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Littérature scientifique sur le sujet « And tectonics »

Auteur : Grafiati
Publié le 10 mars 2023

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Articles de revues sur le sujet "And tectonics"

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Stern, Robert J. « The evolution of plate tectonics ». Philosophical Transactions of the Royal Society A : Mathematical, Physical and Engineering Sciences 376, no 2132 (octobre 2018) : 20170406. http://dx.doi.org/10.1098/rsta.2017.0406.

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To understand how plate tectonics became Earth's dominant mode of convection, we need to address three related problems. (i) What was Earth's tectonic regime before the present episode of plate tectonics began? (ii) Given the preceding tectonic regime, how did plate tectonics become established? (iii) When did the present episode of plate tectonics begin? The tripartite nature of the problem complicates solving it, but, when we have all three answers, the requisite consilience will provide greater confidence than if we only focus on the long-standing question of when did plate tectonics begin? Earth probably experienced episodes of magma ocean, heat-pipe, and increasingly sluggish single lid magmatotectonism. In this effort we should consider all possible scenarios and lines of evidence. As we address these questions, we should acknowledge there were probably multiple episodes of plate tectonic and non-plate tectonic convective styles on Earth. Non-plate tectonic styles were probably dominated by ‘single lid tectonics’ and this evolved as Earth cooled and its lithosphere thickened. Evidence from the rock record indicates that the modern episode of plate tectonics began in Neoproterozoic time. A Neoproterozoic transition from single lid to plate tectonics also explains kimberlite ages, the Neoproterozoic climate crisis and the Neoproterozoic acceleration of evolution. This article is part of a discussion meeting issue ‘Earth dynamics and the development of plate tectonics’.
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Lenardic, A. « The diversity of tectonic modes and thoughts about transitions between them ». Philosophical Transactions of the Royal Society A : Mathematical, Physical and Engineering Sciences 376, no 2132 (octobre 2018) : 20170416. http://dx.doi.org/10.1098/rsta.2017.0416.

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Plate tectonics is a particular mode of tectonic activity that characterizes the present-day Earth. It is directly linked to not only tectonic deformation but also magmatic/volcanic activity and all aspects of the rock cycle. Other terrestrial planets in our Solar System do not operate in a plate tectonic mode but do have volcanic constructs and signs of tectonic deformation. This indicates the existence of tectonic modes different from plate tectonics. This article discusses the defining features of plate tectonics and reviews the range of tectonic modes that have been proposed for terrestrial planets to date. A categorization of tectonic modes relates to the issue of when plate tectonics initiated on Earth as it provides insights into possible pre-plate tectonic behaviour. The final focus of this contribution relates to transitions between tectonic modes. Different transition scenarios are discussed. One follows classic ideas of regime transitions in which boundaries between tectonic modes are determined by the physical and chemical properties of a planet. The other considers the potential that variations in temporal evolution can introduce contingencies that have a significant effect on tectonic transitions. The latter scenario allows for the existence of multiple stable tectonic modes under the same physical/chemical conditions. The different transition potentials imply different interpretations regarding the type of variable that the tectonic mode of a planet represents. Under the classic regime transition view, the tectonic mode of a planet is a state variable (akin to temperature). Under the multiple stable modes view, the tectonic mode of a planet is a process variable. That is, something that flows through the system (akin to heat). The different implications that follow are discussed as they relate to the questions of when did plate tectonics initiate on Earth and why does Earth have plate tectonics. This article is part of a discussion meeting issue ‘Earth dynamics and the development of plate tectonics’.
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Widjaja, M.T., Robert Rianto. « TANTANGAN TEKTONIKA DIGITAL ». JoDA Journal of Digital Architecture 2, no 1 (25 novembre 2022) : 29–36. http://dx.doi.org/10.24167/joda.v2i1.5547.

