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Journal articles on the topic 'Domain zone'

Author: Grafiati

Published: 28 May 2022

Last updated: 30 July 2025

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1

Behera, K. K., and J. P. Mohakul. "Delineating the Lithotectonic Domains in the Eastern Ghats Mobile Belt: Implication for the Regional Exploration of the Metasediment Hosted Graphite and Manganese Ore Horizons." Journal Of The Geological Society Of India 100, no. 12 (2024): 1741–54. https://doi.org/10.17491/jgsi/2024/174046.

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ABSTRACT The present work documents and discusses the spatial disposition and lithotectonic control of graphite and manganese mineralization associated with metasediments of the Proterozoic Eastern Ghats Mobile Belt (EGMB) of eastern Indian shield and attempts to evolve a working model for furthering their exploration activities. Detailed satellite image based trendline mapping was done for the part of EGMB north of the Godavari Rift to map the marker horizons and demarcate structural discontinuities. Based on the contiguity of mineralised zones and their disruption due to structural discontin

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Matsumoto, Hideyuki, Ko Kobayakawa, Reiko Kobayakawa, et al. "Spatial Arrangement of Glomerular Molecular-Feature Clusters in the Odorant-Receptor Class Domains of the Mouse Olfactory Bulb." Journal of Neurophysiology 103, no. 6 (2010): 3490–500. http://dx.doi.org/10.1152/jn.00035.2010.

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The glomerular layer of the mammalian olfactory bulb (OB) forms odorant receptor (OR) maps. Each OR map is structurally and functionally compartmentalized into zones (dorsal and ventral) and domains (DI and DII in the dorsal zone). We previously reported that glomeruli with similar molecular receptive range properties formed molecular feature clusters at stereotypical positions in the rat OB. However, the spatial arrangement of the molecular feature clusters with regard to the OR zones and domains has not been systematically examined. In this study, we optically mapped the molecular feature cl

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Wang, Xiaolu, Mark Kibschull, Michael M. Laue, Beate Lichte, Elisabeth Petrasch-Parwez, and Manfred W. Kilimann. "Aczonin, a 550-Kd Putative Scaffolding Protein of Presynaptic Active Zones, Shares Homology Regions with Rim and Bassoon and Binds Profilin." Journal of Cell Biology 147, no. 1 (1999): 151–62. http://dx.doi.org/10.1083/jcb.147.1.151.

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Neurotransmitter exocytosis is restricted to the active zone, a specialized area of the presynaptic plasma membrane. We report the identification and initial characterization of aczonin, a neuron-specific 550-kD protein concentrated at the presynaptic active zone and associated with a detergent-resistant cytoskeletal subcellular fraction. Analysis of the amino acid sequences of chicken and mouse aczonin indicates an organization into multiple domains, including two pairs of Cys4 zinc fingers, a polyproline tract, and a PDZ domain and two C2 domains near the COOH terminus. The second C2 domain

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4

James, D. T., J. N. Connelly, H. A. Wasteneys, and G. J. Kilfoil. "Paleoproterozoic lithotectonic divisions of the southeastern Churchill Province, western Labrador." Canadian Journal of Earth Sciences 33, no. 2 (1996): 216–30. http://dx.doi.org/10.1139/e96-019.

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The southeastern Churchill Province (SECP) is a Paleoproterozoic system of orogens that formed during collision of the Nain and Superior cratons with a composite lithotectonic terrane that now forms the medial, metamorphic–plutonic core zone of the SECP. In western Labrador, the core zone consists of reworked Archean gneisses, Paleoproterozoic supracrustal rocks, and variably deformed 1.83–1.81 Ga granitic plutons. It is subdivided into three Paleoproterozoic lithotectonic domains (McKenzie River, Crossroads, and Orma), which are separated from each other by dextral transpressive high-strain z

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Guillot, Stéphane, Silvia di Paola, René-Pierre Ménot, et al. "Suture zones and importance of strike-slip faulting for Variscan geodynamic reconstructions of the External Crystalline Massifs of the western Alps." Bulletin de la Société Géologique de France 180, no. 6 (2009): 483–500. http://dx.doi.org/10.2113/gssgfbull.180.6.483.

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Abstract This paper reviews the geodynamic evolution of the Belledonne, Grandes Rousses and Oisans massifs in the western Alps from Early Ordovician to Permian times. Three domains are distinguished. The eastern domain, which includes the NE Belledonne massif and the inner Oisans massif, records the subduction of the Central-European ocean along a NW dipping subduction zone. The western domain is marked by Cambro-Ordovician back-arc rifting (Chamrousse ophiolite) initiating the opening of the Rheic ocean. It was followed by Mid-Devonian obduction of the back-arc Chamrousse ophiolite, towards t

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Culshaw, Nicholas, Christopher Gerbi, and Laura Ratcliffe. "Macro- and microstructural analysis of the North Tea Lake Mylonite Zone: an extensional shear zone in the Central Gneiss Belt, Grenville Province, Ontario." Canadian Journal of Earth Sciences 52, no. 11 (2015): 1027–44. http://dx.doi.org/10.1139/cjes-2015-0009.

