Journal articles: 'Olivine de San Carlos'

1

Gérard, O., and O. Jaoul. "Oxygen diffusion in San Carlos olivine." Journal of Geophysical Research: Solid Earth 94, B4 (April 10, 1989): 4119–28. http://dx.doi.org/10.1029/jb094ib04p04119.

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2

Houlier, Bernard, Mohammad Cheraghmakani, and Olivier Jaoul. "Silicon diffusion in San Carlos olivine." Physics of the Earth and Planetary Interiors 62, no. 3-4 (January 1990): 329–40. http://dx.doi.org/10.1016/0031-9201(90)90177-y.

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3

Kohlstedt, D. L., and S. J. Mackwell. "High-temperature stability of San Carlos olivine." Contributions to Mineralogy and Petrology 95, no. 2 (February 1987): 226–30. http://dx.doi.org/10.1007/bf00381272.

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4

Nunez, Ryan, Yougchul Kim, R. W. Carpenter, Mike McKelvy, Andrew Chizmeshya, and Hamdallah Bearat. "Interfacial Reaction Study of San Carlos Olivine Carbonation." Microscopy and Microanalysis 9, S02 (July 21, 2003): 682–83. http://dx.doi.org/10.1017/s1431927603443419.

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Béjina, F., P. Raterron, J. Zhang, O. Jaoul, and R. C. Liebermann. "Activation volume of silicon diffusion in San Carlos olivine." Geophysical Research Letters 24, no. 21 (November 1, 1997): 2597–600. http://dx.doi.org/10.1029/97gl02735.

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Abramson, E. H., J. M. Brown, L. J. Slutsky, and J. Zaug. "The elastic constants of San Carlos olivine to 17 GPa." Journal of Geophysical Research: Solid Earth 102, B6 (June 10, 1997): 12253–63. http://dx.doi.org/10.1029/97jb00682.

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7

Wanamaker, B. J., Teng-Fong Wong, and Brian Evans. "Decrepitation and crack healing of fluid inclusions in San Carlos olivine." Journal of Geophysical Research 95, B10 (1990): 15623. http://dx.doi.org/10.1029/jb095ib10p15623.

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8

Galoisy, Laurence, Georges Calas, and Gordon E. Brown. "Intracrystalline distribution of Ni in San Carlos Olivine; an EXAFS study." American Mineralogist 80, no. 9-10 (October 1, 1995): 1089–92. http://dx.doi.org/10.2138/am-1995-9-1028.

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9

Kubo, T. "Effects of Water on the - Transformation Kinetics in San Carlos Olivine." Science 281, no. 5373 (July 3, 1998): 85–87. http://dx.doi.org/10.1126/science.281.5373.85.

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10

Jaoul, O., B. Houlier, M. Cheraghmakani, R. Pichon, and R. C. Liebermann. "Surface destabilization and laboratory-induced non-stoichiometry in San Carlos olivine." Physics and Chemistry of Minerals 15, no. 1 (October 1987): 41–53. http://dx.doi.org/10.1007/bf00307607.

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11

Kubo, T., E. Ohtani, T. Kato, T. Shinmei, and K. Fujino. "Experimental investigation of the ?-? transformation of San Carlos olivine single crystal." Physics and Chemistry of Minerals 26, no. 1 (November 23, 1998): 1–6. http://dx.doi.org/10.1007/s002690050155.

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12

Afra, B., M. D. Rodriguez, M. Lang, R. C. Ewing, N. Kirby, C. Trautmann, and P. Kluth. "SAXS study of ion tracks in San Carlos olivine and Durango apatite." Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 286 (September 2012): 243–46. http://dx.doi.org/10.1016/j.nimb.2012.03.007.

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13

Su, Chang, Yonggang Liu, Wei Song, Dawei Fan, Zhigang Wang, and Hongfeng Tang. "Thermodynamic properties of San Carlos olivine at high temperature and high pressure." Acta Geochimica 37, no. 2 (February 23, 2018): 171–79. http://dx.doi.org/10.1007/s11631-018-0261-z.