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The rapid development of digital technology has an impact on the ease of processing mass forms and the appearance of buildings in architecture. This significantly influenced tectonics as an important part of architecture. Tectonics is like finding a new window of view from the same existence. This situation demands an explanation of the position and role of tectonics in contemporary architectural works. This explanation is very important to rediscover the nature of tectonics as an art of construction in the new face of digital technology. This paper will examine the classical tectonic discourse that has developed from the core form and art form to the understanding of ontology and representation which is the beginning of the discussion of digital tectonics. Through a study of several relevant cases, it can be found that epistemologically, digital tectonic still has the same nature as classical tectonic. The difference lies in the richness of the quality and richness of the truth representation which implicitly gives birth to hidden truth conditions in digital tectonic representations. The existence of this hidden truth poses a challenge for digital tectonics to survive as the art of construction.
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Brown, Michael, Tim Johnson et Nicholas J. Gardiner. « Plate Tectonics and the Archean Earth ». Annual Review of Earth and Planetary Sciences 48, no 1 (30 mai 2020) : 291–320. http://dx.doi.org/10.1146/annurev-earth-081619-052705.

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If we accept that a critical condition for plate tectonics is the creation and maintenance of a global network of narrow boundaries separating multiple plates, then to argue for plate tectonics during the Archean requires more than a local record of subduction. A case is made for plate tectonics back to the early Paleoproterozoic, when a cycle of breakup and collision led to formation of the supercontinent Columbia, and bimodal metamorphism is registered globally. Before this, less preserved crust and survivorship bias become greater concerns, and the geological record may yield only a lower limit on the emergence of plate tectonics. Higher mantle temperature in the Archean precluded or limited stable subduction, requiring a transition to plate tectonics from another tectonic mode. This transition is recorded by changes in geochemical proxies and interpreted based on numerical modeling. Improved understanding of the secular evolution of temperature and water in the mantle is a key target for future research. ▪ Higher mantle temperature in the Archean precluded or limited stable subduction, requiring a transition to plate tectonics from another tectonic mode. ▪ Plate tectonics can be demonstrated on Earth since the early Paleoproterozoic (since c. 2.2 Ga), but before the Proterozoic Earth's tectonic mode remains ambiguous. ▪ The Mesoarchean to early Paleoproterozoic (3.2–2.3 Ga) represents a period of transition from an early tectonic mode (stagnant or sluggish lid) to plate tectonics. ▪ The development of a global network of narrow boundaries separating multiple plates could have been kick-started by plume-induced subduction.
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Chandra ; Jonathan Hans Yoas Sihotang, Jansen. « SOPO BATAK TOBA RESILIENCE TECTONICS TOWARD EARTHQUAKE STUDY OBJECT : SOPO NAGARI SIHOTANG ». Riset Arsitektur (RISA) 3, no 03 (5 juillet 2019) : 222–39. http://dx.doi.org/10.26593/risa.v3i03.3333.222-239.

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Abstract- Sopo is a granary house in traditional Batak Toba architecture. Sopo is important for Batak Toba community because it serves as a place to store rice which is the source of life. Nowadays sopo is harder to find than ruma. Most of the sopo has transformed into Batak Toba house and uses as a residence. Sopo is located in Lake Toba, North Sumatra, which is prone to earthquakes. Sopo Nagari Sihotang was built in the 1920s and has experienced many earthquakes, now the sopo still survive without any structural damage. The resistance of the sopo over the years proves the sopo resilience to earthquakes. From the evidence of resilience to earthquake, its interesting to investigate the tectonics of this sopo. The purpose of the research is to understand the tectonic of Sopo Nagari Sihotang that resilience to earthquake and find local wisdom in facing earthquake disaster.The research used descriptive method with qualitative approach by describing the existing state of Sopo Nagari Sihotang and comparing it with tectonic theory and earthquake resistant structure. The sopo’s data were collected by field observation and literature study. The data are grouped into four parts, namely construction, detail, space, and ornaments that become points for analysis of tectonics. Tectonic analysis is associated with the theory of earthquake resistant structures to find out what makes tectonic of the sopo resilient to earthquakes.The result is the tectonic resilience of the Sopo Nagari Sihotang to earthquakes are found in the tectonics construction in the use of materials; tectonics detail on vertical structures and horizontal structures; and tectonics space at the story height – the activity, the spatial form – the building hape, the spatial form - the structure, and the activity - the structure. The tectonic resilience of Sopo Nagari Sihotang to earthquakes is not found in the tectonics construction and tectonics ornament. The local wisdom which are the main factors make the sopo resilience to earthquake are found on, the tectonics detail of the sopo post-batu ojahan can retain the sopo by relying on the frictional force resulting from self-weight of the sopo; the tectonics detail of the sopo post-ransang can bind every sopo posts; the use of lightweight wood materials thus reducing inertia forces. Key Words: resilience, tectonics, sopo, earthquake, Batak Toba
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MUSUMECI, DANIELE, STEFANO BRANCA et LUIGI INGALISO. « MAGMATOLOGICAL TECTONICS : ALFRED RITTMANN’S PARADIGM ». Earth Sciences History 40, no 1 (1 janvier 2021) : 266–81. http://dx.doi.org/10.17704/1944-6187-40.1.261.

