arnold F. Brimmer. Smolt Monitoring at the Head of Lower Granite Reservoir and Lower Granite Dam, 1995 Annual Report. Office of Scientific and Technical Information (OSTI), October 1996. http://dx.doi.org/10.2172/441714.

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