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14

Pack, Andreas, Ryoji Tanaka, Markus Hering, Sukanya Sengupta, Stefan Peters, and Eizo Nakamura. "The oxygen isotope composition of San Carlos olivine on the VSMOW2-SLAP2 scale." Rapid Communications in Mass Spectrometry 30, no. 13 (June 8, 2016): 1495–504. http://dx.doi.org/10.1002/rcm.7582.

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15

Perrillat, J. P., I. Daniel, N. Bolfan-Casanova, M. Chollet, G. Morard, and M. Mezouar. "Mechanism and kinetics of the α-β transition in San Carlos olivine Mg1.8Fe0.2SiO4." Journal of Geophysical Research: Solid Earth 118, no. 1 (January 2013): 110–19. http://dx.doi.org/10.1002/jgrb.50061.

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16

Fournelle, J. "An Investigation of “San Carlos Olivine”: Comparing USNM-distributed Material with Commercially Available Material." Microscopy and Microanalysis 17, S2 (July 2011): 842–43. http://dx.doi.org/10.1017/s1431927611005083.

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17

Béjina, Frédéric, Olivier Jaoul, and Robert C. Liebermann. "Activation volume of Si diffusion in San Carlos olivine: Implications for upper mantle rheology." Journal of Geophysical Research: Solid Earth 104, B11 (November 10, 1999): 25529–42. http://dx.doi.org/10.1029/1999jb900270.

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18

Malvoisin, Benjamin, Fabrice Brunet, Julie Carlut, Stéphane Rouméjon, and Mathilde Cannat. "Serpentinization of oceanic peridotites: 2. Kinetics and processes of San Carlos olivine hydrothermal alteration." Journal of Geophysical Research: Solid Earth 117, B4 (April 2012): n/a. http://dx.doi.org/10.1029/2011jb008842.

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19

Wanamaker, B. J., and Brian Evans. "Mechanical re-equilibration of fluid inclusions in San Carlos olivine by power-law creep." Contributions to Mineralogy and Petrology 102, no. 1 (1989): 102–11. http://dx.doi.org/10.1007/bf01160194.

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20

Tingle, Tracy N., Michael F. Hochella, Christopher H. Becker, and Ripudaman Malhotra. "Organic compounds on crack surfaces in olivine from San Carlos, Arizona and Hualalai Volcano, Hawaii." Geochimica et Cosmochimica Acta 54, no. 2 (February 1990): 477–85. http://dx.doi.org/10.1016/0016-7037(90)90337-k.

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21

Brearley, Adrian J., and David C. Rubie. "Transformation mechanisms of San Carlos olivine to (MgFe)2SiO4 β-phase under subduction zone conditions." Physics of the Earth and Planetary Interiors 86, no. 1-3 (October 1994): 45–67. http://dx.doi.org/10.1016/0031-9201(94)05061-9.

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22

Wirth, R. "Nucleation of pyroxene and amphibole in glassy veins along interfaces and cracks in ultramafic inclusions from San Carlos, Arizona." Proceedings, annual meeting, Electron Microscopy Society of America 53 (August 13, 1995): 384–85. http://dx.doi.org/10.1017/s0424820100138294.

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Ultramafic inclusions occur in ellipsoidal bombs in basalt flows. The inclusions of the San Carlos ultramafic inclusion locality have been described in detail by Frey & Prinz (1978). They mainly consist of olivine, orthopyroxene (opx), clinopyroxene (cpx) and Cr-spinel. Ultramafic inclusions are important because they are samples of the upper mantle material, and thus they provide direct insight into the upper mantle processes and composition. Glassy veins are fairly abundant along mineral interfaces and cracks. The glass apparently results from incongruent melting of hydrous phases. The glassy veins are between a few nanometer and several microns wide. Veins with a width > 1 μm exhibit crystals of olivine, pyroxene and feldspar. The narrow veins (< 1 μm) only occasionally show crystallization of small crystals (several hundred nanometer). The early stages of crystallization of pyroxene and amphibole and the chemical composition have been investigated by HRTEM and analytical TEM.Glassy veins along interfaces: small grains (several hundred nanometer) of opx have nucleated at an opx/glass interface.

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23

Burnley, Pamela C., and Shirin Kaboli. "Elastic plastic self-consistent (EPSC) modeling of San Carlos olivine deformed in a D-DIA apparatus." American Mineralogist 104, no. 2 (February 1, 2019): 276–81. http://dx.doi.org/10.2138/am-2019-6666.

