Bibliografías temáticas / Crystals Apatite. Silicon crystals

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Literatura académica sobre el tema "Crystals Apatite. Silicon crystals"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 9 de febrero de 2022

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Artículos de revistas sobre el tema "Crystals Apatite. Silicon crystals"

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Ma, Hai Zhu, Fang Huang, Shi Rong Liu, Bo Xu y Hua Long Liu. "Classification and Morphological Structure of Scale in the Process of Alumina Production High Pressure Digestion". Advanced Materials Research 960-961 (junio de 2014): 274–80. http://dx.doi.org/10.4028/www.scientific.net/amr.960-961.274.

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The chemical composition, phase component and morphology characteristics of scale were researched by chemical analysis, XRD, SEM and TEM. The results show that the scale can be divided into iron minerals, silicon minerals, Ca-Ti-Mg minerals and aluminum hydroxide. Alumogoethite and micro-fine sodium-silicon slag fill in the gaps between the neat and bulky hematite crystals. Microgranular hydrated garnet and olivine fill in the gaps between the goethite crystals with a dense layered structure, accompanied by a small amount of galena and apatite precipitation particles. Perovskite and magnesium hydroxide have five periodic sedimentary cycles, forming an alternating sedimentary layer structure. Aluminum hydroxide forms thick scale and presents two kinds of typical structures, spherulitic and laminated. The research provides the theoretical basis for preventing and controlling scale in high-pressure digester group.
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Barbee, Olivia, Craig Chesner y Chad Deering. "Quartz crystals in Toba rhyolites show textures symptomatic of rapid crystallization". American Mineralogist 105, n.º 2 (1 de febrero de 2020): 194–226. http://dx.doi.org/10.2138/am-2020-6947.

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Abstract Textural and chemical heterogeneities in igneous quartz crystals preserve unique records of silicic magma evolution, yet their origins and applications are controversial. To improve our understanding of quartz textures and their formation, we examine those in crystal-laden rhyolites produced by the 74 ka Toba supereruption (>2800 km3) and its post-caldera extrusions. Quartz crystals in these deposits can reach unusually large sizes (10–20 mm) and are rife with imperfections and disequilibrium features, including embayments, melt inclusions, titanomagnetite and apatite inclusions, spongy morphologies, hollow faces, subgrain boundaries, multiple growth centers, and Ti-enriched arborescent zoning. Using a combination of qualitative and quantitative analyses (petrography, CL, EBSD, X-ray CT, LA-ICPMS), we determine that those textures commonly thought to signify crystal resorption, crystal deformation, synneusis, or fluctuating P–T conditions are here a consequence of rapid disequilibrium crystal growth. Most importantly, we discover that an overarching process of disequilibrium crystallization is manifested among these crystal features. We propose a model whereby early skeletal to dendritic quartz growth creates a causal sequence of textures derived from lattice mistakes that then proliferate during subsequent stages of slower polyhedral growth. In a reversed sequence, the same structural instabilities and defects form when slow polyhedral growth transitions late to fast skeletal-dendritic growth. Such morphological transitions result in texture interdependencies that become recorded in the textural-chemical stratigraphy of quartz, which may be unique to each crystal. Similar findings in petrologic experimental studies allow us to trace the textural network back to strong degrees of undercooling and supersaturation in the host melt, conditions likely introduced by dynamic magmatic processes acting on short geologic timescales. Because the textural network can manifest in single crystals, the overall morphology and chemistry of erupted quartz can reflect not only its last but its earliest growth behavior in the melt. Thus, our findings imply that thermodynamic disequilibrium crystallization can account for primary textural and chemical heterogeneities preserved in igneous quartz and may impact the application of quartz as a petrologic tool.
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Szopa, Krzysztof, Roman Włodyka y David Chew. "LA-ICP-MS U-Pb apatite dating of Lower Cretaceous rocks from teschenite-picrite association in the Silesian Unit (southern Poland)". Geologica Carpathica 65, n.º 4 (1 de agosto de 2014): 273–84. http://dx.doi.org/10.2478/geoca-2014-0018.

