Relevant bibliographies by topics / Restite

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Restite'

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

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Journal articles on the topic "Restite"

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Zeck, H. P. "Restite-melt and mafic-felsic magma mixing and mingling in an S-type dacite, Cerro del Hoyazo, southeastern Spain." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 139–44. http://dx.doi.org/10.1017/s0263593300007823.

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ABSTRACTApproximately 10-15 vol% of the Neogene Hoyazo dacite consists of Al-rich restite rock inclusions (A12O3 = 20–45%) and monocrystal inclusions derived therefrom. Restite material and dacitic melt were formed syngenetically from a (semi-)pelitic rock sequence by means of anatexis. Restite rock fragments and dacite show similar high δ18O values (13–16‰) corresponding to those found for sedimentary material. Striking monocrystal restite inclusions in the dacite rock are graphite crystals measuring a few hundred μm, 0.5–10 mm blue cordierite crystals and 2–10 mm ruby red crystals of almandine-rich garnet (1.1 ± 0.2 vol%). Although the almandine crystals are perfectly euhedral, they are identical in every respect to the crystals found in the Al-rich restite rock inclusions and cannot be crystallisation products of the magmatic melt. The dacite also contains many inclusions of quartz gabbroic and basaltoid material which contains inclusions identical to the restite material found in the dacitic glass base. Many basaltoid inclusions show well-developed chilled borders. These inclusions may represent a more mafic magma of deeper origin which mixed with some dacite magma before mingling into it.
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Wyborn, D., and B. W. Chappell. "The petrogenetic significance of chemically related plutonic and volcanic rock units." Geological Magazine 123, no. 6 (November 1986): 619–28. http://dx.doi.org/10.1017/s0016756800024134.

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AbstractComagmatic granitic and volcanic rocks are divided into two types depending on whether or not the primary magma contains restite crystals. Examples of both of these types are discussed from the Lachlan Fold Belt of southeastern Australia.Volcanic rocks containing restite phenocrysts are chemically identical to the associated plutonic rocks containing the same amount of restite. The more mafic granitic rocks correspond in composition to the most phenocryst-rich volcanics (up to 60% phenocrysts), and thus cannot be cumulate rocks produced by fractional crystallization, but must represent true magma compositions. These restite-bearing magmas result from partial melting in a source region up to the rheological critical melt percentage, which we estimate to be about 40% in the S-type Hawkins Suite of volcanics.Melts which escape their restite at the source, before the critical melt percentage is reached, are able to undergo fractional crystallization in high level magma chambers by heterogeneous crystallization on chamber walls. In this case volcanic products from the top of the chamber are more felsic than the plutonic products, the plutonics are crystal cumulates and the volcanics are composed of the complementary fractionated liquid. Those phenocrysts present in the volcanics were probably eroded from the chamber walls and are less abundant (< 20%) than in the restite-retentive volcanic products.
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White, A. J. R. "Water, restite and granite mineralisation." Australian Journal of Earth Sciences 48, no. 4 (August 2001): 551–55. http://dx.doi.org/10.1046/j.1440-0952.2001.00878.x.

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Matrosova, E. А., А. А. Bendeliani, A. V. Bobrov, A. A. Kargal’tsev, and Yu A. Ignat’ev. "Phase relations in the model pyrolite at 2.5, 3.0, 7.0 GPа and 1400–1800°c: evidence for the formation of high-chromium garnets." Геохимия 64, no. 9 (September 20, 2019): 974–85. http://dx.doi.org/10.31857/s0016-7525649974-985.

