Relevant bibliographies by topics / Metamorphing architecture

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

Academic literature on the topic 'Metamorphing architecture'

Author: Grafiati
Published: 1 July 2021
Last updated: 9 February 2022

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Journal articles on the topic "Metamorphing architecture"

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Lardeaux, Jean-Marc. "Deciphering orogeny: a metamorphic perspective. Examples from European Alpine and Variscan belts." Bulletin de la Société Géologique de France 185, no. 2 (2014): 93–114. http://dx.doi.org/10.2113/gssgfbull.185.2.93.

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AbstractIn this paper we review and discuss, in a synthetic historical way, the main results obtained on Alpine metamorphism in the western Alps. First, we describe the finite metamorphic architecture of the western Alps and discuss its relationships with subduction and collision processes. Second, we portray the progressive metamorphic evolution through time and space with the presentation of 5 metamorphic maps corresponding to critical orogenic periods, namely 85-65 Ma, 60-50 Ma, 48-40 Ma, 38-33 Ma and 30-20 Ma. We underline the lack of temporal data on high-pressure/low-temperature metamorphic rocks as well as the severe uncertainties on the sizes of rock units that have recorded the same metamorphic history (i.e. coherent P-T-t/deformation trajectories). We discuss the role of subduction-driven metamorphism in ocean-derived protoliths and the conflicting models that account for the diachrony of continental subductions in the western Alps.
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Lardeaux, Jean-Marc. "Deciphering orogeny: a metamorphic perspective Examples from European Alpine and Variscan belts." Bulletin de la Société Géologique de France 185, no. 5 (2014): 281–310. http://dx.doi.org/10.2113/gssgfbull.185.5.281.

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AbstractIn this paper we review and discuss, in a synthetic historical way, the main results obtained on Variscan metamorphism in the French Massif Central. First, we describe the pre-orogenic architecture of the French Massif Central on the base of available lithostratigraphic and geochemical constraints. Second, we portray the progressive metamorphic evolution through time and space with the presentation of 6 metamorphic maps corresponding to critical orogenic periods, namely 430–400 Ma, 400–370 Ma, 370–360 Ma, 360–345 Ma, 340–325 Ma and 320–290 Ma. We discuss the role of multiple subductions in orogeny, the metamorphic effects of continental collision (i.e. regional development of intermediate-pressure metamorphic series) as well as the links between post-thickening tectonics and the regional development of low-pressure metamorphic series coeval with crustal partial melting. As it was the case for the western Alps, we emphasize the lack of temporal data on high-pressure/low-temperature metamorphic rocks as well as the uncertainties on the sizes of rock units that have recorded the same metamorphic history (i.e. coherent P-T-t/deformation trajectories). Finally, we underline the main differences and similarities between the metamorphic evolutions of the western Alps and the French Massif Central.
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Anderson, J. E., A. Cunha, and M. F. Docker. "Novel “omega muscle units” in superficial body-wall myotomes during metamorphosis in the northern brook lamprey (Ichthyomyzon fossor)." Canadian Journal of Zoology 97, no. 12 (2019): 1218–24. http://dx.doi.org/10.1139/cjz-2019-0051.

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Lampreys transform from sedentary filter feeders to more mobile adults through a dramatic metamorphosis that includes remodeling of head muscle and skeletal systems. Metamorphic modifications of body-wall myotomes that could support changes in swimming behavior from larvae to adults have not been previously reported. Thus, transverse sections of northern brook lamprey (Ichthyomyzon fossor Reighard and Cummins, 1916) in larval (n = 4), metamorphosing (n = 3), and adult (n = 2) stages were used to investigate the architecture of body-wall muscle and to detect whether Pax7 and MyoD, proteins important in myogenesis, were co-localized in any muscle nuclei. In addition to myotomal complexity of muscle units composed of parietal and central fibers, there was a novel pattern of omega-shaped muscle units with curves of muscle fibers in the superficial mid-body myotome in metamorphosing lamprey. Small satellite-like cells were identified on central fibers in metamorphosing and adult lamprey muscle using routine histology and immunolocalization of Pax7 and MyoD with antibodies that specifically detect mammalian and teleost proteins. Transient “omega muscle units” may be a marker for impending myotomal growth and increasing swimming efficiency during maturation, possibly restricted to metamorphosis. Finding satellite-like cells suggests that Pax7 and MyoD may have distinctive roles in lamprey myogenesis.
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MacLachlan, K., W. J. Davis, and C. Relf. "Paleoproterozoic reworking of an Archean thrust fault in the Hearne domain, Western Churchill Province: U–Pb geochronological constraints." Canadian Journal of Earth Sciences 42, no. 7 (2005): 1313–30. http://dx.doi.org/10.1139/e05-036.