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The North Tea Lake Mylonite Zone is a late extensional ductile fault that is concordant with and has reworked fabrics of the North Tea Lake Shear Zone, the frontal thrust shear zone of the upper amphibolite–granulite facies Kiosk domain within the interior of the Central Gneiss Belt. North Tea Lake Mylonite Zone fabric is an anomalously fine-grained mylonite compared to Central Gneiss Belt gneisses, and consists of three microstructural domains that display progressive recrystallization and grain size refinement of the protolith granitoid. On the basis of petrography and electron backscatter d

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Shin, J. W., J. Y. Lee, Y. S. No, T. W. Kim, and W. K. Choi. "Atomic arrangement variations of 30° in-plane rotation domain boundaries in ZnO thin films grown on Si substrates due to thermal annealing." Journal of Materials Research 24, no. 6 (2009): 2006–10. http://dx.doi.org/10.1557/jmr.2009.0233.

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High-resolution transmission electron microscopy (HRTEM) images of annealed ZnO thin films showed the domain boundaries of a (0) plane with a transition zone and a (1) plane without a transition zone. The 30° in-plane rotation domain boundaries were formed in the ZnO thin films because the angle of the c-axis was tilted 3.5° in comparison with that of neighboring 30° in-plane rotation domains to reduce the misfit strain energy. The atomic arrangement variations of 30° in-plane rotation domain boundaries in ZnO thin films grown on Si substrates due to thermal annealing are described.

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8

Wen, Xin, Haijun Wu, Yilong Fan, and Weikang Jiang. "A multizone sound field reproduction method based on modal domain analysis." INTER-NOISE and NOISE-CON Congress and Conference Proceedings 268, no. 5 (2023): 3916–21. http://dx.doi.org/10.3397/in_2023_0559.

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Multizone sound field reproduction for synthesizing desired sound fields over multiple spatial zones has been widely studied. In the traditional multizone sound field reproduction modal domain method, the final loudspeaker weights required to reproduce the desired sound field are obtained by translating the optimal equivalent global modal domain coefficients, which is susceptible to the characteristics and location of the loudspeakers and reduces the reproduction performance. This paper investigates a multizone sound field reproduction in modal domain for directly obtaining the reproducing lou

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Luebbers, R., D. Ryan, and J. Beggs. "A two-dimensional time-domain near-zone to far-zone transformation." IEEE Transactions on Antennas and Propagation 40, no. 7 (1992): 848–51. http://dx.doi.org/10.1109/8.155753.

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10

Ashton, K. E., J. F. Lewry, L. M. Heaman, R. P. Hartlaub, M. R. Stauffer, and H. T. Tran. "The Pelican Thrust Zone: basal detachment between the Archean Sask Craton and Paleoproterozoic Flin Flon Glennie Complex, western Trans-Hudson Orogen." Canadian Journal of Earth Sciences 42, no. 4 (2005): 685–706. http://dx.doi.org/10.1139/e04-035.

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The Pelican Thrust Zone is a 37 km-wide recrystallized mylonite zone, along which Paleoproterozoic arc volcano-plutonic and derived sedimentary rocks of the Flin Flon Glennie Complex were thrust over an Archean package (Jan Lake Complex) consisting of ca. 3.1 Ga calc-alkaline orthogneisses, pelitic migmatites, and a ca. 2.45 Ga tholeiitic charnockitenorite intrusive suite. A regional northeast-plunging stretching lineation and a variety of kinematic indicators imply southwesterly transport, matching that of other coeval shallower crustal-level structures observed throughout the northern Fl

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Scanlan, Martin, and Peter Miller. "In Fits and Starts: Learning to Create a Neighborhood Educational Opportunity Zone." Teachers College Record: The Voice of Scholarship in Education 115, no. 5 (2013): 1–44. http://dx.doi.org/10.1177/016146811311500503.

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Background/Context Disparities in educational opportunity and academic achievement are closely connected to social class characteristics that lie beyond the schoolhouse doors. Comprehensive approaches to urban school reform are ecological, seeing schools nested in broader communities. The research presented here examines one such approach in a neighborhood educational opportunity zone: a geographically defined area where a traditionally marginalized children and families are clustered and resources are intensely focused to respond to their concomitant needs. Purpose/Objective/Research Question

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Williantarra, Ivanna, Timmy Richardo, Inge Kumalasari Sudibjo, and Putu Virgina Partha Devanthi. "An Overview of the Primary Cilium and RPGRIP1L: The Signalling Hub’s Anchor for Organ Development and Homeostasis." Malaysian Journal of Fundamental and Applied Sciences 17, no. 5 (2021): 582–92. http://dx.doi.org/10.11113/mjfas.v17n5.2284.

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Research on the primary cilium has been growing exponentially in the past several decades due to its functions as a cell signalling hub, which defects leads to several disorders and abnormalities collectively known as ciliopathies. Among other parts of the primary cilium structures, the transition zone is the area whose defects lead to the most severe clinical manifestations and high lethality. The ciliary transition zone consists of multiple protein modules that are hypothesized to be anchored by the RPGRIP1L protein. Despite its importance, RPGRIP1L studies remain hidden from the limelight,

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Tucker, R. D., J. Y. Roig, C. Delor, et al. "Neoproterozoic extension in the Greater Dharwar Craton: a reevaluation of the “Betsimisaraka suture” in MadagascarThis article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh." Canadian Journal of Earth Sciences 48, no. 2 (2011): 389–417. http://dx.doi.org/10.1139/e10-034.