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24

Zha, Chang-sheng, Thomas S. Duffy, Robert T. Downs, Ho-kwang Mao, and Russell J. Hemley. "Brillouin scattering and X-ray diffraction of San Carlos olivine: direct pressure determination to 32 GPa." Earth and Planetary Science Letters 159, no. 1-2 (June 1998): 25–33. http://dx.doi.org/10.1016/s0012-821x(98)00063-6.

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25

Shinozaki, A., H. Hirai, H. Kagi, T. Kondo, and T. Yagi. "Polymerization of methane molecules and phase transition of san carlos olivine under the Earth's mantle conditions." Journal of Physics: Conference Series 215 (March 1, 2010): 012104. http://dx.doi.org/10.1088/1742-6596/215/1/012104.

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26

Chandler, Brian, Michelle Devoe, Martin Kunz, and Hans-Rudolf Wenk. "Using Multigrain Crystallography to Explore the Microstructural Evolution of the α-Olivine to γ-Ringwoodite Transformation and ε-Mg2SiO4 at High Pressure and Temperature." Minerals 11, no. 4 (April 16, 2021): 424. http://dx.doi.org/10.3390/min11040424.

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The introduction of multigrain crystallography (MGC) applied in a laser-heated diamond anvil cell (LH-DAC) using synchrotron X-rays has provided a new path to investigate the microstructural evolution of materials at extreme conditions, allowing for simultaneous investigations of phase identification, strain state determination, and orientation relations across phase transitions in a single experiment. Here, we applied this method to a sample of San Carlos olivine beginning at ambient conditions and through the α-olivine → γ-ringwoodite phase transition. At ambient temperatures, by measuring the evolution of individual Bragg reflections, olivine shows profuse angular streaking consistent with the onset of yielding at a measured stress of ~1.5 GPa, considerably lower than previously reported, which may have implications for mantle evolution. Furthermore, γ-ringwoodite phase was found to nucleate as micron to sub-micron grains imbedded with small amounts of a secondary phase at 15 GPa and 1000 °C. Using MGC, we were able to extract and refine individual crystallites of the secondary unknown phase where it was found to have a structure consistent with the ε-phase previously described in chondritic meteorites.

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27

Darling, Kenneth L., Gabriel D. Gwanmesia, Jennifer Kung, Baosheng Li, and Robert C. Liebermann. "Ultrasonic measurements of the sound velocities in polycrystalline San Carlos olivine in multi-anvil, high-pressure apparatus." Physics of the Earth and Planetary Interiors 143-144 (June 2004): 19–31. http://dx.doi.org/10.1016/j.pepi.2003.07.018.

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28

Wirth, Richard. "Thin amorphous films (1-2 nm) at olivine grain boundaries in mantle xenoliths from San Carlos, Arizona." Contributions to Mineralogy and Petrology 124, no. 1 (June 24, 1996): 44–54. http://dx.doi.org/10.1007/s004100050172.

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29

Wanamaker, B. J. "Point defect diffusivites in San Carlos olivine derived from reequilibration of electrical conductivity following changes in oxygen fugacity." Geophysical Research Letters 21, no. 1 (January 1, 1994): 21–24. http://dx.doi.org/10.1029/93gl02790.

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30

Chang, Yun-Yuan, Wen-Pin Hsieh, Eh Tan, and Jiuhua Chen. "Hydration-reduced lattice thermal conductivity of olivine in Earth’s upper mantle." Proceedings of the National Academy of Sciences 114, no. 16 (April 4, 2017): 4078–81. http://dx.doi.org/10.1073/pnas.1616216114.