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The nature, timing and control of Archean crustal architecture on the distribution of Proterozoic reworking in Western Churchill Province are investigated in the Yathkyed Lake area, central Nunavut. The Tyrrell shear zone (TSZ) marks the boundary between the northwestern and central Hearne subdomains, respectively, in the hanging wall and footwall. Metamorphism and deformation in the hanging wall are ca. 2.66–2.50 Ga. Two episodes of metamorphism are recorded in a foliated granodiorite in the footwall, at 1818+5–2 and 1827 ± 5.6 Ma. The latter age is interpreted as the time of amphibolite-facies metamorphism and deformation in the footwall. A crosscutting dyke provides a minimum age of 1818 ± 2 Ma for this metamorphism and deformation. The TSZ is dominated by dextral oblique-slip shear fabrics. A suite of leucogranite dykes provide a maximum age of 1816 ± 2 Ma for dextral shearing. Dextral deformation is bracketed between 1815 ± 2 and 1811 ± 1 Ma, the ages of two other granitoid dykes. In an area of low dextral strain, there are proto-sheath folds related to Neoarchean thrusting. Paleoproterozoic transtensional shearing in the TSZ was localized along a preexisting late Archean thrust fault. The prior existence of this structure resulted in localization of penetrative Paleoproterozoic deformation in its footwall. This domain of high-grade Proterozoic deformation was uplifted in a regional, antiformal, metamorphic culmination, in part, by dextral-normal shearing along the TSZ. Penetrative basement deformation at depth played a role in transmitting farfield stresses related to the Trans-Hudson Orogen into its hinterland.
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Jackson, V. A., O. van Breemen, L. Ootes, et al. "U–Pb zircon ages and field relationships of Archean basement and Proterozoic intrusions, south-central Wopmay Orogen, NWT: implications for tectonic assignments." Canadian Journal of Earth Sciences 50, no. 10 (2013): 979–1006. http://dx.doi.org/10.1139/cjes-2013-0046.

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New field and U–Pb zircon data from the south-central Wopmay Orogen (south of 65°N) establish crystallization ages of basement and plutonic phases and bring to the forefront questions on the architecture of the orogen. The complex and extensive >3300–2575 Ma basement domain was derived from the adjacent Slave craton. Paleoproterozoic supracrustal rocks, dominated by an extensive pelitic–psammitic sequence with basal arenite, conglomerate, and carbonate, unconformably overlie this basement. Pre- to post-kinematic Paleoproterozoic plutons intrude both basement and overlying strata and crystallized at 1877, 1867–1862, and 1858–1850 Ma. The first pulse of plutonism constrains an early generation of metamorphism and deformation to younger than 1877 Ma and is corroborated by metamorphic zircon in Archean basement. The interval from 1867 to 1862 Ma brackets ductile deformation in granite and granodiorite intrusions; although corresponding structure in the metasedimentary strata is equivocal. Post-kinematic ca. 1858–1850 Ma plutons were coeval with localized high-grade metamorphism and concomitant recrystallization of Archean basement. The absence of older (>1880 Ma) phases of the Hepburn intrusive suite in south-central Wopmay Orogen demonstrates a previously unrecognized north–south plutonic dichotomy and that the historical assignment of Calderian metamorphism to ca. 1885 Ma may be too old. The designation of part of the area to a klippe of Hottah terrane is not compatible with field and zircon age data which shows that basement and the overlying strata can be tied directly to the Slave craton. The study raises questions regarding the tectonic relationship between the Hottah terrane and Slave craton.
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Peres, Guilherme G., Fernando F. Alkimim, and Hanna Jordt-Evangelista. "The southern Araçuaí belt and the Dom Silvério Group: geologic architecture and tectonic significance." Anais da Academia Brasileira de Ciências 76, no. 4 (2004): 771–90. http://dx.doi.org/10.1590/s0001-37652004000400011.