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Based on study of partial melting in the model pyrolite, it is shown that garnets synthesized at 7.0 GPa in a temperature range of 1400–1800°C are characterized by an excessive Si content (in relation to 3 f.u.), stable admixture of Cr2O3, and, thus, represent a solid solution of the pyrope–majorite–knorringite composition. Increase in the Cr/Al value in the starting composition results in increase of this ratio in garnet. With increasing temperature, the concentration of Cr2O3 decreases in restite and increases in melt. Cr/Al increases in all garnets from the zone of restite and from the quenched melt aggregate. Estimates of the bulk compositions of restite formed by partial melting of the model pyrolite at 2.5 and 3.0 GPa show that the concentration of Cr in it is higher than that in the starting composition. All minerals from the zone of restite are characterized by the high Cr concentrations, and upon partial melting in the spinel-depth facies, Cr is redistributed to restite. Our results show that the formation of high-chromium garnets relates to the protolith with the high Cr/Al value formed as a residue from partial melting in the spinel-depth facies and further transported to the garnet facies.
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Chappell, B. W. "Compositional variation within granite suites of the Lachlan Fold Belt: its causes and implications for the physical state of granite magma." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 159–70. http://dx.doi.org/10.1017/s026359330000657x.

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ABSTRACT:Granites within suites share compositional properties that reflect features of their source rocks. Variation within suites results dominantly from crystal fractionation, either of restite crystals entrained from the source, or by the fractional crystallisation of precipitated crystals. At least in the Lachlan Fold Belt, the processes of magma mixing, assimilation or hydrothermal alteration were insignificant in producing the major compositional variations within suites. Fractional crystallisation produced the complete variation in only one significant group of rocks of that area, the relatively high temperature Boggy Plain Supersuite. Modelling of Sr, Ba and Rb variations in the I-type Glenbog and Moruya suites and the S-type Bullenbalong Suite shows that variation within those suites cannot be the result of fractional crystallisation, but can be readily accounted for by restite fractionation. Direct evidence for the dominance of restite fractionation includes the close chemical equivalence of some plutonic and volcanic rocks, the presence of plagioclase cores that were not derived from a mingled mafic component, and the occurrence of older cores in many zircon crystals. In the Lachlan Fold Belt, granite suites typically evolved through a protracted phase of restite fractionation, with a brief episode of fractional crystallisation sometimes evident in the most felsic rocks. Evolution of the S-type Koetong Suite passed at about 69% SiO2 from a stage dominated by restite separation to one of fractional crystallisation. Other suites exist where felsic rocks evolved in the same way, but the more mafic rocks are absent. In terranes in which tonalitic rocks formed at high temperatures are more common, fractional crystallisation would be a more important process than was the case for the Lachlan Fold Belt.
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Burnham, C. Wayne. "Calculated melt and restite compositions of some Australian granites." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 387–97. http://dx.doi.org/10.1017/s0263593300008051.

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ABSTRACTThe thermodynamic relations embodied in the Quasicrystalline Model of Burnham and Nekvasil (1986), as recently extended by the author, have been used to quantitatively assess the feldspar-quartz liquidus relations in two I-type (Jindabyne and Moruya) and two S-type (Bullenbalong and Dalgety) suites of Australian granites, using analytical data provided by B. W. Chappell and co-workers. Among the more notable results obtained from these calculations at a constant pressure of 5·0kbar and = 0·30 (≍2·8 wt% H2O), for purposes of comparison, are that: (1) felsic melts of remarkably uniform, but distinctive composition can be extracted from each suite, leaving solid residues in amounts up to 65 mol%; (2) all melts from both S-type suites have two feldspars plus quartz on their liquidii, whereas both I-type suites have only plagioclase plus quartz on their liquidii; (3) the total solid residue ranges from 27-63% in the Jindabyne suite, from 15–62% in the Moruya suite, from 30–65% in the Bullenbalong suite, and from 27–65% in the Dalgety suite; (4) liquidus temperatures of the S-type Bullenbalong and Dalgety melts are similar (856° and 860°C), reflecting similar feldspar compositions of An53, Or75 and An60, Or77, respectively; (5) liquidus temperatures of the I-type Jindabyne and Moruya melts, however, are distinctly different (950° and 894°C), reflecting correspondingly different plagioclase compositions of An80 and An52; (6) the calculated liquidus plagioclase composition throughout a given suite is very uniform (±1%) and amounts to as much as 46% of the total rock; and (7) these calculated liquidus and residual plagioclase compositions are also the same, within the uncertainty of measurement, as those of the plagioclase crystal-cores determined optically by A. J. R. White. The only plausible explanation for this remarkable consanguinity in plagioclase liquidus, residue, and crystal-core compositions, hence liquidus temperatures, is that the bulk of the residue is restite, in accordance with the model of White and Chappell (1977). This explanation is corroborated by the very systematic variations in the amounts of individual restite minerals with respect to total restite contents. Accordingly, those members of each suite that contain more than 60% total restite probably closely represent the bulk composition of the source rock, which is dioritic or andesitic for the Jindabyne suite, tonalitic or dacitic for the Moruya suite, pelitic metagreywacke for the Bullenbalong suite, and feldspathic metagreywacke for the Dalgety suite. As a corollary, those members with less than 60% restite must have undergone melt-restite segregation (unmixing), probably during ascent and emplacement.
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Barbero, L., and C. Villaseca. "The Layos Granite, Hercynian Complex of Toledo (Spain): an example of parautochthonous restite-rich granite in a granulitic area." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 127–38. http://dx.doi.org/10.1017/s0263593300007811.