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Earth’s water cycle enables the incorporation of water (hydration) in mantle minerals that can influence the physical properties of the mantle. Lattice thermal conductivity of mantle minerals is critical for controlling the temperature profile and dynamics of the mantle and subducting slabs. However, the effect of hydration on lattice thermal conductivity remains poorly understood and has often been assumed to be negligible. Here we have precisely measured the lattice thermal conductivity of hydrous San Carlos olivine (Mg0.9Fe0.1)2SiO4 (Fo90) up to 15 gigapascals using an ultrafast optical pump−probe technique. The thermal conductivity of hydrous Fo90 with ∼7,000 wt ppm water is significantly suppressed at pressures above ∼5 gigapascals, and is approximately 2 times smaller than the nominally anhydrous Fo90 at mantle transition zone pressures, demonstrating the critical influence of hydration on the lattice thermal conductivity of olivine in this region. Modeling the thermal structure of a subducting slab with our results shows that the hydration-reduced thermal conductivity in hydrated oceanic crust further decreases the temperature at the cold, dry center of the subducting slab. Therefore, the olivine−wadsleyite transformation rate in the slab with hydrated oceanic crust is much slower than that with dry oceanic crust after the slab sinks into the transition zone, extending the metastable olivine to a greater depth. The hydration-reduced thermal conductivity could enable hydrous minerals to survive in deeper mantle and enhance water transportation to the transition zone.

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31

Ferriss, Elizabeth, Terry Plank, Megan Newcombe, David Walker, and Erik Hauri. "Rates of dehydration of olivines from San Carlos and Kilauea Iki." Geochimica et Cosmochimica Acta 242 (December 2018): 165–90. http://dx.doi.org/10.1016/j.gca.2018.08.050.

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32

Wanamaker, B. J., and A. G. Duba. "Electrical conductivity of San Carlos Olivine along [100] under oxygen- and pyroxene-buffered conditions and implications for defect equilibria." Journal of Geophysical Research: Solid Earth 98, B1 (January 10, 1993): 489–500. http://dx.doi.org/10.1029/92jb01584.

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33

Spandler, Carl, and Hugh St C. O’Neill. "Diffusion and partition coefficients of minor and trace elements in San Carlos olivine at 1,300°C with some geochemical implications." Contributions to Mineralogy and Petrology 159, no. 6 (November 11, 2009): 791–818. http://dx.doi.org/10.1007/s00410-009-0456-8.

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34

Hu, Yan, Melissa D. Harrington, Yang Sun, Zhe Yang, Jasper Konter, and Fang-Zhen Teng. "Magnesium isotopic homogeneity of San Carlos olivine: a potential standard for Mg isotopic analysis by multi-collector inductively coupled plasma mass spectrometry." Rapid Communications in Mass Spectrometry 30, no. 19 (September 5, 2016): 2123–32. http://dx.doi.org/10.1002/rcm.7700.

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35

Chen, SiBo, XinZhuan Guo, ChunYin Zhou, and ZhenMin Jin. "Negative pressure effect on the electrical conductivity of San Carlos olivine and its implication to the electrical structure in the upper mantle." Science China Earth Sciences 59, no. 10 (September 6, 2016): 2078–88. http://dx.doi.org/10.1007/s11430-015-0216-y.

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36

Libourel, G. "High Temperature Reduction of San Carlos Olivines and Role of Kinetics on Metal/Silicate Interactions." Mineralogical Magazine 62A, no. 2 (1998): 889–90. http://dx.doi.org/10.1180/minmag.1998.62a.2.135.

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37

Chen, J., H. Liu, and J. Girard. "Comparative in situ X-ray diffraction study of San Carlos olivine: Influence of water on the 410 km seismic velocity jump in Earth's mantle." American Mineralogist 96, no. 5-6 (May 1, 2011): 697–702. http://dx.doi.org/10.2138/am.2011.3602.

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38

Quintanilla-Terminel, Alejandra, Mark E. Zimmerman, Brian Evans, and David L. Kohlstedt. "Microscale and nanoscale strain mapping techniques applied to creep of rocks." Solid Earth 8, no. 4 (July 10, 2017): 751–65. http://dx.doi.org/10.5194/se-8-751-2017.