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The Araçuaí belt corresponds to the external portion of the western half of the Araçuaí-West Congo Neopro-terozoic orogen. TheAraçuaí belt fringes the São Francisco craton to east and is separated from the crystalline core of the orogen by the Abre Campo geophysical discontinuity. The southern Araçuaí belt involves four major lithologic units: the Archean and Paleoproterozoic gneisses of the Mantiqueira Complex, the Pedra Dourada Charnockite, the Paleoproterozoic Borrachudos Granitoid, and the metavolcanosedimentary rocks of the Dom Silvério Group. The Dom Silvério Group occurs in a NNE-SSW striking belt and consists of a thick package of metapelitic rocks with intercalations of quartzites, amphibolites, meta-ultramafics, banded iron formations, gondites and marbles. All units of the southern Araçuaí belt underwent four syn-metamorphic phases of deformation in the course of the Brasiliano event. The first phase, synchronous to a regional amphibolite facies metamorphism, was associated to a general tectonic transport towards north along the left-lateral Dom Silvério shear zone and its low angle segment. The second and third phases represent progressive stages of a west directed shortening, which led to the development of local thrusts and pervasive folds in several scales. The fourth phase is extensional and reflects the collapse of the orogen.
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Culshaw, N. G., J. W. F. Ketchum, N. Wodicka, and P. Wallace. "Deep crustal ductile extension following thrusting in the southwestern Grenville Province, Ontario." Canadian Journal of Earth Sciences 31, no. 1 (1994): 160–75. http://dx.doi.org/10.1139/e94-013.

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Two lithotectonic assemblages in southern Britt domain have different histories of plutonism, metamorphism, structural development, and mafic dyke emplacement. These differences are accounted for by postulating that a cryptic Grenvillian thrust separates the assemblages. Amphibolite-facies extensional shear along the Central Britt shear zone (CBSZ) overprinted the thrust, obscuring kinematic evidence for its existence. The structurally lower Bayfield–Nadeau Island assemblage contains orthogneiss suites of disparate age, lesser amounts of supracrustal rocks deposited before intrusion of the youngest orthogneiss, pre-Grenvillian and Grenvillian metamorphic assemblages, and at least three mafic dyke suites. The overlying Ojibway – Sand Bay assemblage contains only younger orthogneiss with Grenvillian metamorphic assemblages, volumetrically important supracrustal rocks that are younger than the youngest orthogneiss, and lacks cross-cutting mafic dykes.Comparable tectono-stratigraphic changes are present across the thrust boundary separating the Ojibway – Sand Bay assemblage and the basal Parry Sound assemblage. Extensional shearing did not strongly overprint this boundary and it therefore serves as a relatively unmodified analogue of the overprinted boundary.Extension on the CBSZ overlapped formation of transverse ductile folds (hinges parallel to the extension–transport direction). These folds and the CBSZ dominate the crustal architecture at this level and are interpreted to be late orogenic structures formed during a gravity-assisted shape adjustment of the orogenic wedge. Thermal softening of the lower crust caused by thrust thickening may have allowed this to occur.
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Bogossian, Jessica, Anthony I. S. Kemp, and Steffen G. Hagemann. "Linking Gold Systems to the Crust-Mantle Evolution of Archean Crust in Central Brazil." Minerals 11, no. 9 (2021): 944. http://dx.doi.org/10.3390/min11090944.