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ABSTRACTThe Layos Granite forms elongated massifs within the Toledo Complex of central Spain. It is late-tectonic with respect to the F2 regional phase and simultaneous with the metamorphic peak of the region, which reached a maximum temperature of 800–850°C and pressures of 400–600 MPa. Field studies indicate that this intrusion belongs to the “regional migmatite terrane granite” type. This granite is typically interlayered with sill-like veins and elongated bodies of cordierite/garnet-bearing leucogranites. Enclaves are widespread and comprise restitic types (quartz lumps, biotite, cordierite and sillimanite-rich enclaves) and refractory metamorphic country-rocks including orthogneisses, amphibolites, quartzites, conglomerates and calc-silicate rocks.These granites vary from quartz-rich tonalites to melamonzogranites and define a S-type trend on a QAP plot. Cordierite and biotite are the mafic phases of the rocks. The particularly high percentage of cordierite (10%–30%) varies inversely with the silica content. Sillimanite is a common accessory mineral, always included in cordierite, suggesting a restitic origin. The mineral chemistry of the Layos Granite is similar to that of the leucogranites and country-rock peraluminous granulites (kinzigites), indicating a close approach to equilibrium. The uniform composition of plagioclase (An25), the high albitic content of the K-feldspar, the continuous variation in the Fe/Mg ratios of the mafic minerals, and the high Ti content of the biotites (2.5–6.5%) suggest a genetic relationship.Geochemically, the Layos Granite is strongly peraluminous. Normative corundum lies between 4% and 10% and varies inversely with increase in SiO2. The CaO content is typically low (<1.25%) and shows little variation; similarly the LILE show a limited range. On many variation diagrams, linear trends from peraluminous granulites to the Layos Granite and associated leucogranite can be observed. The chemical characteristics argue against an igneous fractionation or fusion mechanism for the diversification of the Layos Granite. A restite unmixing model between a granulitic pole (represented by the granulites of the Toledo Complex) and a minimum melt (leucogranites) could explain the main chemical variation of the Layos Granite. Melting of a pelitic protolith under anhydrous conditions (biotite dehydration melting) could lead to minimum-temperature melt compositions and a strongly peraluminous residuum.For the most mafic granites (61–63% SiO2), it is estimated that the trapped restite component must have been around 65%. This high proportion of restite is close to the estimated rheological critical melt fraction, but field evidence suggests that this critical value has been exceeded. This high restite component implies high viscosity of the melt which, together with the anhydrous assemblage of the Layos Granite and the associated leucogranites, indicates H2O-undersaturated melting conditions. Under such conditions, the high viscosity magma (crystal-liquid mush) had a restricted movement capacity, leading to the development of parautochthonous plutonic bodies.
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CHAPPELL, B. W., A. J. R. WHITE, and D. WYBORN. "The Importance of Residual Source Material (Restite) in Granite Petrogenesis." Journal of Petrology 28, no. 6 (December 1, 1987): 1111–38. http://dx.doi.org/10.1093/petrology/28.6.1111.

