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Journal articles on the topic 'Asymmetric edifices'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

C., N. Gagan, Gornale Avinash, Karthik S., and G. Naresh Kumar B. "Application of N2 Method for Performance Evaluation of Reinforced Concrete Framed Asymmetric Edifices." Journal of Scientific Research & Reports 15, no. 1 (2017): 1–6. https://doi.org/10.9734/JSRR/2017/35028.

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As urban population is expanding constantly, the construction of edifices on the earthquake active area is also increasing. Due to aesthetic appearance, most of the edifices in the present era are asymmetric in nature. But when symmetric edifices are subjected to earthquake, their behaviors are not complex as compared to asymmetric edifices. Hence, for safety purpose, there is need to study the complex behavior of asymmetric edifices by conducting performance evaluation. In the present study, the performance evaluation of four RC edifices is done using N2 method. An effort is made to calculate

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2

Gagan, C., Avinash Gornale, S. Karthik, and B. Kumar. "Application of N2 Method for Performance Evaluation of Reinforced Concrete Framed Asymmetric Edifices." Journal of Scientific Research and Reports 15, no. 1 (2017): 1–6. http://dx.doi.org/10.9734/jsrr/2017/35028.

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3

Neuffer, Daniel P., Richard A. Schultz, and Robert J. Watters. "Mechanisms of slope failure on Pyramid Mountain, a subglacial volcano in Wells Gray Provincial Park, British Columbia." Canadian Journal of Earth Sciences 43, no. 2 (2006): 147–55. http://dx.doi.org/10.1139/e05-100.

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Pyramid Mountain is a subglacial volcano in Wells Gray Provincial Park in east-central British Columbia. Landslides deform the north and east flanks of the volcano. Field strength testing and rock mass classification designate the hyaloclastite breccia in which the landslides originated as a weak, massive rock mass: uniaxial compressive strengths (UCS) range from 24 to 35 MPa, and geologic strength index (GSI) and rock mass rating (RMR) values are 6070. The shear strength of fracture surfaces in the hyaloclastite breccia, as measured by laboratory direct shear tests, can be characterized by a

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4

Tsilavo, Raharimahefa, and Rasoazanamparany Christine. "Geomorphological Classification of Volcanic Cones in the Itasy Volcanic Field, Central Madagascar." International Journal of Geology and Earth Sciences 4, no. 4 (2018): 14–34. https://doi.org/10.32937/IJGES.4.4.2018.14-34.

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The Itasy Volcanic Field (IVF) is a monogenetic volcanic field located in the central highlands of Madagascar and is characterized by numerous volcanic cones displaying various geomorphological landforms. The IVF was a result of Pliocene to Quaternary volcanic eruptions and mainly composed of basaltic volcanic cones and trachyte domes. This paper aims to describe and to establish a geomorphological classification of basaltic volcanic cones within the IVF, based on their morphometric characteristics such as shape and diameter of the cone base; slope of the flanks of the edifice, and height of t

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5

Negbi, Ora. "Levantine Elements in the Sacred Architecture of the Aegean at the Close of the Bronze Age." Annual of the British School at Athens 83 (November 1988): 339–57. http://dx.doi.org/10.1017/s0068245400020797.

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Two cult structures from Mycenae and from a sanctuary recently discovered at Phylakopi, on the island of Melos, shed a new light on the sacred architecture of the Aegean at the close of the Bronze Age. This paper suggests that the edifices of both these sites should be classified as popular places of worship. This suggestion is based on their location, layout and size as well as on their foreign architectural affinities. The Phylakopi sanctuary, located against the fortification wall of the town, consists of a major temple to which a subsidiary shrine is attached. The pair of adjacent structur

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6

Emmanuel, S. "Short Communication: Evidence for non-Gaussian distribution of rock weathering rates." Earth Surface Dynamics 3, no. 3 (2015): 441–45. http://dx.doi.org/10.5194/esurf-3-441-2015.

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Abstract. The weathering of rocks influences the geochemistry of the oceans, the erosion of landscapes and man-made structures, and even the global climate. Although a high degree of variance is often observed in rate measurements, little is understood about the statistical characteristics of weathering rate distributions. This preliminary study demonstrates that the weathering rates of limestone, determined from measurements of an ancient eroded limestone edifice, can exhibit highly non-Gaussian behavior. While a Gaussian model produced a poor fit with the data, an alternative model – the gen

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7

Emmanuel, S. "Evidence for non-Gaussian distribution of rock weathering rates." Earth Surface Dynamics Discussions 3, no. 3 (2015): 561–75. http://dx.doi.org/10.5194/esurfd-3-561-2015.