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The Goiás Archean Block (GAB) in central Brazil is an important gold district that hosts several world-class orogenic gold deposits. A better comprehension of the crustal, tectono-magmatic, and metallogenic settings of the GAB is essential to accurately define its geological evolution, evaluate Archean crustal growth models, and target gold deposits. We present an overview of gold systems, regional whole-rock Sm-Nd analyses that have been used to constrain the geological evolution of the GAB, and augment this with new in situ zircon U-Pb and Hf-O isotope data. The orogenic gold deposits show variable host rocks, structural settings, hydrothermal alteration, and ore mineralogy, but they represent epigenetic deposits formed during the same regional hydrothermal event. The overprinting of metamorphic assemblages by ore mineralogy suggests the hydrothermal event is post-peak metamorphism. The metamorphic grade of the host rocks is predominantly greenschist, locally reaching amphibolite facies. Isotope-time trends support a Mesoarchean origin of the GAB, with ocean opening at 3000–2900 Ma, and reworking at 2800–2700 Ma. Crustal growth was dominated by subduction processes via in situ magmatic additions along lithospheric discontinuities and craton margins. This promoted a crustal architecture composed of young, juvenile intra-cratonic terranes and old, long-lived reworked crustal margins. This framework provided pathways for magmatism and fluids that drove the gold endowment of the GAB.
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Eilouti, Buthayna. "Scenario-based design: New applications in metamorphic architecture." Frontiers of Architectural Research 7, no. 4 (2018): 530–43. http://dx.doi.org/10.1016/j.foar.2018.07.003.

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Balasubramanian, Sivaram, Robert W. Brennan, and Douglas H. Norrie. "An architecture for metamorphic control of holonic manufacturing systems." Computers in Industry 46, no. 1 (2001): 13–31. http://dx.doi.org/10.1016/s0166-3615(01)00101-4.

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Dissertations / Theses on the topic "Metamorphing architecture"

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Tuma, Fischer Vincent, and Tara Dyi. "Architecture to the Rescue : Metamorphing Built Space for Changing Purposes." Thesis, Malmö universitet, Institutionen för Urbana Studier (US), 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:mau:diva-44068.

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In December of 2019, the city of Wuhan in China reported an outbreak of a high number of pneumoniacases (Bassareo, 2020). The SARS-CoV-2 Virus (severe acute respiratory syndrome coronavirus 2)started to cause disturbance in societal functions, eventually leading to anomalous infection controlmeasures. Covid-19 was believed to have appeared in Sweden on 31st January and on the 9th ofMarch, it was confirmed in the Stockholm Region (Roden, 2020). Historically, pandemics have struckhumanity numerous times before, yet the virus proved that the modern world was still not prepared. Patients had to be accommodated in hospital corridors, general wards, and makeshift hospitals.Currently, the way of dealing with the virus is to admit patients into negative pressure isolation rooms.Negative pressure isolation rooms eliminate the airborne infectious particles, unlike regular emergencyrooms. Thus isolation rooms within alternative arrangements could offer a bigger space capacitywithout placing the burden on a municipality. Our thesis sheds light on disadvantages within temporary health facility solutions used during theCoronavirus pandemic. The project proposes an alternate strategy for dealing with sudden massdemand of hospital patient beds for quarantine units. This strategy involves a permanent buildingplanning, which is prepared in advance to limit the time for shifting space. In addition, multiple interiorfittings are prefabricated, easy to install as well as transport. By proposing a building with a floor planfor a primary office usage, the building could be transformed for a secondary usage as an infectiousdisease clinic in case of serious health threats to the modern welfare society.<br>I december 2019 rapporterade staden Wuhan i Kina ett utbrott av ett stort antal lunginflammationfall (Bassareo, 2020). SARS-CoV-2-viruset (allvarligt akut respiratoriskt syndrom-coronavirus 2) börjadeorsaka störningar i samhällsfunktionerna och ledde så småningom till avvikande åtgärder förinfektionskontroll. Covid-19 tros ha dykt upp i Sverige den 31 januari och den 9 mars bekräftades det iStockholmsregionen (Roden, 2020). Historiskt sett har pandemier drabbat mänskligheten flera gångertidigare, ändå bevisade viruset att den moderna världen fortfarande inte var beredd. Patienterna fick bo på sjukhuskorridorer, allmänna avdelningar och provisoriska sjukhus. För närvarandeär sättet att hantera viruset på att ta in patienter i negativ tryck isoleringsrum. Isoleringsrum med negativttryck eliminerar de luftburna smittsamma partiklarna, till skillnad från vanliga akutrum. Således kanisoleringsrum inom alternativa arrangemang erbjuda en större utrymmes kapacitet utan att belastaen kommun. Vår avhandling belyser nackdelar med tillfälliga sjukvårds lösningar som används under Coronaviruspandemin. Projektet föreslår en alternativ strategi för att hantera plötslig mass efterfrågan på sjukhuspatientsängar för karantän avdelningar. Denna strategi innebär en permanent byggnadsplanering,som är förberett i förväg för att limitera tiden det tar att skifta ett utrymme. Dessutom är flerainredningsdetaljer prefabricerade, lätta att installera och transportera. Genom att föreslå enbyggnad med en planlösning för en primär kontorsanvändning kan byggnaden omvandlas till ensekundär användning som är en infektionsklinik, i händelse av allvarliga hälsorisker mot det modernavälfärdssamhället.
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Balasubramanian, Sivaram. "A metamorphic control architecture for holonic systems." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0019/NQ47923.pdf.