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The Precambrian shield of Madagascar is reevaluated with recently compiled geological data and new U–Pb sensitive high-resolution ion microprobe (SHRIMP) geochronology. Two Archean domains are recognized: the eastern Antongil–Masora domain and the central Antananarivo domain, the latter with distinctive belts of metamafic gneiss and schist (Tsaratanana Complex). In the eastern domain, the period of early crust formation is extended to the Paleo–Mesoarchean (3.32–3.15 Ga) and a supracrustal sequence (Fenerivo Group), deposited at 3.18 Ga and metamorphosed at 2.55 Ga, is identified. In the centr

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WENDT, ANKE S., ALAN P. M. VAUGHAN, and ALEXANDER TATE. "Metamorphic rocks in the Antarctic Peninsula region." Geological Magazine 145, no. 5 (2008): 655–76. http://dx.doi.org/10.1017/s0016756808005050.

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AbstractThe distribution of metamorphic rocks in the Antarctic Peninsula region, new quantitative peak pressure–temperature data along the Antarctic Peninsula, and a literature review on the current knowledge of metamorphic conditions in the Antarctic Peninsula region have been compiled into a single metamorphic map. The pressure–temperature data for the Antarctic Peninsula indicate (1) burial of supracrustal rocks to low to mid-crustal depth along the eastern and western side of the Antarctic Peninsula and on some islands adjacent to the western side of the peninsula; (2) uplift of lower- to

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Ahmed, Nisar, Akhter Muhammad Kassi, Aimal Khan Kasi, et al. "GIS-BASED HIGH-RESOLUTION GEOLOGICAL MAP (SCALE 1:50,000): A NEW WINDOW INTO STRUCTURAL DOMAINS OF THE QUETTA AND SURROUNDING AREAS." Journal of Mountain Area Research 8 (December 3, 2022): 27. http://dx.doi.org/10.53874/jmar.v8i0.146.

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The Quetta and surrounding areas are part of the collision zone between the Indian and Eurasian plates, named as Kirthar and Sulaiman Fold-Thrust belts. The collision is accommodated by folding, thrusting and the Nushki-Chaman Transform Fault System. Detailed high-resolution (scale 1:50,000) mapping and structural analyses were carried out using modern remote-sensing techniques of the ArcGIS to understand mutual relationships of the structural patterns and geometries, and the regional and local stress patterns in the study area. Fieldwork was carried out to acquire the stratigraphic, structura

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Martínez, Ana, and Leonardo Ortega. "Delimitation of domains in the external Río de la Plata estuary, involving phytoplanktonic and hydrographic variables." Brazilian Journal of Oceanography 63, no. 3 (2015): 217–27. http://dx.doi.org/10.1590/s1679-87592015086106303.

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AbstractAutumn and spring hydrological (temperature and salinity) and biological (chlorophyll, phaeopigments and phytoplankton species) variables were analysed. Phytoplankton biomass, expressed as chlorophyll a reach a maximum of 6.1 µg L-1in autumn and 22.8 µg L-1 during spring. Maxima were found in the frontal zone and marine adjacent area. Four domains were identified through multivariate analysis: Riverine, Estuarine, Frontal and Oceanic; mainly due to salinity and depth in autumn and due to salinity and chlorophyll in spring. The Riverine and Oceanic domains (West and East boundaries) mat

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Tian, Chi, Yunfeng Chen, Jiansong Zhang, and Yiheng Feng. "Integrating Domain Knowledge with Deep Learning Model for Automated Worker Activity Classification in mobile work zone." Journal of Information Technology in Construction 29 (April 18, 2024): 264–80. http://dx.doi.org/10.36680/j.itcon.2024.013.

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Accurate classification of workers’ activity is critical to ensure the safety and productivity of construction projects. Previous studies in this area are mostly focused on building construction environments. Worker activity identification and classification in mobile work zone operations is more challenging, due to more dynamic operating environments (e.g., more movements, weather, and light conditions) than building construction activities. In this study, we propose a deep learning (DL) based classification model to classify workers’ activities in mobile work zones. Sensor locations are opti

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18

White, D. J., R. M. Easton, N. G. Culshaw, et al. "Seismic images of the Grenville Orogen in Ontario." Canadian Journal of Earth Sciences 31, no. 2 (1994): 293–307. http://dx.doi.org/10.1139/e94-028.

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In 1990, Lithoprobe acquired 240 km of seismic-reflection data across parts of the Central Gneiss Belt (CGB) and the Central Metasedimentary Belt (CMB) within the western Grenville Province of southern Ontario. Interpretation of these data in conjunction with geological constraints provided by bedrock mapping supports a model of northwest-directed thrusting and crustal shortening for the Grenville Orogen. Within the CGB, the Parry Sound shear zone is imaged as a 3 km wide zone of reflections dipping southeastward at 20–25° and soling at depths < 7 km in the north and < 3 km in the south

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Zhou, Wenlong, Jianquan Liu, Yu Zhou, and Jie Wei. "Impact of blockage size on recirculation zones and flow instability in CEFR single-box fuel assemblies: A CFD simulation study." Journal of Physics: Conference Series 3033, no. 1 (2025): 012048. https://doi.org/10.1088/1742-6596/3033/1/012048.

