Relevant bibliographies by topics / Los Angeles Basin

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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 'Los Angeles Basin'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Los Angeles Basin"

1

Cline, Susan, and Brianna Garcia. "Brownfield Redevelopment in the Los Angeles Basin." disP - The Planning Review 36, no. 140 (2000): 23–27. http://dx.doi.org/10.1080/02513625.2000.10556730.

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Denney, Dennis. "Los Angeles Basin: New Oil From Old Fields." Journal of Petroleum Technology 49, no. 09 (1997): 982–83. http://dx.doi.org/10.2118/0997-0982-jpt.

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Harlan, Harold J. "Insects of the Los Angeles Basin. 2nd ed." Annals of the Entomological Society of America 88, no. 4 (1995): 598–99. http://dx.doi.org/10.1093/aesa/88.4.598.

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Dravinski, M., T. K. Mossessian, H. Eshraghi, and H. Kagami. "Predominant motion of the Los Angeles sedimentary basin." Engineering Analysis with Boundary Elements 8, no. 4 (1991): 206–14. http://dx.doi.org/10.1016/0955-7997(91)90015-l.

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Liu, Xin, Gregory C. Beroza, Lei Yang, and William L. Ellsworth. "Ambient noise Love wave attenuation tomography for the LASSIE array across the Los Angeles basin." Science Advances 7, no. 22 (2021): eabe1030. http://dx.doi.org/10.1126/sciadv.abe1030.

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The Los Angeles basin is located within the North America–Pacific plate boundary and contains multiple earthquake faults that threaten greater Los Angeles. Seismic attenuation tomography has the potential to provide important constraints on wave propagation in the basin and to provide supplementary information on structure in the form of the distribution of anelastic properties. On the basis of the amplitude information from seismic interferometry from the linear LASSIE array in the Los Angeles basin, we apply station-triplet attenuation tomography to obtain a 2D depth profile for the attenuation structure of the uppermost 0.6 km. The array crosses four Quaternary faults, three of which are blind. The attenuation tomography resolves strong attenuation (shear attenuation Qs ~ 20) for the fault zones and is consistent with sharp boundaries across them.
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Viatte, Camille, Thomas Lauvaux, Jacob K. Hedelius, et al. "Methane emissions from dairies in the Los Angeles Basin." Atmospheric Chemistry and Physics 17, no. 12 (2017): 7509–28. http://dx.doi.org/10.5194/acp-17-7509-2017.

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Abstract. We estimate the amount of methane (CH4) emitted by the largest dairies in the southern California region by combining measurements from four mobile solar-viewing ground-based spectrometers (EM27/SUN), in situ isotopic 13∕12CH4 measurements from a CRDS analyzer (Picarro), and a high-resolution atmospheric transport simulation with a Weather Research and Forecasting model in large-eddy simulation mode (WRF-LES). The remote sensing spectrometers measure the total column-averaged dry-air mole fractions of CH4 and CO2 (XCH4 and XCO2) in the near infrared region, providing information on total emissions of the dairies at Chino. Differences measured between the four EM27/SUN ranged from 0.2 to 22 ppb (part per billion) and from 0.7 to 3 ppm (part per million) for XCH4 and XCO2, respectively. To assess the fluxes of the dairies, these differential measurements are used in conjunction with the local atmospheric dynamics from wind measurements at two local airports and from the WRF-LES simulations at 111 m resolution. Our top-down CH4 emissions derived using the Fourier transform spectrometers (FTS) observations of 1.4 to 4.8 ppt s−1 are in the low end of previous top-down estimates, consistent with reductions of the dairy farms and urbanization in the domain. However, the wide range of inferred fluxes points to the challenges posed by the heterogeneity of the sources and meteorology. Inverse modeling from WRF-LES is utilized to resolve the spatial distribution of CH4 emissions in the domain. Both the model and the measurements indicate heterogeneous emissions, with contributions from anthropogenic and biogenic sources at Chino. A Bayesian inversion and a Monte Carlo approach are used to provide the CH4 emissions of 2.2 to 3.5 ppt s−1 at Chino.
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Hauksson, Egill. "Earthquakes, faulting, and stress in the Los Angeles Basin." Journal of Geophysical Research 95, B10 (1990): 15365. http://dx.doi.org/10.1029/jb095ib10p15365.