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Abstract. Usually several deformation mechanisms interact to accommodate plastic deformation. Quantifying the contribution of each to the total strain is necessary to bridge the gaps from observations of microstructures, to geomechanical descriptions, to extrapolating from laboratory data to field observations. Here, we describe the experimental and computational techniques involved in microscale strain mapping (MSSM), which allows strain produced during high-pressure, high-temperature deformation experiments to be tracked with high resolution. MSSM relies on the analysis of the relative displacement of initially regularly spaced markers after deformation. We present two lithography techniques used to pattern rock substrates at different scales: photolithography and electron-beam lithography. Further, we discuss the challenges of applying the MSSM technique to samples used in high-temperature and high-pressure experiments. We applied the MSSM technique to a study of strain partitioning during creep of Carrara marble and grain boundary sliding in San Carlos olivine, synthetic forsterite, and Solnhofen limestone at a confining pressure, Pc, of 300 MPa and homologous temperatures, T∕Tm, of 0.3 to 0.6. The MSSM technique works very well up to temperatures of 700 °C. The experimental developments described here show promising results for higher-temperature applications.

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39

Nimz, G. J., K. L. Cameron, M. Cameron, and S. L. Morris. "The petrology of the lower crust and upper mantle beneath southeastern chihuahua, mexico: a progress report." Geofísica Internacional 25, no. 1 (January 1, 1986): 85–116. http://dx.doi.org/10.22201/igeof.00167169p.1986.25.1.802.

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En el basalto alcalino de la mina de peridotita La Olivina (localizada ~150 km al SE de Chihuahua, Chih.), se encuentran granulitas y nódulos ultramáficos del manto superior o la corteza inferior bajo la forma de xenolitos. Estos xenolitos ultramáficos pertenecen a tres grupos que se diferencian por su composición de clinopiroxenos: grupo I, alto magnesio (Mg/Mg+ Fe=0.90) y alto Cr203; grupo II, moderado magnesio (Mg/Mg+ Fe=0.76), alto Al203 y alto TiO2; y grupo III, con composición intermedia entre I y II (grupo de transición). Los análisis de minerales primarios muestran que los xenolitos son similares a los de San Carlos, Arizona, E.U., Xalapasco de la Joya, San Luis Potosi, México y Kilburne Hole, New Mexico, E.U. Los xenolitos del manto de La Olivina perte- necen a tres grupos con distinta textura: grupo I, granoblástica (Â¿metamórfica?); grupo II, granular allotriomórfica (Â¿ígnea?); y grupo III, granular allotriomórfica (Â¿ígnea?) con algunas texturas porfiroclasticas (Â¿metamórfica?). Los xenolitos de corteza inferior de La Olivina son predominantemente gneises pelíticos y granulitos de piroxeno. Los gneises pelíticos presentan ensambles uniformes de granate + cuarzo + plagioclasa + sanidina + silimanita + rutilo + grafito. La mayoría de las granulitas de piroxeno tienen plagioclasa, aunque algunas presentan escapolita en vez de plagioclasa. Estas muestras del manto inferior son idénticas en ensamble de minerales y muy simi- lares en geoquímica a los xenolitos del Kilburne Hole. Las granulitas y los gneises peliticos tienen edades modelo de Nd de 1.1 a 1.2 m.a., usando un cociente inicial de condritas, o bien 1.6 m.a. si se usa el modelo de fuente empobrecida. La edad de 1.6 m.a. concuerda muy bien con las edades del Kilbourne Hole, de aquí que se extiendan bajo el norte de México, al menos hasta el área de La Olivina, rocas precámbricas cratónicas, similares en edad, historia metamórfica y composición de protolito a las que están bajo Kilbourne Hole.

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40

Assaf-Balut, Carla, Nuria Garcia de la Torre, Alejandra Durán, Manuel Fuentes, Elena Bordiú, Laura del Valle, Johanna Valerio, et al. "Medical nutrition therapy for gestational diabetes mellitus based on Mediterranean Diet principles: a subanalysis of the St Carlos GDM Prevention Study." BMJ Open Diabetes Research & Care 6, no. 1 (October 2018): e000550. http://dx.doi.org/10.1136/bmjdrc-2018-000550.