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ABSTRACT The aim of this research is to present the life and research of Alfred Rittmann (1893–1980). He was an Earth scientist in the broadest sense: a petrographer, mineralogist, magmatologist, tectonist, geodynamicist, planetologist, volcanologist and, what is more, a philosopher of geosciences. He is considered the founder of contemporary, volcanology by combining in his interdisciplinary research the study of volcanic phenomena at the surface with tectonic activity and magmatology. In his books, Rittmann discussed the first correlations between volcanism and tectonics; his geodynamic model comprises complex studies of geology, volcanology, magmatology and geodynamics. We propose to name his scientific worldview ‘Magmatological Tectonics’ (MT) and to describe it as a Kuhnian paradigm. The leading concept of all geological processes is the fundamental law. Rittmann also made abundant use of Chamberlin’s method, the method of multiple working hypotheses. Some brief interpretations will be proposed regarding the importance of Rittmann in the history of geosciences in the twentieth century and the emergence of some philosophical problems deriving from this research.
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O'Neill, Craig, Simon Turner et Tracy Rushmer. « The inception of plate tectonics : a record of failure ». Philosophical Transactions of the Royal Society A : Mathematical, Physical and Engineering Sciences 376, no 2132 (octobre 2018) : 20170414. http://dx.doi.org/10.1098/rsta.2017.0414.

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The development of plate tectonics from a pre-plate tectonics regime requires both the initiation of subduction and the development of nascent subduction zones into long-lived contiguous features. Subduction itself has been shown to be sensitive to system parameters such as thermal state and the specific rheology. While generally it has been shown that cold-interior high-Rayleigh-number convection (such as on the Earth today) favours plates and subduction, due to the ability of the interior stresses to couple with the lid, a given system may or may not have plate tectonics depending on its initial conditions. This has led to the idea that there is a strong history dependence to tectonic evolution—and the details of tectonic transitions, including whether they even occur, may depend on the early history of a planet. However, intrinsic convective stresses are not the only dynamic drivers of early planetary evolution. Early planetary geological evolution is dominated by volcanic processes and impacting. These have rarely been considered in thermal evolution models. Recent models exploring the details of plate tectonic initiation have explored the effect of strong thermal plumes or large impacts on surface tectonism, and found that these ‘primary drivers’ can initiate subduction, and, in some cases, over-ride the initial state of the planet. The corollary of this, of course, is that, in the absence of such ongoing drivers, existing or incipient subduction systems under early Earth conditions might fail. The only detailed planetary record we have of this development comes from Earth, and is restricted by the limited geological record of its earliest history. Many recent estimates have suggested an origin of plate tectonics at approximately 3.0 Ga, inferring a monotonically increasing transition from pre-plates, through subduction initiation, to continuous subduction and a modern plate tectonic regime around that time. However, both numerical modelling and the geological record itself suggest a strong nonlinearity in the dynamics of the transition, and it has been noted that the early history of Archaean greenstone belts and trondhjemite–tonalite–granodiorite record many instances of failed subduction. Here, we explore the history of subduction failure on the early Earth, and couple these with insights from numerical models of the geodynamic regime at the time. This article is part of a discussion meeting issue ‘Earth dynamics and the development of plate tectonics'.
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Barnes, Gina L. « Tectonic Archaeology as a Foundation for Geoarchaeology ». Land 10, no 5 (23 avril 2021) : 453. http://dx.doi.org/10.3390/land10050453.