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Abstract. The weathering of rocks influences the geochemistry of the oceans, the erosion of landscapes and manmade structures, and even the global climate. Although a high degree of variance is often observed in rate measurements, little is understood about the statistical characteristics of weathering rate distributions. This preliminary study demonstrates that the weathering rates of limestone, determined from measurements of an ancient eroded limestone edifice, can exhibit highly non-Gaussian behavior. While a Gaussian model produced a poor fit with the data, an alternative model – the gene

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8

Gonzales, Katherine, Anthony Finizola, Jean-François Lénat, et al. "Asymmetrical structure, hydrothermal system and edifice stability: The case of Ubinas volcano, Peru, revealed by geophysical surveys." Journal of Volcanology and Geothermal Research 276 (April 2014): 132–44. http://dx.doi.org/10.1016/j.jvolgeores.2014.02.020.

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9

Chu, Leo. "Desiring Futures." Journal of Anime and Manga Studies 1 (October 11, 2020): 113–37. http://dx.doi.org/10.21900/j.jams.v1.231.

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In this paper, I analyze the animated television series Puella Magi Madoka Magica based on a variety of literary critical methods: neo-noir criticism, feminist epistemology and studies of technoscience, and discussion of utopia/dystopia imagination. My focus is on the depiction of desire and hope, as two interconnected but potentially conflicting concepts, in Madoka Magica which presents different philosophical edifices related to them as one central narrative tension. On the other hand, the feminist methods I utilize will demonstrate how the “genre subversion” the series introduce can be read

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10

Tammaro, Umberto, Umberto Riccardi, Vittorio Romano, Michele Meo, and Paolo Capuano. "Topography and structural heterogeneities in surface ground deformation: a simulation test for Somma-Vesuvius volcano." Advances in Geosciences 52 (March 19, 2021): 145–52. http://dx.doi.org/10.5194/adgeo-52-145-2021.

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Abstract. We simulate the deformation of Somma-Vesuvius volcano due to some overpressure sources by means of a finite element 3D code. The main goal of these simulations is to investigate the influence of topography and structural heterogeneity on ground deformation. In our model the sources of deformation are embedded in an elastic linear isotropic medium and located at various depths. Geometry (shape and lateral extension) of the sources is mainly constrained by the results coming from recent seismic tomography studies. The structural heterogeneity has been modelled in terms of dynamic elast

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11

Gusella, Vittorio, and Riccardo Liberotti. "Seismic Vulnerability of Sub-Structures: Vantitelli’s Modulus in Murena Palace." Buildings 10, no. 9 (2020): 164. http://dx.doi.org/10.3390/buildings10090164.

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This paper focuses on the Murena Palace in Perugia, part of an architectural complex designed by Luigi Vanvitelli and completed by Carlo Murena in the 18th century. In the context of the seismic vulnerability assessment of this masonry building, the safety of a construction modulus, which gathers several peculiar features identified within the edifice, is analyzed by means of an integrated architectural-structural approach. This construction modulus, that will be called Vanvitelli’s Modulus, is characterized by an intrinsic structural asymmetry with clusters of rooms with masonry vaults, combi

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12

Bachèlery, Patrick, Bernard Robineau, Michel Courteaud, and Cécile Savin. "Debris avalanches on the western flank of Piton des Neiges shield volcano (Reunion Island)." Bulletin de la Société Géologique de France 174, no. 2 (2003): 125–40. http://dx.doi.org/10.2113/174.2.125.

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Abstract The Saint-Gilles breccias, on the western flank of Piton des Neiges volcano, are clearly identified as debris avalanche deposits. A petrographic, textural and structural analysis of the breccias and inter-bedded autochthonous lava flows enables us to distinguish at least four successive flank slides. The oldest deposit sampled the hydrothermally-altered inner parts of the volcano, and has a large volume. Failure was favored by the presence of a deep intensely-weathered layer. The younger deposits are from superficial sources, as their products are rarely hydrothermalized and are more

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13

Carmen, García Sánchez. "El pabellón Niels Bohr. Tradición Danesa y Modernidad = The Niels Bohr Pavilion. Danish Tradition and Modernity." rita_ Revista Indexada de Textos Académicos, no. 4 (October 5, 2015): 64–75. https://doi.org/10.24192/2386-7027(2015)(v4)(02).