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ObjectivesTo assess whether Mediterranean Diet (MedDiet)-based medical nutrition therapy facilitates near-normoglycemia in women with gestational diabetes mellitus (GDMw) and observe the effects on adverse pregnancy outcomes.Research design and methodsThis is a secondary analysis of the St Carlos GDM Prevention Study, conducted between January and December 2015 in Hospital Clínico San Carlos (Madrid, Spain). One thousand consecutive women with normoglycemia were included before 12 gestational weeks (GWs), with 874 included in the final analysis. Of these, 177 women were diagnosed with gestational diabetes mellitus (GDM) and 697 had normal glucose tolerance. All GDMw received MedDiet-based medical nutrition therapy with a recommended daily extra virgin olive oil intake ≥40 mL and a daily handful of nuts. The primary goal was comparison of hemoglobin A1c (HbA1c) levels at 36–38 GWs in GDMw and women with normal glucose tolerance (NGTw).ResultsGDMw as compared with NGTw had higher HbA1c levels at 24–28 GWs (5.1%±0.3% (32±0.9 mmol/mol) vs 4.9%±0.3% (30±0.9 mmol/mol), p=0.001). At 36–38 GWs values were similar between the groups. Similarly, fasting serum insulin and homeostatic model assessment insulin resitance (HOMA-IR) were higher in GDMw at 24–28 GWs (p=0.001) but became similar at 36–38 GWs. 26.6% of GDMw required insulin for glycemic control. GDMw compared with NGTw had higher rates of insufficient weight gain (39.5% vs 22.0%, p=0.001), small for gestational age (6.8% vs 2.6%, p=0.009), and neonatal intensive care unit admission (5.6% vs 1.7%, p=0.006). The rates of macrosomia, large for gestational age, pregnancy-induced hypertensive disorders, prematurity and cesarean sections were comparable with NGTw.ConclusionsUsing a MedDiet-based medical nutrition therapy as part of GDM management is associated with achievement of near-normoglycemia, subsequently making most pregnancy outcomes similar to those of NGTw.

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41

Pascual, E. "San Carlos." Journal of Epidemiology & Community Health 55, no. 10 (October 1, 2001): 689a—689. http://dx.doi.org/10.1136/jech.55.10.689a.

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42

Healy, Donald T. "San Carlos Apache." Raven: A Journal of Vexillology 3 (1996): 152–53. http://dx.doi.org/10.5840/raven1996/19973/492.

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43

Romero de Terreros, Manuel. "Museo de San Carlos." Anales del Instituto de Investigaciones Estéticas 7, no. 28 (July 30, 2012): 117. http://dx.doi.org/10.22201/iie.18703062e.1959.28.664.

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44

Rivaya-Martínez, Joaquín, and Carole Cancel. "San Carlos de los Jupes." Recherches amérindiennes au Québec 41, no. 2-3 (January 20, 2014): 29–42. http://dx.doi.org/10.7202/1021611ar.

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En juillet 1787, Paruanarimuco, principal chef des Comanches jupes, sollicita le soutien de Juan Bautista de Anza, gouverneur espagnol du Nouveau-Mexique, en vue de la construction d’un village pour accueillir les siens. Les autorités du nord de la Nouvelle-Espagne s’empressèrent de donner suite à cette requête pour le moins inhabituelle, envisageant de créer ainsi un précédent chez les nomades païens de la frontière dans la sédentarisation et l’hispanisation des Jupes. C’est ainsi que débuta, en été 1787, la construction du village de San Carlos de los Jupes sur les rives de l’Arkansas, dans l’État actuel du Colorado, mobilisant main-d’oeuvre et fonds espagnols. Or, en janvier 1788, les Jupes quittèrent le village et n’y retournèrent jamais plus. Cet essai explore la fondation et la disparition de San Carlos selon une perspective ethnohistorique. L’auteur affirme que ce village comanche éphémère était voué à l’échec, et ce, pour diverses raisons écologiques, culturelles et géostratégiques.

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45

Pimentel Gurmendi, Víctor. "CARLOS VILLALOBOS MOLINA." Devenir - Revista de estudios sobre patrimonio edificado 4, no. 7 (January 18, 2018): 5. http://dx.doi.org/10.21754/devenir.v4i7.141.

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Autodidacta en dibujo arquitectónico, artístico y técnico, intervino en la elaboración de numerosos proyectos de restauración de monumentos arqueológicos e histórico-artísticos junto con el autor de la presente nota, por ejemplo el Convento de San Francisco de Lima, la Casa Osambela (Lima), la fortaleza Real Felipe (Callao), el conjunto arqueológico Gran Pajatén (San Martín), los restos arquitectónicos de la Villa de Zaña (Lambayeque), la iglesia Conayca (Huancavelica), el Palacio del Almirante (Cusco), la casa del Inca Garcilaso de la Vega (Cusco), la Antigua Casona de San Marcos (Lima), el Monasterio de Santa Catalina (Arequipa), la iglesia de la Compañía (Arequipa), la Casa Vivanco (Ayacucho), la iglesia de la Quinua (Ayacucho), además de otros inmuebles de valor histórico-artístico de las épocas virreinal y republicana, y sitios arqueológicos de nuestro país.