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Wolf, Michael B., and Peter J. Wyllie. "Garnet Growth during Amphibolite Anatexis: Implications of a Garnetiferous Restite." Journal of Geology 101, no. 3 (May 1993): 357–73. http://dx.doi.org/10.1086/648229.

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Jumaniyozov, D. I., A. M. Musayev, and S. Y. Nematullayev. "Geochemical Criteria Of Ore Content Of Metasomatites Of The Urtalik Deposit (North Nuratau)." American Journal of Social Science and Education Innovations 2, no. 09 (September 10, 2020): 79–100. http://dx.doi.org/10.37547/tajssei/volume02issue09-12.

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On the studied site of the Urtalik ore deposit, rare, rare-earth and polymetallic mineralization is shown. Rare elements zirconium and niobium can have restite character which gets a steady state at the recrystallization of ore-bearing minerals. At the same time a rare element zirconium and a rare-earth element ytterbium selectively concentrate in the zircon and apatite respectively.
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Dissertations / Theses on the topic "Restite"

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Pett, Teresa K. "Garnetites of the Cardigan Pluton - Evidence for Restite and Implications for Source Rock Compositions." BYU ScholarsArchive, 2006. https://scholarsarchive.byu.edu/etd/1099.

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The Cardigan pluton, located in the southern half of New Hampshire, is a strongly peraluminous, S-type granite which is granodioritic in composition. It is inferred to have been emplaced rapidly, thrust up along west-verging nappes during the Acadian orogeny. Distinctive pods, consisting of 50 to 70 percent modal garnet, are found throughout the pluton in assemblages of garnet + sillimanite + biotite + plagioclase + quartz. These garnetite rocks present an intriguing case for restite. Textural features of the garnetite rocks, such as fibrolitic sillimanite mats and flat, unzoned major and trace-element garnet grain profiles, provide evidence for biotite dehydration melting with single-stage garnet growth from the reaction: bio + plag + qtz + kspar = gar + sill + liq. Temperatures calculated using garnet-biotite (GB) thermometry and garnet-aluminum silicate-quartz-plagioclase (GASP) barometry yield estimates between 662-714ºC and 3.8 kbars. These low calculated temperatures are most likely the result of biotite compositions which have been altered by retrograde exchange reactions. The dominant source rock for the Cardigan magmas was likely calc-pelitic to greywacke in composition. Major element modeling suggests that ~70% melting of a calc-pelitic metasediment from the Central Maine trough could have generated a granodioritic melt similar to the average granodiorite of the Cardigan pluton. However, most of the Cardigan garnetite rocks appear to have been derived from pelites, as they are too poor in CaO and Na2O. Hence, though the majority of garnetite rocks cannot represent the dominant restite of the source rocks that produced the Cardigan pluton, they do appear to be the melt-depleted residue of an unidentified pelitic source. Comparison of Nd and Sr isotopic data from garnetite and Central Maine trough metasediments permit an interpretation that the Lower Rangeley Formation, from the Central Maine trough, could be the source rock of the Cardigan magmas. However, one feldspar Pb isotopic analysis in the literature (Moench and Allienikoff, 2002) and rare monazite chemical ages near 600 Ma suggest that the Cardigan pluton does not have a Laurentian source (i.e. Lower Rangeley Formation or other Central Maine trough metasediments), whereas an inferred peri-Gondwanan basement source is permissible.
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Towbin, W. Henry. "Thermobarometric modeling of the Catalina amphibolite unit: implications for tectonic and metasomatic models." Oberlin College Honors Theses / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1384646494.

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Braaten, Ellen. "Resting places /." This resource online, 1995. http://scholar.lib.vt.edu/theses/available/etd-08222009-040549/.