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La casa de invitados de Niels Bohr fue el primer edificio del arquitecto danés Vilhelm Wohlert (1920-2007). Arraigado a la tradición danesa, representa una renovación basada en la absorción de influencias extranjeras: la arquitectura americana y la tradición japonesa. La caja de madera tiene el carácter sensible de un organismo vivo, siempre cambiante según las variaciones de luz del día o temperatura. Puertas plegables y contraventanas generan extensiones de las habitaciones. Cuando se abren, crean una prolongación del espacio int

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14

O’Hara, D., and L. Karlstrom. "The arc-scale spatial distribution of volcano erosion implies coupled magmatism and regional climate in the Cascades arc, United States." Frontiers in Earth Science 11 (June 19, 2023). http://dx.doi.org/10.3389/feart.2023.1150760.

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The morphology and distribution of volcanic edifices in volcanic terrains encodes the structure and evolution of underlying magma transport as well as surface processes that shape landforms. How magmatic construction and erosion interact on long timescales to sculpt these landscapes, however, remains poorly resolved. In the Cascades arc, distributed volcanic edifices mirror long-wavelength topography associated with underlying crustal magmatism and define the regional drainage divide. The resulting strong along- and across-arc modern precipitation gradients and extensive glaciation provide a n

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15

Cocchi, L., F. Muccini, C. Palmiotto, and G. Ventura. "Imaging the Plumbing System of the Asymmetric Vavilov Spreading Ridge (Tyrrhenian Sea Back‐Arc Basin) From Combined Bathymetry and Magnetic Data." Geophysical Research Letters 50, no. 22 (2023). http://dx.doi.org/10.1029/2023gl105196.

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AbstractBack‐arc basins (BABs) are associated with plate margins where crustal shortening, seafloor spreading, and volcanism coexist. The Vavilov basin (Tyrrhenian Sea) is a Pliocene BAB associated with the Apennine‐Tyrrhenian Sea subduction system and characterized by mantle exhumation. The NNE‐SSW elongated Vavilov seamount represents the easternmost and younger spreading ridge of the Vavilov basin. Here we present results of a morphological and magnetic study of the Vavilov seamount. Our results show that the seamount represents the last stage of the eastward asymmetric opening of the BAB.

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16

Rincón, M., A. Márquez, R. Herrera, F. Martín-González, I. López, and C. Crespo-Martín. "Morpho-structural criteria for the identification of spreading-induced deformation processes potentially compromising stratovolcano stability." Bulletin of Volcanology 85, no. 3 (2023). http://dx.doi.org/10.1007/s00445-023-01635-2.

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AbstractCharacterisation of surface deformation at stratovolcanoes is essential for a better understanding of the processes that can compromise edifice structural stability and potential for flank collapse. Spreading produced by the presence of a hydrothermal system or intrusion of a viscous magma body can produce similar deformation signatures, and both processes have implications for flank instability. In this work, we perform analogue models and consider examples from real volcanoes (Damavand, Ubinas, Semeru and Casita) so as to characterise and recognise surface deformation patterns produc

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17

Marco, Bonini, Maestrelli Daniele, Corti Giacomo, et al. "Modelling intra‐caldera resurgence settings: Laboratory experiments with application to the Los Humeros Volcanic Complex (Mexico)." Journal of Geophysical Research - Solid Earth 126, e2020JB020438. (2021). https://doi.org/10.1029/2020JB020438.

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Scaled analogue models explored the role of different boundary conditions in intra‐caldera resurgence processes. Models investigated the role of magma intrusion depth (Series 1), asymmetric and symmetric caldera collapse (Series 2), as well as the presence of existing discontinuities in the pre‐volcanic substratum (Series 3) on the style of caldera resurgence. Experimental results indicate that different intrusion depths resulted in different resurgence styles and structural patterns, which evolved from piston‐like resurgence, for deeper intrusions, to intra‐caldera resurgent domes for shallow

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18

Sonu, Amit Kumar, M. Satyanarayanan, Vamdev Pathak, Nimisha Vedanti, and J. P. Shrivastava. "Chemical stratigraphy of subsurface lava flows from the Koyna (KBH1) core and correlation with the southwestern stratigraphy of the Deccan Traps." Geological Society, London, Special Publications, July 2, 2021, SP518–2020–214. http://dx.doi.org/10.1144/sp518-2020-214.

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AbstractEarlier studies resolve well-constrained stratigraphy of southwestern Deccan Traps, although lack in adequate subsurface data. To establish stratigraphy and its correlation with the main Deccan Formations, we report flow-wise physical and chemical data of a ∼ 932 m thick core. We document 37 lava flow-units and 4 lava-flow groups having similar major-oxides. These groups fit into two of the recognized chemostratitigraphic Formations, and transitional Poladpur-Ambenali lavas. Also, data plots confine to Poladpur and Ambenali Formation on Ba vs. Sr, Ba vs. Zr/Nb; Ba/Y vs. Zr/Nb; and Ba,

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