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Abstract The main products of volcanic activity in the teschenite-picrite association (TPA) are shallow, sub-volcanic intrusions, which predominate over extrusive volcanic rocks. They comprise a wide range of intrusive rocks which fall into two main groups: alkaline (teschenite, picrite, syenite, lamprophyre) and subalkaline (dolerite). Previous 40Ar/39Ar and 40K/40Ar dating of these rocks in the Polish Outer Western Carpathians, performed on kaersutite, sub-silicic diopside, phlogopite/biotite as well as on whole rock samples has yielded Early Cretaceous ages. Fluorapatite crystals were dated by the U-Pb LA-ICP-MS method to obtain the age of selected magmatic rocks (teschenite, lamprophyre) from the Cieszyn igneous province. Apatite-bearing samples from Boguszowice, Puńców and Lipowa yield U-Pb ages of 103± 20 Ma, 119.6 ± 3.2 Ma and 126.5 ± 8.8 Ma, respectively. The weighted average age for all three samples is 117.8 ± 7.3 Ma (MSWD = 2.7). The considerably smaller dispersion in the apatite ages compared to the published amphibole and biotite ages is probably caused by the U-Pb system in apatite being less susceptible to the effects of hydrothermal alternation than the 40Ar/39Ar or 40K/40Ar system in amphibole and/or biotite. Available data suggest that volcanic activity in the Silesian Basin took place from 128 to 103 Ma with the the main magmatic phase constrained to 128-120 Ma.
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Barbarand, Jocelyn y Maurice Pagel. "Cathodoluminescence study of apatite crystals". American Mineralogist 86, n.º 4 (abril de 2001): 473–84. http://dx.doi.org/10.2138/am-2001-0411.

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Aizawa, Mamoru, Nelesh Patel, Alexandra E. Porter, Serena Best y William Bonfield. "Syntheses of Silicon-Containing Apatite Fibres by a Homogeneous Precipitation Method and Their Characterization". Key Engineering Materials 309-311 (mayo de 2006): 1129–32. http://dx.doi.org/10.4028/www.scientific.net/kem.309-311.1129.

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Silicon-containing apatite (Si-HAp) fibres were successfully synthesized by a homogeneous precipitation method. The resulting Si-HAp fibres were composed of carbonate-containing apatite fibres with preferred orientation in the c-axis. The Si contents in the Si-HAp fibres could be controlled by the Si concentration of the starting solutions. TEM observation indicated that the Si-HAp fibres were of single crystal. The Si-HAp fibres have potential as novel materials for high-performance biomedical devices.
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Dorozhkin, Sergey V. "A hierarchical structure for apatite crystals". Journal of Materials Science: Materials in Medicine 18, n.º 2 (febrero de 2007): 363–66. http://dx.doi.org/10.1007/s10856-006-0701-x.

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López, Cefe. "Silicon Photonic Crystals". Optics and Photonics News 20, n.º 1 (1 de enero de 2009): 28. http://dx.doi.org/10.1364/opn.20.1.000028.

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Müller, Frank A., Lenka Müller, Daniel Caillard y Egle Conforto. "Preferred growth orientation of biomimetic apatite crystals". Journal of Crystal Growth 304, n.º 2 (junio de 2007): 464–71. http://dx.doi.org/10.1016/j.jcrysgro.2007.03.014.

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Su, X. W. y F. Z. Cui. "Direct observations on apatite crystals in ivory". Journal of Materials Science Letters 16, n.º 14 (julio de 1997): 1198–200. http://dx.doi.org/10.1007/bf02765409.

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Rusiecka, Monika K. y Don R. Baker. "Monazite and xenotime solubility in hydrous, boron-bearing rhyolitic melt". American Mineralogist 104, n.º 8 (1 de agosto de 2019): 1117–30. http://dx.doi.org/10.2138/am-2019-6931.