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Braaten, Ellen B. 1942. "Resting places." Thesis, Virginia Tech, 1995. http://hdl.handle.net/10919/44409.

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Ancient humans stored family remains under their houses as we have surely stored memories in our attics. As civilization progressed, ashes were placed in urns which often replicated the house where one lived on earth. Eventually more elaborate and stylized monuments housed the remains. Recent practices have shown estrangement to death and denial of its importance in the natural cycle. this project reintroduces the funeral urn as object and ritual. It attempts to reawaken and reconnect us to our historically diverse cultures and to the life-death cycle by creating the house for ashes. This house is our last abode.
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Arndt, Bjorn Lewis. "reStill: rethinking distillation." Thesis, University of Canterbury. Master of Engineering Management, 2014. http://hdl.handle.net/10092/8942.

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The reStill is the next generation in home-distillation columns, more commonly referred to as Stills. The advances in design and control make it easier than ever to produce high quality alcohol. The project focussed on producing a proof of concept and conducting market validation for the product as it was in the design/concept stage. This report summarises the planning processes involved in the project, the progression of the venture to date and analyses the lessons learnt during this process.
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Heber, Ashley Dawn. "Resting cake face." Thesis, University of Iowa, 2015. https://ir.uiowa.edu/etd/1623.

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My most recent series of paintings places specific focus on the societal struggles young women face with an emphasis on the need to constantly be viewed as attractive. I am interested in cultural taboos of women's sexuality, and body image anxiety. Layered imagery of anonymous groups of young women paired with grotesque representations of food mimic the internet bombardment so inescapable for young women today. Painted stereotypes of beauty further show the imbalance of male / female gender roles and holographic glitter as well as day glow color push the drama further. In spending time with my drawings and paintings the viewer will, ideally, begin to question the cultural expectations for women, and contemplate possibilities for change.
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Lee, Kam-sing, and 李金成. "From painted brick to facing brick: to restore or not to restore." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B47584130.

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Traditionally, architectural and construction development in Hong Kong relies on load bearing bricks for structural support. In the modern age after World War II, the common application of reinforced concrete structure in high-rise construction has seen a change in the use of brick as an infill material for reinforced concrete frame construction. Because load bearing brick cannot meet the structural requirement of high-rise buildings, it is no longer common used in construction, and brick buildings that have been built are gradually demolished for redevelopment. For surviving brick buildings in Hong Kong, the ones built with red facing bricks are generally Western style buildings mostly located in Kowloon and Hong Kong Island. For buildings built of Chinese grey brick, they are usually Chinese vernacular buildings, such as ancestral halls and temples, located in New Territories. However, with the common availability of modern paint for redecoration as well as weather protection, some brick heritage buildings have been plastered with rendering and painted. The reason for this is that a smooth painted surface gives a neater appearance and the impression of being easier to maintain and clean. Of course, there are also some traditional Chinese vernacular brick buildings, particularly Hakka houses (客家屋), which have a tradition of having brick surfaces painted with white wash covered with lime plaster (Tsang Tai Uk at Shatin and Poon Uk at Yuen Long are examples). With heritage conservation becoming more important, there are now more and more restoration work carried out on historical brick buildings. These projects are usually led by the Antiquities and Monuments Office and executed by the Architectural Services Department. One of the restoration problems faced in these projects is the removal of paint so that the original brick surface will be revealed. This dissertation aims to concentrate on the common methods used in Hong Kong to restore painted brick surfaces and to evaluate these paint removal methods through case studies that involves buildings of red engineering facing brick and Chinese grey brick. Through this dissertation, it will be demonstrated that restoring a brick surface is not straight forward technical work, but a process that must have a systematic conservation approach and planning. The dissertation will examine case studies of conservation projects involving paint removal work, and use the lesson learned to establish guidelines for paint removal in a planned and systematic way.
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Master of Science in Conservation
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Cushman, G. Mark. "Resting in God's guidance." Online full text .pdf document, available to Fuller patrons only, 2004. http://www.tren.com.