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Abstract This study employs CFD software to numerically simulate accidents in a single-box CEFR fuel assembly, focusing on the impact of recirculation zones on flow instability within the domain during blockage incidents. The analysis explores how various factors affect the recirculation zone and its implications for system performance. The key findings are as follows: The size of the recirculation zone is positively correlated with both the area and thickness of the blockage. Larger blockage areas and thicknesses result in more extensive recirculation zones, which in turn have a greater impac

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Cairns, S., C. Relf, K. MacLachlan, and W. J. Davis. "Neoarchean decoupling of upper- and mid-crustal tectonothermal domains in the southeast Slave Province: evidence from the Walmsley Lake area." Canadian Journal of Earth Sciences 42, no. 6 (2005): 869–94. http://dx.doi.org/10.1139/e05-057.

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The Walmsley Lake area of the southeastern Slave Province, Northwest Territories, exposes a crustal transect from greenschist through to upper amphibolite facies. Two tectonothermal crustal domains are proposed based on disparate tectonic histories and rock types. Within the upper tectonothermal domain, D1 deformation reached lower amphibolite facies prior to 2614 Ma and associated M1 metamorphic conditions outlasted D1. Peak M2 conditions reached middle amphibolite facies prior to 2603 Ma and outlasted D2 deformation. Deformation style and metamorphic sequencing during these two pre-2600 Ma e

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Ma, Hui, Yuan Ping, and Yong Zhang. "Privacy-Preserving Cross-Zone Ride-Matching for Online Ride-Hailing Service." Mathematical Problems in Engineering 2022 (May 31, 2022): 1–7. http://dx.doi.org/10.1155/2022/5040766.

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Although online ride-hailing supplies the nearest taxi matching for riders, the potential leakage of riders’ hobbies and physical condition raises privacy concerns. Since most of the privacy-preserving schemes do limited matching of riders and drivers in the same zone, in this paper, we propose a novel privacy-preserving cross-zone ride-matching scheme, namely, Cride, which extends one zone into multiple neighboring zones. Based on the zone division of a city, CRide allows distance computation between rider and driver across adjacent zones in the encrypted domain. Furthermore, towards efficien

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Shayakhmetov, N. M., and D. Y. Aizhulov. "Identification and research of factors affecting the optimal distribution of well flow rates in space." Bulletin of the National Engineering Academy of the Republic of Kazakhstan 82, no. 4 (2021): 204–14. http://dx.doi.org/10.47533/2020.1606-146x.134.

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The paper discusses and research the factors affecting the filtration rate to reduce stagnant zones in the domain and spreading outside the block under consideration. The main hydrodynamic factors in production by In-Situ Leaching are the distribution of permeability in the reservoir and well flow rates. The study of the factors was carried out on the basis of mathematical models using Darcy Law and Law of Conservation of Mass. Calculation was accomplished on a two-dimensional area with an isotropic and non-uniform permeability distribution to determine the effect of permeability on the leache

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Lins dos Santos, Bianca, João Paulo Rodrigues dos Santos, José Damião Saraiva Gomes-Júnior, et al. "Association of aerobic capacity and muscular strength with health-related quality of life in adolescents: A school-based cross-sectional study." Retos 64 (January 15, 2025): 176–87. https://doi.org/10.47197/retos.v64.110467.

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Background: The independent associations of aerobic capacity and muscular strength on health-related quality of life (HRQoL), when mutually adjusted, remain understudied, particularly in adolescents. Aim: To examine the association between aerobic capacity, muscle strength, and HRQoL in adolescents. Methods: A cross-sectional design was employed, including 202 Brazilian adolescents. Aerobic capacity was assessed using the PACER test and categorized into “healthy zone”, “needs improvement”, and “at risk”. Muscle strength was evaluated through field tests, including the 90º push-up, and categori

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Kim, Ho Bang, and Chung Sun An. "Differential Expression Patterns of an Acidic Chitinase and a Basic Chitinase in the Root Nodule of Elaeagnus umbellata." Molecular Plant-Microbe Interactions® 15, no. 3 (2002): 209–15. http://dx.doi.org/10.1094/mpmi.2002.15.3.209.

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Two cDNA clones encoding chitinase were isolated from a root nodule cDNA library of Elaeagnus umbellata by the hybridization-competition method. The two clones, EuNOD-CHT1 and EuNOD-CHT2, encode for 335 and 317 amino acid residues with the molecular mass of mature proteins being 33.3 and 31.1 kDa, respectively. The two chitinases showed similar protein structures consisting of four domains: hydrophobic signal peptide domain, cysteine-rich chitin-binding domain, hinge domain, and catalytic domain. The EuNOD-CHT1 gene showed similar expression levels in root nodules and leaves, with no detection

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Cawood, Peter A., Jeroen A. M. van Gool, and Greg R. Dunning. "Geological development of eastern Humber and western Dunnage zones: Corner Brook–Glover Island region, Newfoundland." Canadian Journal of Earth Sciences 33, no. 2 (1996): 182–98. http://dx.doi.org/10.1139/e96-017.