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Abstract We conducted a series of monazite and xenotime dissolution experiments in a boron-bearing silicic melt at 1000–1400 °C and 800 MPa in a piston-cylinder apparatus. We present new measurements of monazite and xenotime solubility in hydrous (~3 wt% water), boron-bearing rhyolitic melts, as well as the diffusivities of the essential structural constituents of those minerals (LREE, P, and Y). We compare our results to the previous studies and discuss the implications of this study on the understanding of natural, silicic (granitic/rhyolitic) systems. We propose one equation describing the relationship between the solubility of xenotime and temperature in hydrous rhyolitic melts: ln ⁡ Y = 18.3 ± 0.3 − 125499 ± 3356 R T and another for monazite: ln ⁡ Σ LREE = 18.6 ± 1.5 − 129307 ± 18163 R T . In the presence of sufficient phosphorous, the concentration of LREE needed for monazite saturation is within the uncertainty of the Y concentration needed from xenotime saturation and indicates that in the case of equilibrium crystallization the mineral that forms will only depend on the availability of LREE and Y and HREE. Given the similarity of the solubility of xenotime to that of monazite, we propose that previously published models of monazite solubility in silicic melts can potentially be applied to xenotime, and could, like monazite, serve as a geothermometer. In the case of disequilibrium crystallization in front of rapidly growing crystals, Y will diffuse faster than LREE and xenotime will only crystallize when LREE are depleted. We also found that the diffusion of Y is greater than the diffusion of P from dissolving xenotime, unlike the similar diffusivities of LREE and P during monazite dissolution. The significant difference between Y and P diffusivities suggests that the components forming xenotime diffuse as separate entities rather than molecular complexes. The dissolution of phosphates (monazite, xenotime, apatite) in hydrous, silicic melts with the addition of boron leads to liquid-liquid immiscibility at high temperatures where the saturation values of P and either light rare earth elements or Y are in the weight percent range. Immiscibility is not observable at low, magmatic temperatures, most probably due to the lower concentrations of P2O5 necessary for phosphate saturation at these conditions; however addition of other components, notably F, may result in liquid-liquid immiscibility at magmatic temperatures.
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Tesis sobre el tema "Crystals Apatite. Silicon crystals"

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Rulis, Paul Michael Ching Wai-Yim. "Computational studies of bioceramic crystals & related materials". Diss., UMK access, 2005.

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Thesis (Ph. D.)--Dept. of Physics and School of Computing and Engineering. University of Missouri--Kansas City, 2005.
"A dissertation in physics and computer networking." Advisor: Wai-Yim Ching. Typescript. Vita. Title from "catalog record" of the print edition Description based on contents viewed March 12, 2007. Includes bibliographical references (leaves 256-267). Online version of the print edition.
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Balmforth, Barnaby William. "Silicon photonic crystals for quantum optics applications". Thesis, University of Cambridge, 2009. https://www.repository.cam.ac.uk/handle/1810/252125.

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Deng, Xin y 鄧欣. "Positron studies of silicon and germanium nanocrystals embedded in silicon dioxide". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2009. http://hub.hku.hk/bib/B41508749.

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Deng, Xin. "Positron studies of silicon and germanium nanocrystals embedded in silicon dioxide". Click to view the E-thesis via HKUTO, 2009. http://sunzi.lib.hku.hk/hkuto/record/B41508749.

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Van, Hoose Ashley Elizabeth. "Apatite Crystal Populations of the 1991 Mount Pinatubo Eruption, Philippines: Implications for the Generation of High Sulfur Apatite in Silicic Melts". PDXScholar, 2012. https://pdxscholar.library.pdx.edu/open_access_etds/123.