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Micena, Fernando Pereira. "Problema restrito dos três corpos." Universidade de São Paulo, 2007. http://www.teses.usp.br/teses/disponiveis/55/55135/tde-09052007-142925/.

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O problema de n?corpos é um dos problemas mais importantes em Sistemas Dinâmicos. Nós estudamos o modelo do problema dos três corpos restrito introduzido por Sitnikov. Nesse modelo os corpos primários tem a mesma massa e o terceiro corpo é de massa muito pequena com respeito aos corpos primários. Usando os métodos de Alekseev, nós mostramos a existência de uma ?ferradura de Smale?como um subsistema da dinâmica do terceiro corpo e concluímos ricas conseqüências probabilísticas. Nós também estudamos o problema pelo método de Melnikov
The n?body problem is one of the most important problems in dynamical systems. We study the model introduced by Sitnikov of restricted three body problem. In this model the primaries are of equal mass and the third body is very small with respect to the primaries. Using methods of Alekseev, we show the existence of ?Smale horseshoe?as a subsystem of the dynamic of the third body and conclude rich probabilistic consequences. We also study the same problem by Melnikov?s method
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Ruggiero, Jérôme. "Stocker et restituer un photon unique." Phd thesis, Université Paris Sud - Paris XI, 2010. http://tel.archives-ouvertes.fr/tel-00551521.

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L'objet de ce travail de thèse est d'étudier un cas particulier de l'interaction lumière-matière dans le cadre du stockage d'information quantique. Nous nous sommes intéressés aux processus appelés transitoires optiques cohérents, et plus précisément à l'écho de photon à deux impulsions. Ce processus est observé dans des cristaux dopés aux ions lanthanides, tel que le Tm3+:YAG. Une fois éclairé par une impulsion faible (le signal à stocker) puis par une impulsion plus intense (servant à la remise en phase des dipôles induits), ce milieu atomique, essentiellement un système à deux niveaux avec une transition large, réemet une troisième impulsion, qui est l'"écho" temporel de la première (chapitre 1). Nous avons observé de tels échos expérimentalement, et ce pour des impulsions de signal faibles. Néanmoins, des effets délétères, dûs à l'impulsion de rephasage et à sa propagation, nous ont permis de conclure sur l'impossibilité d'utiliser ce processus tel quel en tant que protocole de mémoire quantique (chapitre 2). Le troisième chapitre a pour objet l'état des lieux des diverses méthodes dérivées de l'écho de photon à deux impulsions. Notamment, nous examinons la capacité théorique des échos Stark à restituer une éventuelle information quantique. Bien que prometteuse, nous lui avons préféré un autre processus, basé sur la structuration de l'absorption du système en peigne de fréquences atomiques (AFC en anglais). Son étude théorique consistitue la fin du chapitre 3. Le dernier chapitre (4) s'attache à résumer les expériences que nous avons réalisées sur le protocole AFC. Elles ont permis d'observer des échos AFC avec une efficacité proche de 10%. Elles ont également permis de dégager des axes de recherche pour améliorer le protocole, comme l'AFC large- bande, ou en régime de comptage de photons.
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Books on the topic "Restite"

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Resting. London: Raintree, 2012.

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Restrike. Stamford, CT: The Story Plant, 2013.

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Poste restante. Santiago: Editorial Sudamericana, 2001.

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Hinthorn, Aletha. Quietly resting. Waterville, Me: Thorndike Press, 2005.

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Mafi, Tahereh. Restore me. New York: HarperCollins Publishers, 2018.

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Jaffe, Shirley. Poste restante. [Paris]: Collectif Génération, 1991.

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Quietly resting. Kansas City, Mo: Beacon Hill Press of Kansas City, 1996.

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Restive partners: Washington and Bonn diverge. Boulder: Westview Press, 1990.

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Maurice, François. Aulan: Château restitué. L'Isle-sur-la-Sorgue: Edition Scriba, 1995.