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46

Pease, D. S., D. L. Stoneman, T. R. Overdier, and P. L. Smith. "Soils of the San Carlos Apaches." Soil Horizons 32, no. 3 (1991): 78. http://dx.doi.org/10.2136/sh1991.3.0078.

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47

Ramirez, Cybill Ann A., and Rizalie N. E. Mibato. "The Potential of San Carlos City, Negros Occidental as Meetings, Incentives, Conventions and Exhibitions Destination." Philippine Social Science Journal 3, no. 2 (November 10, 2020): 21–22. http://dx.doi.org/10.52006/main.v3i2.217.

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The Meetings, Incentives, Conventions, and Exhibitions (MICE) tourism is a niche segment in the tourism market that has abundant potential and is gaining significance worldwide due to the growth of business tourism. In San Carlos City, the MICE industry is not yet fully developed. The assessment of San Carlos City's potential as a MICE destination is still necessary to determine if the city has met all the essential requirements. However, the city can accommodate small local events. Hence, the paper assesses the potential of San Carlos City, Negros Occidental as Meetings, Incentives, Conventions, and Exhibitions destination. The paper also determines the stakeholders' perceived demands of San Carlos City, Negros Occidental as MICE destination in terms of business and trade, educational and scientific, sports and entertainment, and arts and cultural. Furthermore, the paper also determines the challenges and opportunities of San Carlos City as a MICE destination.

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48

Urtecho, Alvaro. "Bording House "San Antonio" de Carlos Alemán." Revista Iberoamericana 57, no. 157 (December 6, 1991): 1091–92. http://dx.doi.org/10.5195/reviberoamer.1991.4985.

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49

Romanillos, Emmanuel Luis A. "Last Decade of the Recollects in San Carlos Borromeo Parish, Negros Occidental (1965-1975)." Philippine Social Science Journal 3, no. 1 (June 22, 2020): 173–90. http://dx.doi.org/10.52006/main.v3i1.127.

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The controversial cession of San Carlos Borromeo Parish in 1975 by the Augustinian Recollects to the diocesan clergy was significant. Unknown by the present generation, the story is recalled in detail forty-five years after. Rich in primary sources and personal interviews with Recollects and diocesan priests, both protagonists, and eyewitnesses were utilized. The narrative objectively recounts the Recollect ministry in San Carlos. It then focuses on the diocesan consultors' meeting in October 1974 that sanctioned the takeover despite the lack of priests, the uninformed Recollect superiors' vicarial meeting on the reshuffle of curates in November 1974, and the persistent takeover rumors in San Carlos since October 1974. The official cession—that included Calatrava and Barangay Quezon parishes—happened on 6 January 1975. Reasons are revealed and discussed. In retrospect, the early beginnings of San Carlos and its creation as a diocese in 1988 have reminisced. Highlighted is Bishop Epifanio Surban's heartfelt gratitude for the Recollect evangelization effort.

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50

Jara Palacios, Rafael. "Dr. Carlos R. Lanfranco La Hoz." Anales de la Facultad de Medicina 60, no. 2 (April 7, 2014): 133. http://dx.doi.org/10.15381/anales.v60i2.4492.

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Ha fallecido en Lima el Dr. Carlos R. Lanfranco La Hoz, el maestro más representativo que ha tenido la Facultad de Medicina de San Fernando de la Universidad Nacional Mayor de San Marcos en los últimos cuarenta años. Fue médico y maestro universitario, hombre de ciencia, extraordinario semiólogo, gran clínico, pero sobre todo docente por naturaleza. Gremialista cuando los acontecimientos lo requerían, con gran sensibilidad por el dolor humano y ejemplo de muchas generaciones de médicos.

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Journal articles on the topic 'Olivine de San Carlos'

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