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On June 15, 1991, Mount Pinatubo, Philippines, ejected 20 million tonnes of sulfur dioxide into the atmosphere, significantly impacting global climate and stratospheric ozone. Recharging basaltic magma mixed into the 50 km³ dacitic magma reservoir 6 to 11 km beneath Mount Pinatubo, and triggered the 1991 eruption. The result of the magma mixing was a hybrid andesite with quenched basalt inclusions that erupted as a dome between June 7 and June 12. On June 15, approximately 5 km³ of anhydrite-bearing magma was erupted from the main phenocryst-rich, dacitic reservoir. This study will utilize this extraordinary framework of the 1991 Pinatubo eruption to investigate the systematics of sulfur uptake by apatite in order to further develop apatite as a monitor for magmatic sulfur. In the dacite and hybrid andesite, apatite occurs as individual phenocrysts (up to ~200 μm diameter) or included within anhydrite, hornblende, and plagioclase phenocrysts. In the basaltic magmatic inclusions, apatite is found as acicular microphenocrysts. Electron microprobe data collected on apatite yield low- (0.7 wt.% SO₃) apatites in all juvenile products, and show that two distinct populations of apatites exist: "silicic" apatites (hosted in dacite and andesite) and basalt apatites. Apatites crystallizing from silicic melt have predominantly low- to medium-sulfur contents, but high-sulfur apatites with as much as 1.2-1.7 wt.% SO₃ occur sporadically as inclusions in plagioclase, hornblende, Fe-Ti oxide, and anhydrite. These concentrations are much higher than what could be achieved through equilibrium crystal-melt partitioning at pre-eruption conditions (760±20°C, 220MPa, NNO+1.7, 77 ppm S in melt inclusions) and a partition coefficient of 13. Apatite in the basalt is always sulfur-rich with compositions forming a continuous array between 0.7 to 2.6 wt.% SO₃. The population of apatite that crystallized from silicic melt has elevated cerium, fluorine, and chlorine and lower magnesium concentrations (average dacite values in wt.%: 0.21 Ce₂O₃, 1.4 F, 1.1 Cl, & 0.14 MgO) relative to the population of apatite from the basalt (average basalt values in wt.%: 0.05 Ce₂O₃, 1.0 F, 0.78 Cl, & 0.22 MgO). LA-ICP-MS trace element data also show distinct apatite populations between silicic and basalt apatites. Silicic apatites have elevated REE concentrations (La avg. = 750 ppm), lower Sr (avg.= 594 ppm), and a pronounced negative Eu anomaly (avg. Eu/Eu* = 0.57) relative to basalt apatites (avg. values: 217 ppm La, 975 ppm Sr, and Eu/Eu* = 1.16). The correlation of EMP sulfur data and LA-ICP-MS trace element data show no difference between high-S and low-S silicic apatites. These compositional systematics rule out the possibility that sulfur-rich apatite from dacite are inherited from mafic magma. Sulfur element maps of apatites show no evidence of S-diffusion from anhydrite hosts. Areas of high-S concentrations show complicated patterns that suggest multiple periods of sulfur enrichment. High-S silicic apatites are likely the product of "fluid-enhanced crystallization" from early enrichment of a SO₂ rich fluid phase from the underplating basalt, which occurred prior to or at anhydrite saturation. This fluid phase is the only possible sufficient source of sulfur for generating high-S apatites in a cool, "wet", dacitic melt. The dynamics of apatite sulfur enrichment via "fluid-enhanced crystallization" is yet unclear and requires further experimental laboratory investigation.
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Rao, Yeswanth Lakshman. "A process for hydrogenation of silicon carbide crystals". Master's thesis, Mississippi State : Mississippi State University, 2001. http://library.msstate.edu/etd/show.asp?etd=etd-04102001-131544.

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Schonbrun, Ethan. "Negative refraction and anomalous propagation in silicon photonic crystals". Connect to online resource, 2007. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3256376.

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Lee, Grace W. (Grace Wang). "Optical absorption of bismuth silicon oxide (Bi₁₂SiO₂₀) crystals". Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/114089.