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The Corner Brook–Glover Island region records the development of the internal domain of the Humber Zone and its relationship to the adjoining external domain and Dunnage Zone. The region preserves both the Laurentian margin basement–cover contact and the siliciclastic–carbonate transition within the cover sequence. Precambrian Grenville basement of the Corner Brook Lake Complex is the oldest lithostratigraphic unit and yielded a U/Pb zircon age of 1510 ± 6 Ma. Three main lithostratigraphic assemblages overlie basement: silicic and mafic igneous rocks of the Lady Slipper Pluton which yielded a

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St-Onge, M. R., S. B. Lucas, and R. R. Parrish. "Terrane accretion in the internal zone of the Ungava orogen, northern Quebec. Part 1: Tectonostratigraphic assemblages and their tectonic implications." Canadian Journal of Earth Sciences 29, no. 4 (1992): 746–64. http://dx.doi.org/10.1139/e92-064.

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The tectonostratigraphic record of the Ungava orogen contains evidence for the interaction of divergent, transform, and convergent plate boundaries over a > 0.2 Ga period in the Early Proterozoic. Three principal tectonic domains are recognized: (1) autochthonous basement plutonic and supracrustal rocks of Archean age; (2) autochthonous and allochthonous sedimentary and volcanic units associated with a ca. 1.99–1.92 Ga rift-to-drift margin; and (3) "suspect' ' crustal components of a ca. 2.00 Ga ophiolite and ca. 1.90–1.83 Ga island-arc terrane. Domain 1 is the stratigraphic or structural b

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Luebbers, R. J., K. S. Kunz, M. Schneider, and F. Hunsberger. "A finite-difference time-domain near zone to far zone transformation (electromagnetic scattering)." IEEE Transactions on Antennas and Propagation 39, no. 4 (1991): 429–33. http://dx.doi.org/10.1109/8.81453.

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Calamia, Paul T., and U. Peter Svensson. "Time‐domain edge‐diffraction calculations near zone boundaries." Journal of the Acoustical Society of America 118, no. 3 (2005): 1970–71. http://dx.doi.org/10.1121/1.4781756.

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Donzé, Frédéric-Victor, Alexandra Tsopela, Yves Guglielmi, Pierre Henry, and Claude Gout. "Pressurized fluid flow within the mechanical stability domain of fault zones in shale." E3S Web of Conferences 98 (2019): 01013. http://dx.doi.org/10.1051/e3sconf/20199801013.

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Fracture interaction mechanisms and reactivation of natural discontinuities under fluid pressurization conditions inside fault zone can represent critical issues in risk assessment of caprock integrity. A field injection test, carried out in a damage fault zone at the decameter scale i.e. mesoscale, has been studied using a Distinct Element Model. Considering the complex structural nature of a fault zone, the contribution of fracture sets on the bulk permeability has been investigated during a hydraulic injection. It has been shown that their orientation for a given in-situ stress field plays

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Mercer, C., J. R. Williams, D. R. Clarke, and A. G. Evans. "On a ferroelastic mechanism governing the toughness of metastable tetragonal-prime ( t ′) yttria-stabilized zirconia." Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 463, no. 2081 (2007): 1393–408. http://dx.doi.org/10.1098/rspa.2007.1829.

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This article investigates the toughness of yttria-stabilized zirconia (YSZ) with the tetragonal-prime ( t ′) structure. Such materials are used as durable thermal barriers in gas turbines. Their durability has been attributed to high toughness, relative to materials in the cubic phase field. Based on prior literature, a ferroelastic toughening mechanism is hypothesized and this assertion is examined by characterizing the material in the wake of an indentation-induced crack. Assessment by transmission electron microscopy, Raman spectroscopy and optical interferometry has affirmed the existence

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Culshaw, Nicholas, Peter Reynolds, Gavin Sinclair, and Sandra Barr. "Amphibole and mica 40Ar/39Ar ages from the Kaipokok and Aillik domains, Makkovik Province, Labrador: towards a characterization of back-arc processes in the Paleoproterozoic." Canadian Journal of Earth Sciences 39, no. 5 (2002): 749–64. http://dx.doi.org/10.1139/e01-097.

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We report amphibole and mica 40Ar/39Ar ages from the Makkovik Province. Amphibole ages from metamorphic rocks decrease towards the interior of the province, indicating a first-order pattern of monotonic cooling with progressive migration of the province into a more distal back-arc location. The amphibole data, in combination with muscovite ages, reveal a second-order pattern consisting of four stages corresponding to changing spatial and temporal configurations of plutonism and deformation. (1) The western Kaipokok domain cooled through muscovite closure by 1810 Ma, long after the cessation of

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CARPENTER, R. L., and N. A. DUKE. "Geological Setting of the West Meliadine Gold Deposits, Western Churchill Province, Nunavut, Canada." Exploration and Mining Geology 13, no. 1-4 (2004): 49–65. http://dx.doi.org/10.2113/gsemg.13.1-4.49.