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Craven, J. S., A. R. Metcalf, R. Bahreini, et al. "Los Angeles Basin airborne organic aerosol characterization during CalNex." Journal of Geophysical Research: Atmospheres 118, no. 19 (2013): 11,453–11,467. http://dx.doi.org/10.1002/jgrd.50853.

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Xingxin, Du. "On shear-wave splitting in the Los Angeles basin." Pure and Applied Geophysics PAGEOPH 134, no. 2 (1990): 175–94. http://dx.doi.org/10.1007/bf00876997.

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Witiw, M. R., and Steve LaDochy. "Trends in fog frequencies in the Los Angeles Basin." Atmospheric Research 87, no. 3-4 (2008): 293–300. http://dx.doi.org/10.1016/j.atmosres.2007.11.010.

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Dissertations / Theses on the topic "Los Angeles Basin"

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Bergen, Kristian J. "Pleistocene to Modern Deformation of the Central Los Angeles Basin." Thesis, Harvard University, 2015. http://nrs.harvard.edu/urn-3:HUL.InstRepos:23845440.

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We combine the principles of sequence stratigraphy and syntectonic (growth) stratigraphy to assess deformation of the central Los Angeles (LA) basin from the late Pleistocene to the present. Sequence stratigraphy provides temporally correlative horizons that define the activity and structural kinematics of folds and underlying blind-thrust faults. Using these insights, we demonstrate that the slip rate on the western segment of the Puente Hills blind-thrust fault system (PHT), which lies directly beneath downtown Los Angeles, has accelerated from the late Pleistocene through the Holocene. This increase in slip rate implies that the magnitudes and/or the frequency of earthquakes on this fault segment have increased over time, challenging the characteristic earthquake model and presenting an evolving and potentially increasing seismic hazard to metropolitan Los Angeles. To assess the slip rate on the LA segment probabilistically, we developed a new method for estimating uncertainty in the true depths of interpreted geologic features from seismic reflection data. We achieved this by simulating the effects of varying the order and proportionality of interval velocities using an autoregression model based on nearby wellbore velocities. We further assessed the impact of resolution uncertainty on the true depth of interpreted geological features. Combined with age uncertainties for geologic horizons, this approach yields robust assessments of the slip rates on blind-thrust faults. Finally, we map temporally correlative sequence boundaries across the Los Angeles basin from the late Pleistocene to present. This enables us to determine changes in accommodation space in time and from them infer changes in deformation. Our results show persistent deepening in the central trough of the Los Angeles basin, activity of the Compton and PHT faults, and lateral growth of the LA segment of the PHT.<br>Earth and Planetary Sciences
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Wang, Haijiang. "Source-dependent variations of M7 earthquakes in the Los Angeles Basin." Diss., lmu, 2007. http://nbn-resolving.de/urn:nbn:de:bvb:19-75554.

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Lanners, Rebecca K. "Chemostratigraphy of hemipelagic facies of the montery formation and equivalent semimentary rocks, Los Angeles basin, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1527388.

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<p> The submarine-fan-dominated, proximal Los Angeles basin contains interstratified hemipelagic strata coeval with the widespread Miocene Monterey Formation that accumulated in other California margin basins. Although more detritalrich and containing greater abundance of plagioclase and muscovite than more distal, outboard basins, a four-part compositional zonation is recognized in the fine-grained facies, similar to the stratigraphic succession of the Santa Barbara coastal area. In ascending stratigraphic order, these include a basal interbedded calcareous-siliceous zone, a phosphatic zone, a calcareous-siliceous zone, and an uppermost siliceous zone. To establish these zonations, 125 samples from five wells in a north-south transect across the western basin from East and West Beverly Hills, Inglewood, and Wilmington oil fields were analyzed for bulk chemical composition by XRF and quantitative mineralogy by XRD and FTIR. The mineralogic composition of the fine-grained detrital fraction makes use of geochemical equations for sedimentary components developed elsewhere unsuitable to the Los Angeles basin.</p>
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Chavez, Jacqueline A. "Principal stress analysis of rock fracture data from the Long Beach oil field, Los Angeles basin, California." Thesis, California State University, Long Beach, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=1587889.