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Aufrère, Sydney. L' Égypte restituée. Paris: Editions Errance, 1991.

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Book chapters on the topic "Restite"

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Pitcher, Wallace Spencer. "The evidence for restite: unmixing as an alternative hypothesis." In The Nature and Origin of Granite, 125–43. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5832-9_8.

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Pitcher, Wallace Spencer. "The evidence for restite: unmixing as an alternative hypothesis." In The Nature and Origin of Granite, 103–16. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-017-3393-9_8.

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Gawęda, Aleksandra, Mirosław Kierepka, Janusz Janeczek, and Alicja Mazur-Cuber. "Paralava from Coal-Dump Combustion in Upper Silesia, Poland: Melt Separation Leaving a Cordierite-Rich Restite." In Proceedings of the 10th International Congress for Applied Mineralogy (ICAM), 221–27. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-27682-8_28.

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Bährle-Rapp, Marina. "restore." In Springer Lexikon Kosmetik und Körperpflege, 474. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-71095-0_8870.

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Shoff, William H., Catherine T. Shoff, Suzanne M. Shepherd, Jonathan L. Burstein, Calvin A. Brown, Ashita J. Tolwani, Bala Venkatesh, et al. "Restore." In Encyclopedia of Intensive Care Medicine, 1996. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-00418-6_2151.

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Weik, Martin H. "restore." In Computer Science and Communications Dictionary, 1485. Boston, MA: Springer US, 2000. http://dx.doi.org/10.1007/1-4020-0613-6_16275.

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Hohler, Anna DePold, and Marcus Ponce de Leon. "Resting Tremor." In Encyclopedia of Clinical Neuropsychology, 2161. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-0-387-79948-3_477.

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Gooch, Jan W. "Resting Potential." In Encyclopedic Dictionary of Polymers, 920. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_14691.

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Weitz, Edmund. "RESTE." In Pi und die Primzahlen, 99–104. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-62880-5_13.

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Hunt, P. J., and B. Sendell. "Sleeping and Resting." In A Personal Approach to Patient Care, 156–83. London: Macmillan Education UK, 1987. http://dx.doi.org/10.1007/978-1-349-08562-0_6.

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Conference papers on the topic "Restite"

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García-Arias, Marcos, Juan Sebastián Puerto-León, and Carlos Daniel Ronderos-Almeida. "Cordilleran Granitoids and Restite Entrainment: A Thermodynamic Modelling." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.797.

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Sakaguchi, Saki, Hikari Tono, Takuma Tanaka, and Mitsunori Matsushita. "Restive shadow." In SIGGRAPH Asia 2013 Emerging Technologies. New York, New York, USA: ACM Press, 2013. http://dx.doi.org/10.1145/2542284.2542300.

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Strauch, Jakob, and Silvia Schreier. "RESTify." In the Third International Workshop. New York, New York, USA: ACM Press, 2012. http://dx.doi.org/10.1145/2307819.2307824.

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Elghandour, Iman, and Ashraf Aboulnaga. "ReStore." In the 2012 international conference. New York, New York, USA: ACM Press, 2012. http://dx.doi.org/10.1145/2213836.2213937.

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Medeiros, Lívia Salgado, Fabiano De Souza Oliveira, and Jayme Luiz Szwarcfiter. "Limite superior algorítmico para a contagem de intervalo." In Encontro de Teoria da Computação. Sociedade Brasileira de Computação - SBC, 2021. http://dx.doi.org/10.5753/etc.2021.16367.