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Abstract The West Meliadine area is underlain by structurally interleaved panels of mafic and minor ultramafic metavolcanic rocks and metasedimentary rocks that occur along the northern margin of the Neoarchean Rankin Inlet greenstone belt. Three structural and metamorphic domains are recognized: (1) the easterly Wesmeg domain; (2) the central Barracuda-Ridge domain; and (3) the westerly Peter Lake domain. The Wesmeg domain is characterized by a series of southeast-trending, north-dipping, foliation-parallel panels of greenschist facies mafic metavolcanic and metasedimentary rocks. The Barracu

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Michard, André, Abdelkader Mokhtari, Ahmed Chalouan, Omar Saddiqi, Philippe Rossi, and Ech-Cherki Rjimati. "New ophiolite slivers in the External Rif belt, and tentative restoration of a dual Tethyan suture in the western Maghrebides." Bulletin de la Société Géologique de France 185, no. 5 (2014): 313–28. http://dx.doi.org/10.2113/gssgfbull.185.5.313.

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AbstractOphiolite slivers have been described recently in the core of the External zones of the Central Rif belt. The present work aims at illustrating new ophiolite slivers further east and discussing the structural position and tectonic emplacement of all these oceanic floor remnants. Their basement consists of gabbros previously dated at 166±3 Ma and their cover includes mafic breccias, micrites and radiolarites. These oceanic slivers are located within the Mesorif nappe stack at the bottom of the Senhadja nappe that roots beneath the Intrarif Ketama unit and was thrust over the more extern

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Li, Chao, Jiagui Xie, Yanan Cheng, et al. "Research on the Construction of High-Trust Root Zone File Based on Multi-Source Data Verification." Electronics 12, no. 10 (2023): 2264. http://dx.doi.org/10.3390/electronics12102264.

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The root zone is located at the top level of the DNS system’s hierarchical structure and serves as the entry point for all domain name resolutions. The accuracy of the root zone file determines whether domain names can be resolved correctly. To solve the problems of single-source distrust and inaccurate data in the use of root zone files, this paper utilizes multi-source root zone files to build an accurate, real-time, and highly trustworthy root zone file through the validation of data accuracy and integrity. First, we propose a weighted voting statistical verification method. We select top-l

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Cureton, James S., Ben A. van der Pluijm, and Eric J. Essene. "Nature of the Elzevir–Mazinaw domain boundary, Grenville Orogen, Ontario." Canadian Journal of Earth Sciences 34, no. 7 (1997): 976–91. http://dx.doi.org/10.1139/e17-081.

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The Mooroton shear zone (MSZ) of the Metasedimentary Belt of the Grenville Orogen in Ontario separates the Mazinaw domain to the east from the Elzevir domain. The shear zone is composed of mafic metavolcanic, metaclastic, and marble mylonites, and is characterized by a subvertical foliation, which crosscuts the regional foliation, and a near-vertical stretching lineation. Microstructures indicate deformation occurred under crystal–plastic conditions, and shear-sense indicators give movement of east (Mazinaw) side up. The geometry of the MSZ, which follows the eastern margin of the Elzevir tona

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Tsakou Sonwa, Cyrille Stephane, Jan van Bever Donker, and Russell Bailie. "Polyphase Deformation of the High-Grade Metamorphic Rocks along the Neusspruit Shear Zone in the Kakamas Domain: Insights into the Processes during the Namaquan Orogeny at the Eastern Margin of the Namaqua Metamorphic Province, South Africa." Minerals 11, no. 7 (2021): 759. http://dx.doi.org/10.3390/min11070759.

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The central part of the Namaqua Metamorphic Province was subjected to intense deformation under high-grade metamorphic conditions up to granulite facies, but also shows greenschist facies overprints denoting the metamorphic nature during the 1.2–1.0 Ga Namaquan Orogeny. This study examines the structural development of the central Kakamas Domain of the eastern Namaqua Metamorphic Province, which has not been extensively studied previously. The compressional orogenic phase is associated with D1 and D2 deformation events during which northeast–southwest-directed shortening resulted in southwest-

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Ma, Yuqi, Fangyuan Li, Jianbo Wu, Zhaoting Liu, Hui Xia, and Zhaoyuan Xu. "Detecting of Barely Visible Impact Damage on Carbon Fiber Reinforced Polymer Using Diffusion Ultrasonic Improved by Time-Frequency Domain Disturbance Sensitive Zone." Sensors 24, no. 10 (2024): 3201. http://dx.doi.org/10.3390/s24103201.

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Based on the decorrelation calculation of diffusion ultrasound in time-frequency domain, this paper discusses the repeatability and potential significance of Disturbance Sensitive Zone (DSZ) in time-frequency domain. The experimental study of Barely Visible Impact Damage (BVID) on Carbon Fiber Reinforced Polymer (CFRP) is carried out. The decorrelation coefficients of time, frequency, and time-frequency domains and DSZ are calculated and compared. It has been observed that the sensitivity of the scattered wave disturbance caused by impact damage is non-uniformly distributed in both the time an

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Radanovics, S., J. P. Vidal, E. Sauquet, A. Ben Daoud, and G. Bontron. "Optimising predictor domains for spatially coherent precipitation downscaling." Hydrology and Earth System Sciences Discussions 10, no. 4 (2013): 4015–61. http://dx.doi.org/10.5194/hessd-10-4015-2013.