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This article proposes a new subdiscipline, Tectonic Archaeology, based on the efforts of Japanese archaeologists to deal with the effects of earthquakes, volcanic tephra cover, and tsunami on archaeological sites. Tectonic Archaeology is conceived as an umbrella term for those efforts and as a foundation for Geoarchaeology in general. Comparisons distinguish between Geoarchaeology and Tectonic Archaeology, and a survey of major archaeological journals and textbooks reveals how the concept of ‘tectonics’ and specifically the processes of Plate Tectonics have been treated. Al-though the term ‘tectonics’ occurred fairly frequently, particularly as affecting coastlines and sea levels, it was not thoroughly defined and discussed. Volcanic activity was most mentioned in journals due to its provision of resources and modification of the landscape, while the 2011 earthquake and tsunami in Japan seems to have stimulated more studies in Archaeoseismology. The textbooks were found to have scattered references to Plate Tectonic processes but no clear approach tying these together. The major exception is the Encyclopedia of Archaeology which addresses volcanoes, Archaeoseismology, and tsunami—soon to be linked together vis à vis Earth processes. Tectonic Archaeology attempts first to explain the processes of Plate Tectonics to underwrite investigation of their effects; it is applicable worldwide, in continental and coastal contexts.
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Hansen, Vicki L. « Global tectonic evolution of Venus, from exogenic to endogenic over time, and implications for early Earth processes ». Philosophical Transactions of the Royal Society A : Mathematical, Physical and Engineering Sciences 376, no 2132 (octobre 2018) : 20170412. http://dx.doi.org/10.1098/rsta.2017.0412.

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Venus provides a rich arena in which to stretch one's tectonic imagination with respect to non-plate tectonic processes of heat transfer on an Earth-like planet. Venus is similar to Earth in density, size, inferred composition and heat budget. However, Venus' lack of plate tectonics and terrestrial surficial processes results in the preservation of a unique surface geologic record of non-plate tectonomagmatic processes. In this paper, I explore three global tectonic domains that represent changes in global conditions and tectonic regimes through time, divided respectively into temporal eras. Impactors played a prominent role in the ancient era, characterized by thin global lithosphere. The Artemis superstructure era highlights sublithospheric flow processes related to a uniquely large super plume. The fracture zone complex era, marked by broad zones of tectonomagmatic activity, witnessed coupled spreading and underthrusting, since arrested. These three tectonic regimes provide possible analogue models for terrestrial Archaean craton formation, continent formation without plate tectonics, and mechanisms underlying the emergence of plate tectonics. A bolide impact model for craton formation addresses the apparent paradox of both undepleted mantle and growth of Archaean crust, and recycling of significant Archaean crust to the mantle. This article is part of a discussion meeting issue ‘Earth dynamics and the development of plate tectonics’.
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Ruban, Dmitry A., Anna V. Mikhailenko et Vladimir A. Ermolaev. « Tectonics-Related Geosites : Towards Accurate Nomenclature ». Geosciences 9, no 6 (22 juin 2019) : 275. http://dx.doi.org/10.3390/geosciences9060275.

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Accurate nomenclature of geological heritage sites (geosites) is necessary to facilitate their description and territorial geodiversity evaluation (both important for sustainable development and efficient land-use planning). As suggested by previous geological heritage studies, tectonics-related geosites are termed differently and, chiefly, provisionally (e.g., as tectonic geosites or structural geosites). Moreover, the nomenclature should take into account modern advances in the understanding of some basic tectonic phenomena. We propose abandoning the separation of structural, neotectonic, and seismic types of geosites and replacing with a single tectonic type. This can be further subdivided into subtypes, although one should consider the complexities in the links between tectonic and other geological phenomena (e.g., unique seismic features are essentially tectonic, but these can be expressed via geomorphological or sedimentary features—a geosite retains tectonic and geomorphological/sedimentary types in this case). The development of accurate nomenclature of tectonics-related geosites requires debates by experts in geological heritage.
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Thèses sur le sujet "And tectonics"

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Scarmack, Emma E. « Tectonics Today : A Paradigm Shift in Tectonic Thinking ». University of Cincinnati / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1306502946.

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Anderson, Phillip. « THE PROTEROZOIC TECTONIC EVOLUTION OF ARIZONA (PRECAMBRIAN, PLATE TECTONICS, VOLCANIC, STRATIGRAPHY) ». Diss., The University of Arizona, 1986. http://hdl.handle.net/10150/183853.