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O emprego de técnicas de otimização combinatória associadas ao problema da contagem de intervalo foi explorado por Joos et al., resolvendo de forma eficiente uma versão restrita do problema da contagem de intervalo 2. Para o problema de determinação da contagem de intervalo geral, nenhuma técnica semelhante é conhecida atualmente. Elaboramos formulações de programação quadrática, levando a um algoritmo pseudopolinomial, para fornecer um limite superior na contagem de intervalo geral de ordens, que é empiricamente mostrado como próximo ao respectivo valores reais. Para a classe de semiordens, o limite superior é mostrado como restrito.
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Wang, Rujia, Lei Jiang, Youtao Zhang, Linzhang Wang, and Jun Yang. "Selective restore." In DAC '15: The 52nd Annual Design Automation Conference 2015. New York, NY, USA: ACM, 2015. http://dx.doi.org/10.1145/2744769.2744908.

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Chupin, Guerric, and Henrik Nilsson. "Functional Reactive Programming, restated." In PPDP '19: Principles and Practice of Programming Languages 2019. New York, NY, USA: ACM, 2019. http://dx.doi.org/10.1145/3354166.3354172.

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Fereidouni, Marzie, Hamid Soltanian-Zadeh, Quan Jiang, and Kost V. Elisevich. "Impaired resting state networks in temporal lobe epilepsy: A resting state fMRI study." In 2012 19th Iranian Conference of Biomedical Engineering (ICBME). IEEE, 2012. http://dx.doi.org/10.1109/icbme.2012.6519686.

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Reed, Benjamin B., Robert C. Smith, Bo J. Naasz, Joseph F. Pellegrino, and Charles E. Bacon. "The Restore-L Servicing Mission." In AIAA SPACE 2016. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2016. http://dx.doi.org/10.2514/6.2016-5478.

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Billings, Jacob C. W., Alessio Medda, and Shella D. Keilholz. "Agglomerative clustering for resting state MRI." In 2013 6th International IEEE/EMBS Conference on Neural Engineering (NER). IEEE, 2013. http://dx.doi.org/10.1109/ner.2013.6695994.

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Reports on the topic "Restite"

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Karonis, N. T. BURT: back up and restore tool. Office of Scientific and Technical Information (OSTI), November 1994. http://dx.doi.org/10.2172/207584.

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Andrew Tomes, Andrew Tomes. Can fungi help restore the American chestnut? Experiment, August 2014. http://dx.doi.org/10.18258/3273.

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Meredith Root-Bernstein, Meredith Root-Bernstein. Can we restore the Chilean "espinal" with guanacos? Experiment, August 2013. http://dx.doi.org/10.18258/1160.

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Westphal, Lynne M., Cristy Watkins, Paul H. Gobster, Liam Heneghan, Kristen Ross, Laurel Ross, Madeleine Tudor, et al. Social Science Methods Used in the RESTORE Project. Newtown Square, PA: U.S. Department of Agriculture, Forest Service, Northern Research Station, 2014. http://dx.doi.org/10.2737/nrs-gtr-138.

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Clarke, Walter S. SOMALIA: Background Information for Operation Restore Hope. 1992-1993. Fort Belvoir, VA: Defense Technical Information Center, December 1992. http://dx.doi.org/10.21236/ada259959.

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Jennifer R. Pournelle, Jennifer R. Pournelle. Water From Oil: Can We Help Restore Iraq's Marshes? Experiment, March 2014. http://dx.doi.org/10.18258/2206.

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McRoberts, Heidi. Restore McComas Watershed; Meadow Creek Watershed, 2002-2003 Annual Report. Office of Scientific and Technical Information (OSTI), January 2004. http://dx.doi.org/10.2172/901073.

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McRoberts, Heidi. Restore McComas Meadows; Meadow Creek Watershed, 2004-2005 Annual Report. Office of Scientific and Technical Information (OSTI), December 2005. http://dx.doi.org/10.2172/901076.

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McRoberts, Heidi. Restore McComas Meadows; Meadow Creek Watershed, 2003-2004 Annual Report. Office of Scientific and Technical Information (OSTI), August 2006. http://dx.doi.org/10.2172/901078.

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McRoberts, Heidi. Restore McComas Meadows; Meadow Creek Watershed, 2005-2006 Annual Report. Office of Scientific and Technical Information (OSTI), July 2006. http://dx.doi.org/10.2172/901080.

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