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Abstract. Statistical downscaling is widely used to overcome the scale gap between predictors from Numerical Weather Prediction (NWP) models or General Circulation Models (GCMs) and predictands like local precipitation, required for example for medium-term operational forecasts or climate change impact studies. The predictors are considered over a given spatial domain which is rarely optimised with respect to the target predictand location. In this study the geopotential predictor domains used by an analogue downscaling method are optimised for 608 target zones covering France. An extended ver

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Tang, Jun, Wenye Zhu, and Xiaofei Li. "Personal sound zones in the short-time Fourier transform domain with relaxed reverberation." Journal of the Acoustical Society of America 157, no. 2 (2025): 778–96. https://doi.org/10.1121/10.0035578.

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Personal-sound-zones (PSZ) techniques deliver independent sounds to multiple zones within a room using a loudspeaker array. The target signal for each zone is clearly audible within that zone while inaudible or non-distracting in others, assured by applying pre-filters to the loudspeaker array. The pre-filters are traditionally designed with time-domain or frequency-domain methods, which suffer from high computational complexity and large system latency, respectively. This work proposes a subband pressure-matching method in the short-time Fourier transform domain using the convolutive transfer

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Yang, C. Y., Z. R. Huang, Y. Q. Zhou, C. Z. Li, W. H. Yang, and K. K. Fung. "TEM study of lanthanum aluminate." Proceedings, annual meeting, Electron Microscopy Society of America 48, no. 4 (1990): 1060–61. http://dx.doi.org/10.1017/s0424820100178434.

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Lanthanum aluminate(LaAlO3) single crystal as a substrate for high Tc superconducting film has attracted attention recently. We report here a transmission electron microscopy(TEM) study of the crystal structure and phase transformation of LaAlO3 by using Philips EM420 and EM430 microscopes. Single crystals of LaAlO3 were investigated first by optical microscope. Stripe-shaped domains of mm size are clearly seen(Fig.1a), and 90° domain boundary is also obvious. TEM specimens were prepared by mechanical grinding and polishing followed by ion-milling.Fig.lb shows μm size stripe domains of LaAlO3.

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Mardyani, Yeyen, Rahmat Kurnia, and Luky Adrianto. "STATUS PENGELOLAAN PERIKANAN SKALA KECIL BERBASIS ZONASI DI WILAYAH PERAIRAN KABUPATEN BANGKA." Jurnal Kebijakan Perikanan Indonesia 11, no. 2 (2019): 125. http://dx.doi.org/10.15578/jkpi.11.2.2019.125-137.

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Pemanfaatan wilayah perairan di sekitar Pulau Bangka oleh sektor perikanan khususnya perikanan skala kecil semakin terdesak akibat daerah penangkapan ikan (DPI) yang semakin berkurang dikarenakan wilayah Izin Usaha Pertambangan (IUP) di laut semakin bertambah. Hal ini menyebabkan ruang gerak nelayan semakin sempit. Penelitian ini bertujuan untuk menilai status keragaan pengelolaan perikanan skala kecil berdasarkan Zona DPI yang dibagi menjadi 3, yaitu Zona A (DPI dengan IUP aktif), Zona A1 (DPI dengan IUP non aktif), dan Zona B (DPI tanpa IUP). Status keragaan dinilai melalui pendekatan Ecosys

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Kim, Hyeongjun, Taejoo Kim, Won Jo, et al. "Multispectral Benchmark Dataset and Baseline for Forklift Collision Avoidance." Sensors 22, no. 20 (2022): 7953. http://dx.doi.org/10.3390/s22207953.

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In this paper, multispectral pedestrian detection is mainly discussed, which can contribute to assigning human-aware properties to automated forklifts to prevent accidents, such as collisions, at an early stage. Since there was no multispectral pedestrian detection dataset in an intralogistics domain, we collected a dataset; the dataset employs a method that aligns image pairs with different domains, i.e. RGB and thermal, without the use of a cumbersome device such as a beam splitter, but rather by exploiting the disparity between RGB sensors and camera geometry. In addition, we propose a mult

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Huang, C. S., S. Y. Yang, and H. D. Yeh. "Technical Note: Approximate solution of transient drawdown for constant-flux pumping at a partially penetrating well in a radial two-zone confined aquifer." Hydrology and Earth System Sciences 19, no. 6 (2015): 2639–47. http://dx.doi.org/10.5194/hess-19-2639-2015.

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Abstract. An aquifer consisting of a skin zone and a formation zone is considered as a two-zone aquifer. Existing solutions for the problem of constant-flux pumping in a two-zone confined aquifer involve laborious calculation. This study develops a new approximate solution for the problem based on a mathematical model describing steady-state radial and vertical flows in a two-zone aquifer. Hydraulic parameters in these two zones can be different but are assumed homogeneous in each zone. A partially penetrating well may be treated as the Neumann condition with a known flux along the screened pa

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Relf, C., H. A. Sandeman, and M. E. Villeneuve. "Tectonic and thermal history of the Anialik River area, northwestern Slave Province, Canada." Canadian Journal of Earth Sciences 36, no. 7 (1999): 1207–26. http://dx.doi.org/10.1139/e99-050.