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Archean tectonics are irreconcilable with modern plate tectonics without clearly understanding Proterozoic tectonic accretionary prosesses. Arizona best displays a convergent margin where Proterozoic accretion to an Archean craton generated a new Proterozoic crust from 1800 to 160 Ma. This 12 year study independently formulated a definitive understanding of Arizona's Proterozoic tectonic evolution with new lithologic, petrologic, geochemical, structural and relative age data, and extensive new mapping. The Northwest Gneiss Belt contains an early Proterozoic arkosic clastic wedge at the Wyoming Archean edge, but only intraoceanic elements--Antler-Valentine and Bagdad volcanic belts--on Proterozoic oceanic crust south of the wedge. The Central Volcanic Belt evolved diachronously on oceanic crust: 1800-1750 Ma formative volcanism (Bradshaw Mountain, Mayer, Ash Creek and Black Canyon Creek Groups) stepped SE to form the Prescott-Jerome island arc above a SE-dipping subduction zone; a 1740 Ma NW subduction flip accreted the arc to the Archean craton, evolved I-type plutons of NW alkali-enrichment opposit to arc tholeiites, and formed calc-alkaline Union Hills Group volcanics at the southeast arc front. Except for hiatal Alder Group deposition in structural troughs, the central magmatic arc emerged as the trench stepped southeastward across SE Arizona with flattening of subduction, growth of the Pinal Schist fore-arc basin, 1700 Ma accretion of the Dos Cabenzas arc to the margin, eruption of felsic ignimbrite fans across the central arc front, and Mazatzal Group shallow marine sedimentation across the emergent arc. Proterozoic plate tectonics were subtly different from modern plate tectonics, producing oceanic crust, island arcs and other features very different in detail from modern and Archean analogs. The Proterozoic Plate Tectonic Style warrants clear distinction from those of other eras. This study establishes for Arizona an extensive, accurate and new Proterozoic data base, for central Arizona a detailed relative chronology surpassing isotopic resolution, and a new formal stratigraphic framework to be the foundation for future studies. This dissertation is superceded by a new book on Arizona's Proterozoic Tectonic Evolution, published by the Precambrian Research Institute, 810 Owens Lane, Payson, Arizona, 85541.
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Tsamis, Alexandros 1976. « Software tectonics ». Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/77777.

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Thesis (Ph. D. in Design and Computation)--Massachusetts Institute of Technology, Dept. of Architecture, 2012.
Cataloged from PDF version of thesis.
Includes bibliographical references (p. 365-370).
The resent shift of attention in the architectural discourse towards issues of ecological design, coupled with the undeniable role of computation, has already cast a new operative role to the notion of environment. Instead of being the passive, conceptualized or historicized context of an architectural object, environment is quite literally becoming the object of design itself. We are moving away from the imposed-preconceived Cartesian object which negotiates through its boundaries its presence within its immediate context. The discipline is already considering an architecture in which architectural form is only an instance of a designed environment. In many respects, this new understanding of environment aspires to be actively designed as a closed system of constant transformation, an autonomous milieu of exchange at all scales and all levels between substances, properties or qualities. The object of investigation in Software Tectonics is how technologies of design and construction allow newly forming propositions about the role of environment in the discipline to become operational tactics in the design practice. SOFTWARE TECTONICS proposes 3 design research projects. VSpace is a computer drawing application for designers. Unlike traditional CAD systems that work primarily by representing boundaries (B-reps), VSpace derives form by the representation and direct manipulation of properties (P-reps) in space. Boundaries and Properties here are considered simultaneously in the same design environment. Castit is a multi axis, Computer Numerically Controlled device that prints 3D objects by dynamically mixing at least two distinct but chemically compatible materials. Dynamic mixing allows for gradient transitions between two or more materials, resulting in objects with anisotropic material properties. CHUNK aims to eliminate a joint as a third mediating member between two building elements with an area of gradient transition. Conceived as a "dynamic insulation" architectural skin, this building technology project challenges the multi-trade and multi-component tectonics of dominant late-industrial building manufacture.
by Alexandros Tsamis.
Ph.D.in Design and Computation
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Costanza, David (David Nicholas). « Fibrous tectonics ». Thesis, Massachusetts Institute of Technology, 2015. http://hdl.handle.net/1721.1/97378.