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<p>Twelve electric borehole-image logs from oil wells located in the Long Beach oil field were used to conduct a fracture analysis of principal stress orientations associated with the Newport-Inglewood Fault Zone. The fractures analyzed are located in the Puente, Repetto, Pico, and San Pedro formations. Fractures were grouped based on fracture type, orientation, and formation. In-situ SHmax orientation was interpreted to range between 320? to 40?. Variations form the in-situ stress were observed across every formation and interpreted as paleo-stress. The SHmax orientation begins to change from NW to N-NW in the Pico Formation, which may signal the onset of the dextral movement of the Newport-Inglewood Fault 2.5 million years ago or later. The NE SHmax orientation in the San Pedro Formation may reflect stress trajectory changes as the Newport-Inglewood Fault continues to propagate in the Pleistocene. Additional SHmax orientations indicate a more complex structural evolution of stress trajectories.
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Wu, Taia Sean. "Comparing Bulk Aerosol Profiles in the Mixed Layer in Coastal Los Angeles and the Inland Empire." Scholarship @ Claremont, 2015. http://scholarship.claremont.edu/scripps_theses/547.

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Characteristic westerly sea breeze carries air over the Los Angeles Basin in Southern California to the Inland Empire approximately 50 miles inland, directly impacting air quality in both of these two highly polluted regions. As particles play a critical role in air quality and human health, this study compares the bulk aerosol profiles of the Los Angeles pollution "source" and Inland Empire "receptor" regions during the 2013 and 2014 NASA Student Airborne Research Program (SARP) campaigns onboard the NASA DC-8 airborne laboratory. The source and receptor regions were characterized by a series of missed approaches at the Los Angeles International Airport, Long Beach Airport, and Los Alamitos Army Airfield (coastal sources) as well as the Ontario International Airport, San Bernardino International Airport, and March Air Reserve Base (inland receptors). The aerosol populations in each region were compared, and the changes evolved were analyzed alongside volatile organic compound (VOC) concentrations from Whole Air Samples. Particle size distributions were collected using a Droplet Measurement Technologies Ultra High Sensitivity Aerosol Spectrometer (DMT-UHSAS). Aerosol concentration, mass, and mode diameter increased significantly between coastal pollution source and inland pollution receptor regions in all cases, along with an increase in mode diameter. The observed changes cannot be accounted for by aerosol aging over the Los Angeles basin alone, suggesting new particle emission/formation over this region could be a dominating factor in the changes. Positive correlations between particle increases at receptor sites and anthropogenic VOC tracers will be discussed.
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Sterbis, Christopher J. "An analysis of short term mesoscale forecasts in the Los Angeles Basin using Southern Coast Ozone Study 1997 data." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2000. http://handle.dtic.mil/100.2/ADA384877.

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Thesis (M.S. in Meteorology and Physical Oceanography) Naval Postgraduate School, Sept. 2000.<br>Thesis advisor(s): Miller, Douglas K. Includes bibliographical references (p. 99-100). Also available online.
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Zhang, Xiaolu. "The sources, formation and properties of soluble organic aerosols: results from ambient measurements in the southeastern united states and the los angeles basin." Diss., Georgia Institute of Technology, 2012. http://hdl.handle.net/1853/44894.

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900 archived FRM filters from 15 sites over the southeast during 2007 were analyzed for PM2.5 chemical composition and physical properties. Secondary components (i.e. sulfate aerosol and SOA) were the major contributors to the PM2.5 mass over the southeast, whereas the contribution from biomass burning varied with season and was negligible (2%) during summer. Excluding biomass burning influence, FRM WSOC was spatially homogeneous throughout the region, similar to sulfate, yet WSOC was moderately enhanced in locations of greater predicted isoprene emissions in summer. On smaller spatial scale, a substantial urban/rural gradient of WSOC was found through comparisons of online WSOC measurements at one urban/rural pair (Atlanta/Yorkville) in August 2008, indicating important contribution from anthropogenic emissions. A comparative study between Atlanta and LA reveals a number of contrasting features between two cities. WSOC gas-particle partitioning, investigated through the fraction of total WSOC in the particle phase, Fp, exhibited differing relationships with ambient RH and organic aerosols. In Atlanta, both particle water and organic aerosol (OA) can serve as an absorbing phase. In contrast, in LA the aerosol water was not an important absorbing phase, instead, Fp was correlated with OA mass. Fresh LA WSOC had a consistent brown color and a bulk absorption per soluble carbon mass at 365 nm that was 4 to 6 times higher than freshly-formed Atlanta soluble organic carbon. Interpreting soluble brown carbon as a property of freshly-formed anthropogenic SOA, the difference in absorption per carbon mass between the two cities suggests most WSOC formed within Atlanta is not from an anthropogenic process similar to LA.
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Oskin, Michael Eugene Stock J. M. "Tectonic evolution of the northern Gulf of California, Mexico, deduced from conjugate rifted margins of the upper Delfin Basin [Part I]. : Active folding and seismic hazard in central Los Angeles, California [Part II] /." Diss., Pasadena, Calif. : California Institute of Technology, 2002. http://resolver.caltech.edu/CaltechETD:etd-11252001-103911.