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Thesis: S.B., Massachusetts Institute of Technology, Department of Materials Science and Engineering, 2001.
Cataloged from PDF version of thesis.
Includes bibliographical references (page 23).
The purpose of this work is to characterize the optical absorption in bismuth silicon oxide (Bi₁₂SiO₂₀) crystals grown using the Bridgman technique and to identify electronic transitions responsible for absorption. Optical measurements were taken in the range of 0.4 - 11 pm at 300 K and 77 K using a spectrometer. The results show that near the band edge, there is evidence of indirect transitions at 2.3 eV and excition transitions at 1.8 eV. Low temperature measurements revealed peaks of free carrier absorption in the visible light range at 1.7 eV and 2.1 eV. Illuminated samples at low temperature revealed empty donor levels in the visible range at 1.6-1.9 eV and 2.1 eV, indicating the presence of the photochromic effect and photorefractivity.
by Grace W. Lee.
S.B.
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Brody, Jed. "Doping dependence of surface and bulk passivation of multicrystalline silicon solar cells". Diss., Available online, Georgia Institute of Technology, 2004:, 2003. http://etd.gatech.edu/theses/available/etd-04082004-180041/unrestricted/brody%5Fjed%5F200312%5Fphd.pdf.

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Naseh, Sasan. "Experimental investigation of anisotropic etching of silicon in tetra-methyl ammonium hydroxide". Thesis, Connect to online version, 1995. http://0-wwwlib.umi.com.mercury.concordia.ca/cr/concordia/fullcit?pMQ90888.

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Libros sobre el tema "Crystals Apatite. Silicon crystals"

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F, Kiselev V. y Mukashev B. N, eds. Defekty v kremnii i na ego poverkhnosti. Moskva: "Nauka," Glav. red. fiziko-matematicheskoĭ lit-ry, 1990.

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Alliance, Northwest Energy Efficiency. Silicon crystal growing facilities, No. 1. [Portland OR]: The Alliance, 1999.

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Pohoryles, Bronisław. Pochodzenie stanów elektronowych dyslokacji w germanie i krzemie. Wrocław: Zakład Narodowy im. Ossolińskich, 1987.

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Japan) Foton Fakutorī Kenkyūkai (2012 May 26-27 Tsukuba-shi. Shirikon tankesshō: Risō hinshitsu e no akunaki tsuikyū : handōtai sangyō no kome to hōshakō X-sen kōgaku soshi to shite : PF Kenkyūkai = Silicon single crystal : insatiable prusuit towards ideal quality as crop in semiconductor industry and x-ray optical element in synchrotron science. Tsukuba-shi, Ibaraki-ken: High Energy Accelerator Research Organization, 2012.

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Khokhlov, A. F. Allotropii︠a︡ kremnii︠a︡: Monografii︠a︡. Nizhniĭ Novgorod: Izd-vo Nizhegorodskogo gos. im. N.I. Lobachevskogo, 2002.

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Dziuban, J. A. Technologia i zastosowanie mikromechanicznych struktur krzemowych i krzemowo-szklanych w technice mikrosystemenów. Wrocław: Oficyna Wydawnicza Politechniki Wrocławskiej, 2002.

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Goncharov, E. G. Poluprovodnikovye fosfidy i arsenidy kremnii͡a︡ i germanii͡a︡. Voronezh: Izd-vo Voronezhskogo universiteta, 1989.

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International Symposium on High Purity Silicon (9th 2006 Cancún, Mexico). High purity silicon 9. Editado por Claeys Cor L, Electrochemical Society. Electronics and Photonics Division. y Electrochemical Society Meeting. Pennington, NJ: Electrochemical Society, 2006.

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International, Symposium on High Purity Silicon (9th 2006 Cancún Mexico). High purity silicon 9. Pennington, NJ: Electrochemical Society, 2006.

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L, Claeys Cor, Electrochemical Society Electronics Division, Society of Photo-optical Instrumentation Engineers. y Electrochemical Society Meeting, eds. High purity silicon VII. Pennington, NJ: Electrochemical Society, 2002.