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Thesis: S.M., Massachusetts Institute of Technology, Department of Architecture, 2015.
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 152-153).
The inherent possibilities of composites present an exciting frontier in architecture that has remained largely untapped. In light of the current computational capacities and new digital tools in manufacturing, composites are just beginning to re-situate themselves in the field of architecture. Efficiency and durability coupled with a load bearing capacity make a strong case for the use of composites as a primary building material. We now possess the computational and digital manufacturing tools that make the development of a composite building viable.On a holistic level, the research has concerned itself with an overarching focus on developing a composite building which minimizes the required costs and labor while simultaneously creating the potential for customized forms. Based on the concepts of mass customization, when the workflow from digital conception to digital production is seamless, a variety of composite structures can be produced at no greater expense. This potential for an efficient "one off" composite architecture empowered by digital manufacturing and computation, is where the research is positioned At present, the research has been focused on exploring surface composite structures through a reinvention of the 'mold'. This approach has involved using inflated bladders, rather than traditional molds of milled foam or aluminum in order to produce composite structures. In doing so, the benefits of inflatables are all encompassing. Not only do they allow for inexpensive transportation and rapid deployment, but they also lend themselves to the production of large scale structures through the simple use of air and pressure, thus minimizing both material and effort. This lies in stark contrast to traditional composite manufacturing techniques which require molds to be milled out of solid aluminum blocks or high density foam volumes, whereas inflatable molds are easily heat seamed and inflated. When considering issues of scalability, traditional molding techniques demand significantly more labor, material, and with that, overarching costs. Inflatable molds however, require only more air. Coupled with the rethinking of molding techniques is a consideration in the technological methodologies in order to produce such composite structures. The research looks to the new developments in the composite industry, such as Resin Transfer Molding (RTM) and Vacuum Assisted Resin Transfer Molding (VARTM). These processes greatly simplify the manufacturing of composites and eliminate much of the manual labor traditionally associated with composite structures. By taking advantage of the existing vacuum bag used for compaction while producing composites, the VARTM process pulls resin through the bag under vacuum pressure, thus wetting out the fibers and eliminating typical layup deficiencies while producing a nearly weightless composite structure.
by David Costanza.
S.M.
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Ngala, Umar Jibrin. « 4 D Delta Tectonics : Tectonic Evolution of the Deepwater South Central Niger Delta ». Thesis, Royal Holloway, University of London, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.498744.

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Bayasgalan, Amgalan. « Active tectonics of Mongolia ». Thesis, University of Cambridge, 1999. https://www.repository.cam.ac.uk/handle/1810/251670.

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McClay, K. R. « Structural geology and tectonics / ». Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SD/09sdm126.pdf.

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Goldsworthy, Mary. « Active tectonics of Greece ». Thesis, University of Cambridge, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.272731.

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Tai, Yen-Ju Timothy. « Towards material-informed tectonics ». Thesis, Massachusetts Institute of Technology, 2018. http://hdl.handle.net/1721.1/120393.

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Thesis: S.M., Massachusetts Institute of Technology, Department of Materials Science and Engineering, 2018.
Cataloged from PDF version of thesis.
Includes bibliographical references.
This thesis introduces, demonstrates, and implements a unified computational design framework for material distribution modeling that enables the production of geometrically complex, materially heterogeneous, and functionally graded objects, across scales, media, and platforms. Receiving user-defined performance mappings as input, the workflow generates and evaluates instructions for designated fabrication systems, informed by the extrinsic constraints presented by the hardware and the intrinsic characteristics embedded in the materials utilized. As a proof of concept to the generalizable approach, three novel design-to-fabrication processes within the framework are introduced with material and materialization precedents and implemented through computational and robotic platforms: implicit modeling for the fabrication of photopolymers, trajectory optimizing for the fabrication of water-based material, and toolpath planning for the fabrication of fiber-based material. Titled Material-informed Tectonics, the framework extends the domain of parametric design processes from geometry to material, expands the potential application of volumetric material modeling techniques beyond high resolution multi-material 3D printing systems, and bridges between the virtual and the physical by integrating material information into the tectonic relationship between manufactured objects and manufacturing methods; thereby outlining an approach towards a synthesis of material properties, computational design, digital fabrication, and the environment.
by Yen-Ju Timothy Tai.
S.M.
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Edgar, Lynette. « A Tectonics of Opportunity ». Thesis, Curtin University, 2019. http://hdl.handle.net/20.500.11937/77965.