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Lin, Xuanyi. "Creating and Deploying Metamorphic Services for SWMM Community Based on FaaS Architecture." University of Cincinnati / OhioLINK, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1623251020874486.

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Tropper, Robin. "Architecture and programming paradigm for a scalable, metamorphic and cloud-collaborative user environment." Thesis, University of Ottawa (Canada), 2010. http://hdl.handle.net/10393/28486.

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A growing number of enterprise applications on the Internet ranging from banking transactions to business management make use of real-time collaboration. Simultaneous access from any device to any set of applications shared among many users is a hot area of research and development. This thesis designed a thick-client for real-time collaboration supporting the applications development and interoperability. It introduces a new programming paradigm, algorithms and protocols to bring real-time collaboration to a web-based platform. Its component-oriented metamorphic architecture supports a run-time scalable multi-desktop environment connecting client applications through automated remote procedure call and the object request broker pattern while providing new mechanisms for dynamic resource loading. The new architecture supports unsolicited server control actions on the client using an event model to simulate interruptions and sustained user-activity during network failure. Results obtained validate the correctness of the approach and the feasibility of an extensible web-based platform for real-time collaboration.
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Vitale, Brovarone Alberto. "From rifting to orogen : structure of Alpine Corsica and inheritance of rifting-related architectures in HP terranes." Thesis, Montpellier 2, 2011. http://www.theses.fr/2011MON20029/document.

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La Corse Alpine offre une section complète du prisme orogénique alpin où la plupart des équivalents des unités décrites dans les Alpes Occidentales peuvent être trouvés sur une section de 40 km. Les minéraux d'haute pression sont exceptionnellement bien préservés, particulièrement la lawsonite, offrant un accès unique à la compréhension de zones de subduction. La Corse alpine est formée par une pile complexe d’unités métamorphiques d'origine continentale et océanique. Ces unités ont été interprétées soit comme des mélanges tectoniques complexes formés pendant la subduction alpine, soit comme les parties plus continues de lithosphère continentale et-ou océanique. Les rares estimations de condition PT sur des larges régions de la chaîne résultent en plusieurs incertitudes dans l'identification des limites séparant les unités qui ont subi des évolutions tectono-métamorphiques différentes et, par conséquent, dans la définition d'une architecture complète de la chaîne. Les données de terrain, structurelles et métamorphiques obtenues dans cette étude aux différentes échelles suggèrent que la chaîne de la Corse alpine est caractérisée par une forte conservation de structures pré-alpin, de la micro-échelle à l'échelle de la chaîne, malgré la déformation intense associée avec le métamorphisme, qui a localement donné les conditions du facies éclogitique et lawsonite. En détail, seulement neuf domaines tectono-métamorphiques homogènes ont été identifiés. Ces terrains peuvent être attribué aux domaines paléogéographiques différents qui ont subi des évolutions tectono-métamorphiques différentes. Malgré ça, les données géochronologiques fournies pendant cette étude indiquent que la Corse alpine résulte d'une évolution complexe, étant caractérisée par la signature claire tant de la tectonique alpine Eocène, à 35 Ma, que de la tectonique apennine, à 25 Ma. Les résultats fournis dans cette thèse contribuent non seulement à la compréhension des processus de subduction et de formation de montagnes, mais donnent aussi des contraintes importantes pour déchiffrer les systèmes Tethys-Alpes et Alpes-Apennine<br>Alpine Corsica offers a complete section through the Alpine orogenic wedge where most equivalent of the units described in the Western Alps may be found over a 40 km section. High-pressure mineral assemblages are exceptionally well preserved, especially lawsonite, offering a unique access to the understanding of deeply subducted terranes.Alpine Corsica consists of a complex stack of variably metamorphosed units of continental and Tethys-derived material. These units have been interpreted either as complex tectonic mixing formed during the Alpine subduction, or as more continuous portions of continental and/or oceanic lithosphere. The lack of detailed PT estimates over wide regions of the belt results in several uncertainties in identifying the boundaries separating units that experienced different tectono-metamorphic evolutions and, consequently, in the definition of an exhaustive architecture of the belt.Field, structural and metamorphic data collected in this study at different scales suggest that the Alpine Corsica belt is characterized by a high preservation of pre-Alpine sctructures, from the micro-scale up the scale of the belt, despite the intense deformation essociated with metamorphism, which locally reached lawsonite-eclogite metamorphism. In particular, only nine homogeneous tectono-metamorphic domains have been identified. These terranes can be referred to different paleogeographic domains that experienced different tectono-metamorphic evolutions.Despite that, geochronological data provided during this study indicate that Alpine Corsica results fro a complex polyphase evolution, being characterized by clear signature of both Alpine tectonics, at around 35 Ma, and Apennine tectonics, at around 25 Ma.Results provided in this paper contribute not only to the understanding of processes of subduction and mountain building, but also give important constraints for deciphering the Tethys-Alps and Alps-Apennine systems
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Books on the topic "Metamorphing architecture"