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Capítulos de libros sobre el tema "Crystals Apatite. Silicon crystals"

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Estevez, J. Octavio y Vivechana Agarwal. "Porous Silicon Photonic Crystals". En Handbook of Porous Silicon, 805–14. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-05744-6_82.

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Snow, Paul. "Porous Silicon Phononic Crystals". En Handbook of Porous Silicon, 835–43. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-05744-6_85.

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Estevez, J. Octavio y Vivechana Agarwal. "Porous Silicon Photonic Crystals". En Handbook of Porous Silicon, 1201–10. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71381-6_82.

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Snow, Paul. "Porous Silicon Phononic Crystals". En Handbook of Porous Silicon, 1231–40. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71381-6_85.

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Geppert, Torsten, Joerge Schilling, Ralf Wehrspohn y Ulrich Gösele. "Silicon-Based Photonic Crystals". En Topics in Applied Physics, 295–322. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-39913-1_9.

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Ossicini, Stefano, Lorenzo Pavesi y Francesco Priolo. "Silicon-Based Photonic Crystals". En Springer Tracts in Modern Physics, 227–62. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-540-44877-8_6.

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Estevez, J. Octavio y V. Agarwal. "Porous Silicon Photonic Crystals". En Handbook of Porous Silicon, 1–10. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04508-5_82-1.

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Snow, Paul. "Porous Silicon Phononic Crystals". En Handbook of Porous Silicon, 1–9. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04508-5_85-1.

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Snow, Paul. "Porous Silicon Phononic Crystals". En Handbook of Porous Silicon, 1–10. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-04508-5_85-2.

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Stenin, S. I., B. Z. Kanter y A. I. Nikiforov. "Molecular-Beam Epitaxy of Silicon". En Growth of Crystals, 69–76. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-3268-2_6.

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Actas de conferencias sobre el tema "Crystals Apatite. Silicon crystals"

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KAWAGOE, D., K. IOKU, H. FUJIMORI y S. GOTO. "TRANSPARENT APATITE CERAMICS PREPARED FROM APATITE FINE CRYSTALS SYNTHESIZED HYDROTHERMALLY". En Proceedings of the Seventh International Symposium on Hydrothermal Reactions. WORLD SCIENTIFIC, 2003. http://dx.doi.org/10.1142/9789812705228_0015.

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DeLoach, L. D., S. A. Payne, W. F. Krupke, L. K. Smith, W. L. Kway, J. B. Tassano y B. H. T. Chai. "Laser and Spectroscopic Properties of Yb-Doped Apatite Crystals". En Advanced Solid State Lasers. Washington, D.C.: OSA, 1993. http://dx.doi.org/10.1364/assl.1993.lm3.

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Payne, Stephen A., Laura D. DeLoach, Larry K. Smith, William F. Krupke, Bruce H. T. Chai y George Loutts. "New Ytterbium-Doped Apatite Crystals for Flexible Laser Design". En Advanced Solid State Lasers. Washington, D.C.: OSA, 2004. http://dx.doi.org/10.1364/assl.1994.yl3.

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Srinivasan, Kartik, Marcelo Davanço y Karen Grutter. "Silicon nitride optomechanical crystals". En Frontiers in Optics. Washington, D.C.: OSA, 2014. http://dx.doi.org/10.1364/fio.2014.fw4b.2.

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Risse, J., A. Jacobi, Wolfgang Weissflog, D. Lose y S. Diele. "Influence of silicon on phase behavior of low-molecular liquid crystals". En Liquid Crystals, editado por Marzena Tykarska, Roman S. Dabrowski y Jerzy Zielinski. SPIE, 1998. http://dx.doi.org/10.1117/12.301257.

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Sin, Y. K. y K. Ibrahim. "2D Silicon-based Photonic Crystals". En 2006 IEEE International Conference on Semiconductor Electronics. IEEE, 2006. http://dx.doi.org/10.1109/smelec.2006.381055.