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This thesis investigates the forces, processes and themes presenting in understandings of opportunity as experienced through young peoples’ lives, (aged 15-17), where disengagement from formal learning arrangements creates displacement against a range of societal norms. The work delivers through narrative, phenomenology, and writing, within an embodied hermeneutic inquiry. A dialogue with the work of Jean-Jacques Rousseau and student voices is in juxtaposition with the shifting ground of politics and policy within the Tasmanian (Aust) landscape.
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Livres sur le sujet "And tectonics"

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J, Twiss Robert, dir. Tectonics. New York : W.H. Freeman & Co., 1995.

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Iain, Stewart, et Vita-Finzi Claudio, dir. Coastal tectonics. London : Geological Society, 1998.

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3

Plate tectonics. Minneapolis, Minn : Compass Point Books, 2009.

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4

Gregory, Alexis, dir. Comprehensive Tectonics. New York : Routledge, 2019. : Routledge, 2019. http://dx.doi.org/10.4324/9781315683881.

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Frisch, Wolfgang, Martin Meschede et Ronald C. Blakey. Plate Tectonics. Berlin, Heidelberg : Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-540-76504-2.

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Koeberl, Christian, et Herbert Henkel, dir. Impact Tectonics. Berlin, Heidelberg : Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27548-7.

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Watters, Thomas R., et Richard A. Schultz, dir. Planetary Tectonics. Cambridge : Cambridge University Press, 2009. http://dx.doi.org/10.1017/cbo9780511691645.

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McClay, K. R., dir. Thrust Tectonics. Dordrecht : Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3066-0.

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George, Linda. Plate tectonics. San Diego : Kidhaven Press, 2003.

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Georgia Institute of Technology. College of Architecture, dir. Textile tectonics. Rotterdam : NAi Publishers, 2011.

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Chapitres de livres sur le sujet "And tectonics"

1

Alizadeh, Akif A., Ibrahim S. Guliyev, Fakhraddin A. Kadirov et Lev V. Eppelbaum. « Tectonics ». Dans Geosciences of Azerbaijan, 129–201. Cham : Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-27395-2_5.

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Hodgkinson, Jane H., et Frank D. Stacey. « Tectonics ». Dans Practical Handbook of Earth Science, 135–42. Boca Raton : Taylor & Francis, 2017. | “A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc.” : CRC Press, 2017. http://dx.doi.org/10.9774/gleaf.9781315148038_14.

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Singley, Paulette. « Tectonics ». Dans How to Read Architecture, 185–222. New York, NY : Routledge, 2019. : Routledge, 2019. http://dx.doi.org/10.4324/9780429262388-11.

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Wuest, James D. « Molecular Tectonics ». Dans Mesomolecules, 107–31. Dordrecht : Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0005-2_4.

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Ristau, John. « Plate Tectonics ». Dans Encyclopedia of Natural Hazards, 769–72. Dordrecht : Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-1-4020-4399-4_271.

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Yuan, Philip F., Hao Meng et Pradeep Devadass. « Performative Tectonics ». Dans Robotic Fabrication in Architecture, Art and Design 2014, 181–95. Cham : Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04663-1_12.

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Jain, Sreepat. « Plate Tectonics ». Dans Fundamentals of Physical Geology, 313–36. New Delhi : Springer India, 2014. http://dx.doi.org/10.1007/978-81-322-1539-4_14.

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Van Kranendonk, Martin Julian. « Archean Tectonics ». Dans Encyclopedia of Astrobiology, 69–74. Berlin, Heidelberg : Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_100.

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Schulmann, Karel, et Hubert Whitechurch. « Plate Tectonics ». Dans Encyclopedia of Astrobiology, 1287–97. Berlin, Heidelberg : Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_1239.

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Kochemasov, G. G. « Lunar Tectonics ». Dans Encyclopedia of Lunar Science, 1–4. Cham : Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-05546-6_121-1.

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Actes de conférences sur le sujet "And tectonics"

1

Dunaev, Nikolay, Nikolay Dunaev, Nadezhda Politova et Nadezhda Politova. « NEWEST TECTONICS OF THE VISTULA SPIT AREA ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b943117f7e7.33196103.

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The interests of forecasting of the area’s development simulate to take more attention to the study of its newest tectonics. The most informative tectonic pattern for the studies of coastal zones is neotectonic one, based on the structural principle, which shows the newly formed and inherited dislocations, reflected in the modern landscape and exodynamics of the earth's surface. The question of the manifestations of newest tectonics by way on the example of the Vistula Spit (Baltic Sea) is discussed.
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Dunaev, Nikolay, Nikolay Dunaev, Nadezhda Politova et Nadezhda Politova. « NEWEST TECTONICS OF THE VISTULA SPIT AREA ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43162bdb89.