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Salat, Serge. Paul Andreu: Metamorphis of the circle. Electa Moniteur, 1990.

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Ring, Uwe. Extending a continent: Architecture, rheology and heat budget. Geological Society, 2009.

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Peter, Zumthor, and Binet Hélène 1959-, eds. Peter Zumthor--Therme Vals. Scheidegger & Spiess, 2007.

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Book chapters on the topic "Metamorphing architecture"

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Luo, Gang, Xi Zheng, Huai Liu, et al. "Verification of Microservices Using Metamorphic Testing." In Algorithms and Architectures for Parallel Processing. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-38991-8_10.

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"4. THE FOUR ELEMENTS OF ARCHITECTURE." In Metamorphism. Birkhäuser, 2017. http://dx.doi.org/10.1515/9783035608069-005.

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Mendes, David José Murteira, Manuel José Lopes, José Manuel García-Alonso, Jorge Santos, and Luís Manuel Mota Sousa. "Resilient Software Architecture Platform for the Individual Care Plan." In Exploring the Role of ICTs in Healthy Aging. IGI Global, 2020. http://dx.doi.org/10.4018/978-1-7998-1937-0.ch002.

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The individual care plan (ICP) is a metamorphic being. The only steady reality that it maintains is its final objective, stated and explained in the previous chapter where the ICP is thoroughly introduced and debated. It is a fantastic beast, better described as a system of systems that is severely polymorphic due to its coverage both in level of care as well as sources of data to handle. Patient monitoring generates large volumes of data. There is the evident need of an advanced approach that can deal with these huge amounts of healthcare data extracted from various sources such as the wearable sensors, medical, and nursing records that are currently called big data. The purpose of this chapter is to introduce and discuss the software platform that is adequate to develop and deploy the system paying attention to the needs of high-availability, sensitive information security; service-level agreements for multiple healthcare interoperability; law and ruling conformance; as well as other technical and ethical aspects.
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Gottschalk, Richard R. "Petrology of eclogite and associated high-pressure metamorphic rocks, south-central Brooks Range, Alaska." In Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2324-8.141.

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Harris, R. A. "Origin and tectonic evolution of the metamorphic sole beneath the Brooks Range ophiolite, Alaska." In Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2324-8.293.

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"Holonic Metamorphic Architectures for Manufacturing: Identifying Holonic Identifying Holonic Structures in Multiagent Systems by Fuzzy Modeling." In Computational Intelligence In Manufacturing Handbook. CRC Press, 2000. http://dx.doi.org/10.1201/9781420041934-8.

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Gottschalk, Richard R., and Lawrence W. Snee. "Tectonothermal evolution of metamorphic rocks in the south-central Brooks Range, Alaska: Constraints from 40Ar/39Ar geochronology." In Architecture of the Central Brooks Range Fold and Thrust Belt, Arctic Alaska. Geological Society of America, 1998. http://dx.doi.org/10.1130/0-8137-2324-8.225.