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Toshihiko Baba. "Photonic crystals and silicon photonics". En 2008 International Nano-Optoelectronics Workshop. IEEE, 2008. http://dx.doi.org/10.1109/inow.2008.4634438.

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Wong, Chee Wei, Xiaodong Yang, James F. McMillan y Chad A. Husko. "Photonic crystals and silicon photonics". En Integrated Optoelectronic Devices 2006, editado por Louay A. Eldada y El-Hang Lee. SPIE, 2006. http://dx.doi.org/10.1117/12.652641.

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Tokranova, Natalya, Da Song, Alison Gracias y James Castracane. "Porous silicon 2D photonic crystals". En Integrated Optoelectronic Devices 2007, editado por Ali Adibi, Shawn-Yu Lin y Axel Scherer. SPIE, 2007. http://dx.doi.org/10.1117/12.699127.

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Safavi-Naeini, Amir H., Thiago P. Mayer Alegre y Oskar Painter. "Cavity optomechanics and optomechanical crystals". En Integrated Photonics Research, Silicon and Nanophotonics. Washington, D.C.: OSA, 2010. http://dx.doi.org/10.1364/iprsn.2010.imf2.

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Informes sobre el tema "Crystals Apatite. Silicon crystals"

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Payne, S. A., L. D. DeLoach, L. K. Smith, W. F. Krupke, B. H. T. Chai y G. Loutts. New ytterbium-doped apatite crystals for flexible laser design. Office of Scientific and Technical Information (OSTI), marzo de 1994. http://dx.doi.org/10.2172/10166773.

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Kopanski, J. J. MIS capacitor studies on silicon carbide single crystals:. Gaithersburg, MD: National Institute of Standards and Technology, 1990. http://dx.doi.org/10.6028/nist.ir.4352.

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Van Hoose, Ashley. Apatite Crystal Populations of the 1991 Mount Pinatubo Eruption, Philippines: Implications for the Generation of High Sulfur Apatite in Silicic Melts. Portland State University Library, enero de 2000. http://dx.doi.org/10.15760/etd.123.

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Benson, Brandon. Channeling, Volume Reection and Gamma Emission Using 14GeV Electrons in Bent Silicon Crystals. Office of Scientific and Technical Information (OSTI), agosto de 2015. http://dx.doi.org/10.2172/1213166.

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Ptasinski, Joanna N. Absorption-induced Optical Tuning of Silicon Photonic Structures Clad with Nematic Liquid Crystals. Fort Belvoir, VA: Defense Technical Information Center, marzo de 2013. http://dx.doi.org/10.21236/ada577212.

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Benson, Brandon. Channeling, Volume Reflection and Gamma Emission Using 14GeV Electrons in Bent Silicon Crystals - General Abstract. Office of Scientific and Technical Information (OSTI), agosto de 2015. http://dx.doi.org/10.2172/1213168.

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Benson, Brandon. Channeling, volume reflection and gamma emission using 14GeV electrons in bent silicon crystals - Oral presentation. Office of Scientific and Technical Information (OSTI), agosto de 2015. http://dx.doi.org/10.2172/1213196.

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Dudley, Michael. In Situ Studies of Defect Nucleation During the PVT and CVD Growth of Silicon Carbide Single Crystals. Fort Belvoir, VA: Defense Technical Information Center, abril de 2008. http://dx.doi.org/10.21236/ada486859.

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Dudley, Michael. In Situ Studies of Defect Nucleation During the PVT and CVD Growth of Silicon Carbide Single Crystals. Fort Belvoir, VA: Defense Technical Information Center, marzo de 2006. http://dx.doi.org/10.21236/ada458217.

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Smither, R. K. y P. B. Fernandez. Apparent temperature versus true temperature of silicon crystals as a function of their thickness using infrared measurements. Office of Scientific and Technical Information (OSTI), diciembre de 1993. http://dx.doi.org/10.2172/10110324.

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