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Ullrich, Angela [Verfasser]. "Evidenzbasierte Diagnostik phonologischer Störungen : Entwicklung und Evaluation eines Sprachanalyseverfahrens auf der Basis nichtlinearer phonologischer Theorien / Angela Ullrich." Köln : Universitäts- und Stadtbibliothek Köln, 2011. http://d-nb.info/1013735994/34.

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Schillaci, Guido [Verfasser], Verena V. [Akademischer Betreuer] Hafner, Bruno [Akademischer Betreuer] Lara, and Angelo [Akademischer Betreuer] Cangelosi. "Sensorimotor learning and simulation of experience as a basis for the development of cognition in robotics / Guido Schillaci. Gutachter: Verena V. Hafner ; Bruno Lara ; Angelo Cangelosi." Berlin : Humboldt Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät II, 2014. http://d-nb.info/1049249089/34.

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Books on the topic "Los Angeles Basin"

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Insects of the Los Angeles basin. 2nd ed. Natural History Museum of Los Angeles County, 1993.

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Patrick, Robert L. A critical look at earthquake preparations in the Los Angeles Basin. Rand Corp., 1990.

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Hillhouse, John W. Probing the Los Angeles Basin: Insights into ground-water resources and earthquake hazards. U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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1937-, Adams Robert, ed. California: Views by Robert Adams of the Los Angeles Basin, 1978-1983 : essay. Fraenkel Gallery, 2000.

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California. Legislature. Assembly. Select Committee on the Americas. Hearing/roundtable discussion: Regionalism, the Greater Los Angeles Basin Region Agreement, and the Power in Regional Partnership Agreement. Assembly Publications Office, 1995.

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Sterbis, Christopher J. An analysis of short term mesoscale forecasts in the Los Angeles Basin using Southern Coast Ozone Study 1997 data. Naval Postgraduate School, 2000.

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Mathany, Timothy M. Ground-water quality data in the coastal Los Angeles basin study unit, 2006: Results from the California GAMA Program. U.S. Dept. of the Interior, U.S. Geological Survey, 2008.

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Mathany, Timothy M. Ground-water quality data in the coastal Los Angeles basin study unit, 2006: Results from the California GAMA Program. U.S. Dept. of the Interior, U.S. Geological Survey, 2008.

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Mathany, Timothy M. Ground-water quality data in the coastal Los Angeles basin study unit, 2006: Results from the California GAMA Program. U.S. Dept. of the Interior, U.S. Geological Survey, 2008.

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Mathany, Timothy M. Ground-water quality data in the coastal Los Angeles basin study unit, 2006: Results from the California GAMA Program. U.S. Dept. of the Interior, U.S. Geological Survey, 2008.

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Book chapters on the topic "Los Angeles Basin"

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Gidman, June, Will J. Schweller, Chris W. Grant, and Alan A. Reed. "Reservoir Character of Deep Marine Sandstones, Inglewood Field, Los Angeles Basin." In Frontiers in Sedimentary Geology. Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4757-0160-9_11.

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Robinson, Sherman, Shankar Subramanian, and Jacqueline Geoghegan. "Modeling Air Pollution Abatement in a Market-Based Incentive Framework for the Los Angeles Basin." In Economic Instruments for Air Pollution Control. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-1012-9_3.

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Glasscoe, Margaret T., Andrea Donnellan, Louise H. Kellogg, and Gregory A. Lyzenga. "Evidence of Strain Partitioning Between the Sierra Madre Fault and the Los Angeles Basin, Southern California from Numerical Models." In Computational Earthquake Science Part II. Birkhäuser Basel, 2004. http://dx.doi.org/10.1007/978-3-0348-7875-3_16.

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Schwartz, Shalom H. "Basic values: How they motivate and inhibit prosocial behavior." In Prosocial motives, emotions, and behavior: The better angels of our nature. American Psychological Association, 2010. http://dx.doi.org/10.1037/12061-012.