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Conference papers on the topic "Metamorphing architecture"

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Yang, Qiang, Andrew P. Murray, David H. Myszka, and Shujun Li. "Structure Synthesis of Multi-DOF Planar Metamorphic Mechanisms With a Single Driver." In ASME 2020 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/detc2020-22196.

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Abstract This paper approaches the type synthesis of multi-degree of freedom planar metamorphic mechanisms with a single driver in a systematic process. The process is facilitated by implementing a constraint status matrix and a equivalent resistance matrix as a method for identifying an appropriate structure of planar metamorphic mechanisms with a single driver. Multi-structures can be obtained from the same source metamorphic mechanism by designing different constraint architectures of metamorphic joints. To determine the constraint architectures of metamorphic joints and their different assembly combinations, the constraint status matrix is built based on the task-based metamorphic cyclogram of a source mechanism. According to the equivalent resistance gradient model and the constraint status matrix, an equivalent resistance matrix for the metamorphic joints is proposed. A structural synthesis matrix of the metamorphic mechanism is then obtained from the equivalent resistance matrix by deducing the constraint-form vectors of the metamorphic joints. Furthermore, an effective kinematic diagram synthesis of the source mechanism of the planar metamorphic mechanism is proposed which is based only on the 14 one or zero degree-of-freedom (DOF) linkage groups. The entire structural design method of a metamorphic mechanism is based on the structural synthesis matrix and given in steps. Finally, a proposed structural design approach is illustrated by two examples.
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Brennan, Robert W., Sivaram Balasubramanian, and Douglas H. Norrie. "Dynamic control architecture for metamorphic control of advanced manufacturing systems." In Intelligent Systems & Advanced Manufacturing, edited by Bhaskaran Gopalakrishnan, San Murugesan, Odo Struger, and Gerfried Zeichen. SPIE, 1997. http://dx.doi.org/10.1117/12.294433.

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Khodamoradi, Peyman, Mahmood Fazlali, Farhad Mardukhi, and Masoud Nosrati. "Heuristic metamorphic malware detection based on statistics of assembly instructions using classification algorithms." In 2015 18th CSI International Symposium on Computer Architecture and Digital Systems (CADS). IEEE, 2015. http://dx.doi.org/10.1109/cads.2015.7377792.

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van der Wijk, Volkert, Ketao Zhang, and Jian S. Dai. "Force Balance of a Spatial Metamorphic 6R Closed-Chain Linkage With Specific Kinematic Conditions." In ASME 2016 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/detc2016-60068.

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Abstract:
For deployable, reconfigurable, and metamorphic linkages force balance is an important property to bear the static and dynamic forces caused by the mass of each element, either due to gravity or due to inertia when moving. Force balance refers to ‘shaking force balance’ meaning that for all motion of the linkage, no dynamic reaction forces are exerted to its base and to the surroundings preventing base vibrations. This typically is an important feature in high-speed and high-precision robotic manipulation tasks. Force balance also refers to ‘static balancing with solely mass’. Since the center of mass of a force balanced linkage is stationary for all motion, a force balanced linkage is also statically balanced which means that the linkage is not affected by gravity and remains stationary in any pose without the need of actuators or brakes. This property is important for the design of, among others, large moving structures such as mobile platforms and deployable structures used in architecture. In this paper the force balance of a spatial metamorphic plano-spherical 6R closed linkage with plane symmetry is investigated. It is shown that because of its specific kinematic conditions — being pantograph relations in the projected plane — advantageous balance solutions can be found for each of the four reconfiguration modes. For specific geometric conditions on the link design also solutions are found where the links balance one another without the need of any countermass. It is also shown how an advantageous compromise force balance solution for multiple modes is found. For this purpose an approximate force balance solution was investigated. The results are compared with the general force balance solutions of a general spatial 6R closed linkage, which are also shown and explained. All balance solutions are illustrated to have realistic interpretations.
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Sequeira, Nicole, and Abhijit Bhattacharya. "THE ARCHITECTURE AND EVOLUTION OF A SYN-OROGENIC GRENVILLIAN-AGE METAMORPHIC CORE COMPLEX, EASTERN INDIA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-331382.

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