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The interests of forecasting of the area’s development simulate to take more attention to the study of its newest tectonics. The most informative tectonic pattern for the studies of coastal zones is neotectonic one, based on the structural principle, which shows the newly formed and inherited dislocations, reflected in the modern landscape and exodynamics of the earth's surface. The question of the manifestations of newest tectonics by way on the example of the Vistula Spit (Baltic Sea) is discussed.
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Sum, Tiffany. « Platonic tectonics ». Dans ACM SIGGRAPH ASIA 2009 Art Gallery & Emerging Technologies : Adaptation. New York, New York, USA : ACM Press, 2009. http://dx.doi.org/10.1145/1665137.1665173.

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van der Pluijm, Ben, et Christopher Scotese. « DECONSTRUCTING TECTONICS ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-352377.

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Miller, Sally. « Metabolic Tectonics ». Dans 2017 ACSA Annual Conference. ACSA Press, 2017. http://dx.doi.org/10.35483/acsa.amp.105.26.

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Historical conceptions of architecture view buildings as static artifacts within the ever changing global network of natural, economic, and social processes. In most cases, our built environment resists rather than accommodates these ever-changing conditions, necessitating intensive renovation or redevelopment. More fundamentally, the realm of design is thought to neatly conclude with the completion of the building, thus rendering off-limits processes of subtraction, reconstruction, succession and change.
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Harish, Bahuguna. « Application of block tectonic model and interblock tectonics at Koteshwar Dam Project ». Dans Recent Advances in Rock Engineering (RARE 2016). Paris, France : Atlantis Press, 2016. http://dx.doi.org/10.2991/rare-16.2016.3.

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McKenzie, D. P. « PLATE TECTONICS AT 50 ». Dans GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-318024.

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Dimitriu, Livio. « Tectonics of the Symbol ». Dans ARA 40th Congress. American Romanian Academy of Arts and Sciences, 2016. http://dx.doi.org/10.14510/40ara2016.4005.

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Kalenda, P., I. Wandrol, V. Procházka et L. Neumann. « Exogenous mechanism of global tectonics ». Dans Geoinformatics 2014. Netherlands : EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140425.

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Heimsath, Arjun. « Climate, Tectonics and Soil Production ». Dans Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1008.

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Rapports d'organisations sur le sujet "And tectonics"

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Bell, J. W. Quarternary tectonics, Task 1. Office of Scientific and Technical Information (OSTI), septembre 1993. http://dx.doi.org/10.2172/227025.

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Bell, J. W. Task 1 quarternary tectonics. Office of Scientific and Technical Information (OSTI), décembre 1994. http://dx.doi.org/10.2172/240927.

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Kukushkina, Nataliya. North America. Tectonics and mineral resources. Sous la direction de Nikolay Komedchikov, Aleksandr Khropov et Larisa Loginova. Entsiklopediya, février 2015. http://dx.doi.org/10.15356/dm2015-12-01-10.

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Williams, G. K. Tectonics and Structure, Mackenzie Corridor, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/130901.

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Ryerson, F. J., R. Finkel et J. van der Woerd. Satellite-based Observation of the Tectonics of Southern Tibet. Office of Scientific and Technical Information (OSTI), février 2003. http://dx.doi.org/10.2172/15004043.

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Piasecki, M. A. J. Tectonics across the Gander-Dunnage boundary in northeastern Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133580.

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Williams, G. K. Stratigraphy and tectonics of the Ronning and Delorme Groups, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/205762.

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Mcclay, K. R., M. W. Insley, N. A. Way et R. Anderton. Tectonics and mineralization of the Kechika Trough, Gataga area, northeastern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122675.

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Author, Not Given. Progress report. Task 1 - quaternary tectonics, 1 October 1991--30 September 1992. Office of Scientific and Technical Information (OSTI), septembre 1992. http://dx.doi.org/10.2172/227019.

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Heather, K. B., J. A. Percival, D. Moser et W. Bleeker. Tectonics and metallogeny of Archean crust in the Abitibi-Kapuskasing-Wawa region. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205285.

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