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Skillin, R. H. "Monterey development—Onshore and offshore Santa Maria basins." In Oil in the Monterey California Formation Los Angeles to Santa Maria, California July 20-24, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft311p0041.

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Pytte, M. H. "Organic geochemistry of the Miocene Monterey and equivalent formations in five California basins." In Oil in the Monterey California Formation Los Angeles to Santa Maria, California July 20-24, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft311p0033.

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Miller, Paul R., L. I. de Bauer, and Tomás Hernández-Tejeda. "Oxidant Exposure and Effects on Pines in Forests in the Mexico City and Los Angeles, California, Air Basins." In Ecological Studies. Springer New York, 2002. http://dx.doi.org/10.1007/978-0-387-22520-3_9.

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Rapanta, Chrysi, and Susana Trovão. "Intercultural Education for the Twenty-First Century: A Comparative Review of Research." In Dialogue for Intercultural Understanding. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71778-0_2.

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AbstractBased on the assumption that globalization should not imply homogenization, it is important for education to promote dialogue and intercultural understanding. The first appearance of the term ‘intercultural education’ in Europe dates back to 1983, when European ministers of education at a conference in Berlin, in a resolution for the schooling of migrant children, highlighted the intercultural dimension of education (Portera in Intercultural Education 19:481–491, 2008). One of the mandates of intercultural education is to promote intercultural dialogue, meaning dialogue that is “open and respectful” and that takes place between individuals or groups “with different ethnic, cultural, religious and linguistic backgrounds and heritage on the basis of mutual understanding and respect” (Council of Europe in White paper on intercultural dialogue: Living together as equals in dignity. Council of Europe, Strasbourg, p. 10, 2008). Such backgrounds and heritages form cultural identities, not limited to ethnic, religious and linguistic ones, as culture is a broader concept including several layers such as “experience, interest, orientation to the world, values, dispositions, sensibilities, social languages, and discourses” (Cope and Kalantzis in Pedagogies: An International Journal 4:173, 2009). As cultural identities are multi-layered, so is cultural diversity, and therefore it becomes a challenge for educators and researchers to address it (Hepple et al. in Teaching and Teacher Education 66:273–281, 2017). Referring to Leclercq (The lessons of thirty years of European co-operation for intercultural education, Steering Committee for Education, Strasbourg, 2002), Hajisoteriou and Angelides (International Journal of Inclusive Education 21:367, 2017) argue that “intercultural education aims to stress the dynamic nature of cultural diversity as an unstable mixture of sameness and otherness.” This challenge relates to the dynamic concept of culture itself, as socially constructed, and continuously shaped and reshaped through communicative interactions (Holmes et al. in Intercultural Education 26:16–30, 2015).
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Hernández, Kelly Lytle. "An Eliminatory Option." In City of Inmates. University of North Carolina Press, 2017. http://dx.doi.org/10.5149/northcarolina/9781469631189.003.0002.

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The first chapter begins many millennia ago when the region now called the Los Angeles Basin was solely occupied by the Indigenous communities today collectively known as the Tongva-Gabrielino Tribe. This story is vital because there is no evidence that Tongva-Gabrielino communities ever tried or experienced human caging until the Spanish Crown dispatched a small group of colonists to establish El Pueblo de Nuestra Senora la Reina de Los Angeles del Rio Porciuncula, the City of Angels, in 1781. One of the first structures these colonists built was a jail. In time, the colonists and their descendants filled the jail with indios. Throughout the next century of colonial occupation in the Tongva Basin—spanning the Spanish colonial period (1781–1821), the Mexican era (1821–48), and the early years of U.S. rule (1848–70s)—Indigenous peoples consistently comprised a substantive, if not majority, portion of the incarcerated population in Los Angeles. Chapter 1, therefore, firmly grounds the origins of incarceration in Los Angeles with the dynamics of conquest and colonialism in the Tongva Basin.
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Biddle, Kevin T. "Chapter 1 The Los Angeles Basin An Overview." In Active Margin Basins. American Association of Petroleum Geologists, 1991. http://dx.doi.org/10.1306/m52531c1.

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Conference papers on the topic "Los Angeles Basin"

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Hill, James M. "Los Angeles Basin, New Oil from Old Fields." In SPE Western Regional Meeting. Society of Petroleum Engineers, 1997. http://dx.doi.org/10.2118/38330-ms.

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Cook, S., K. Batbayar, and Z. Printz. "Carbon Storage Potential in the Los Angeles Basin." In 1st Geoscience & Engineering in Energy Transition Conference. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202021024.

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Evans, B. L., R. P. Sailor, and E. Santiago. "Well Abandonment in the Los Angeles Basin: A Primer." In SPE Western Regional/AAPG Pacific Section Joint Meeting. Society of Petroleum Engineers, 2003. http://dx.doi.org/10.2118/83443-ms.

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Dayvault, G. P. "Injection Profile Control in a Multizone Los Angeles Basin Waterflood." In SPE California Regional Meeting. Society of Petroleum Engineers, 1990. http://dx.doi.org/10.2118/20044-ms.

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Assimaki, Dominic, Wei Li, Jamison M. Steidl, and Jan Schmedes. "Modeling Nonlinear Site Response Uncertainty in the Los Angeles Basin." In Geotechnical Earthquake Engineering and Soil Dynamics Congress IV. American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40975(318)18.

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Dayvault, G. P., and D. E. Patterson. "Solvent and Acid Stimulation Increase Production in Los Angeles Basin Waterflood." In SPE California Regional Meeting. Society of Petroleum Engineers, 1989. http://dx.doi.org/10.2118/18816-ms.

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Swanson, Glenn S., and Iraj Ershaghi. "Water Control Problems and Solutions-Los Angeles Basin Statistics and Case Histories." In SPE Western Regional Meeting. Society of Petroleum Engineers, 2005. http://dx.doi.org/10.2118/94003-ms.

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Gidman, June, A. E. (Pat) Worthington, and George H. Newman. "Well‐site handling of poorly consolidated core, Inglewood Field, Los Angeles Basin." In SEG Technical Program Expanded Abstracts 1987. Society of Exploration Geophysicists, 1987. http://dx.doi.org/10.1190/1.1892113.

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Withers, Brian, Phil Bolin, Shinichiro Nakauchi, et al. "Gas insulated switchgear developed to meet increased load demand in Los Angeles Basin." In IEEE PES T&D 2010. IEEE, 2010. http://dx.doi.org/10.1109/tdc.2010.5484709.

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Paul, D. L., R. Asaithambi, I. Ershaghi, J. Crompton, and D. Gautier. "Energy Security in the Los Angeles Basin: A New Look at an Old Treasure." In SPE Western Regional Meeting. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/174029-ms.

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Reports on the topic "Los Angeles Basin"

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Davisson, M. L., Gp Eaton, G. B. Hudson, and C. Koester. Tracing and age-dating injected groundwater of the west basin barrier project, Los Angeles, CA. Office of Scientific and Technical Information (OSTI), 1999. http://dx.doi.org/10.2172/9653.

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Taha, Haider. Potential impacts of climate change on tropospheric ozone in California: a preliminary episodic modeling assessment of the Los Angeles basin and the Sacramento valley. Office of Scientific and Technical Information (OSTI), 2001. http://dx.doi.org/10.2172/781837.

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Hashemian, Hassan. Infrastructure Academy Transportation Program. Mineta Transportation Institute, 2021. http://dx.doi.org/10.31979/mti.2021.1919.

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The College of Engineering, Computer Science, and Technology at the California State University, Los Angeles has expanded its National Summer Transportation Institute into a year-long program by creating the Infrastructure Academy Transportation Program (IATP). The goal of this program is to build a pipeline of diverse, well qualified young people for the transportation industry. The program works with high school students and teachers to offer academic courses, basic skills, workforce readiness training, internships, extracurricular activities, and career placements to prepare students and place them into the Science, Technology, Engineering, and Math (STEM) College track. The academy emphasizes on transportation as an industry sector and aims to increase the number of underrepresented minorities and women who directly enter the transportation workforce. It also aims at increasing the number of young people who enter college to study engineering or technology and subsequently pursue careers in transportation- and infrastructure-related careers. The IATP was conducted as a full-year program with 30 student participants from high schools.
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Low-Level Volatile Organic Compounds in Active Public Supply Wells as Ground-Water Tracers in the Los Angeles Physiographic Basin, California, 2000. US Geological Survey, 2001. http://dx.doi.org/10.3133/wri20014188.

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Water-quality changes and organic-carbon characterization during recharge with recycled water at a research basin in Montebello Forebay, Los Angeles County, California, 1991-1996. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034146.

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Geohydrology, Geochemistry, and Ground-Water Simulation-Optimization of the Central and West Coast Basins, Los Angeles County, California. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034065.

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