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The Anialik River area in the northwestern Slave Province comprises two geological domains of different age and origin that were tectonically juxtaposed at ca. 2650 Ma. The older domain, the Kangguyak gneiss belt, comprises ca. 3300-2700 Ma orthogneisses and paragneisses, interpreted as the remnants of a Mesoarchean continental margin. The younger domain, the Anialik River greenstone belt, consists of ca. 2680 Ma mafic to felsic volcanic rocks interpreted to have formed in an ensimatic island-arc setting. Structural and geochronological evidence suggest collision of the two domains began aroun

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Perkins, Dexter. "Metamorphism of the Kisseynew gneisses and related rocks of the Reindeer Zone, Trans-Hudson Orogen, northern Saskatchewan." Canadian Journal of Earth Sciences 28, no. 10 (1991): 1664–76. http://dx.doi.org/10.1139/e91-148.

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In the Reindeer Zone of Saskatchewan, the mostly metasedimentary Kisseynew gneiss crops out in a 300 km wide belt extending from the Tabbernor Fault to the Manitoba border. Metamorphic grade varies from middle amphibolite to granulite facies. Associated with the main Kisseynew gneiss are metasedimentary rocks of the Glennie Domain, Attitti Block, and Hanson Lake Block. Sillimanite is the common aluminosilicate in most parts of the four domains. Andalusite occurs at several places within the southern Glennie Domain, in the southern Hanson Lake Block, and in the northern Flin Flon Belt. Kyanite,

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Radanovics, S., J. P. Vidal, E. Sauquet, A. Ben Daoud, and G. Bontron. "Optimising predictor domains for spatially coherent precipitation downscaling." Hydrology and Earth System Sciences 17, no. 10 (2013): 4189–208. http://dx.doi.org/10.5194/hess-17-4189-2013.

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Abstract. Statistical downscaling is widely used to overcome the scale gap between predictors from numerical weather prediction models or global circulation models and predictands like local precipitation, required for example for medium-term operational forecasts or climate change impact studies. The predictors are considered over a given spatial domain which is rarely optimised with respect to the target predictand location. In this study, an extended version of the growing rectangular domain algorithm is proposed to provide an ensemble of near-optimum predictor domains for a statistical dow

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Vaananen, H. K., H. Zhao, M. Mulari, and J. M. Halleen. "The cell biology of osteoclast function." Journal of Cell Science 113, no. 3 (2000): 377–81. http://dx.doi.org/10.1242/jcs.113.3.377.

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Osteoclasts are multinucleated cells responsible for bone resorption. They have developed an efficient machinery for dissolving crystalline hydroxyapatite and degrading organic bone matrix rich in collagen fibers. When initiating bone resorption, osteoclasts become polarized, and three distinct membrane domains appear: a ruffled border, a sealing zone and a functional secretory domain. Simultaneously, the cytoskeleton undergoes extensive re-organisation. During this process, the actin cytoskeleton forms an attachment ring at the sealing zone, the membrane domain that anchors the resorbing cell

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Haarhoff, J., and J. K. Edzwald. "Modelling of floc-bubble aggregate rise rates in dissolved air flotation." Water Science and Technology 43, no. 8 (2001): 175–84. http://dx.doi.org/10.2166/wst.2001.0492.

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The use of relatively simple, but conceptually sound mathematical models, is a powerful tool to identify and understand parameters that are critical to a process. In this paper, a model is presented which addresses the rise rate of floc-bubble aggregates in the DAF separation zone. The model uses Stoke's Law as a point of departure, which is then progressively extended to incorporate the non-sphericity of the aggregates, the non-laminar nature of their movement, the fractal nature of the flocs, the physical constraints of attaching bubbles to a floc, and the limit on bubble numbers imposed by

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Dombovari, Zoltan, and Gabor Stepan. "On the bistable zone of milling processes." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 373, no. 2051 (2015): 20140409. http://dx.doi.org/10.1098/rsta.2014.0409.

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A modal-based model of milling machine tools subjected to time-periodic nonlinear cutting forces is introduced. The model describes the phenomenon of bistability for certain cutting parameters. In engineering, these parameter domains are referred to as unsafe zones, where steady-state milling may switch to chatter for certain perturbations. In mathematical terms, these are the parameter domains where the periodic solution of the corresponding nonlinear, time-periodic delay differential equation is linearly stable, but its domain of attraction is limited due to the existence of an unstable quas

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Sergo, Anton G., and Ekaterina I. Romanenkova. "World Intellectual Property Organisation's experience in domain dispute resolution." Vestnik Tomskogo gosudarstvennogo universiteta. Pravo, no. 43 (2022): 151–63. http://dx.doi.org/10.17223/22253513/43/13.

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The current pace of development of information technology is such that no country's legal system can objectively keep up with its adequate regulation. As a consequence, the Internet community is looking for its own, equally reliable and effective, but fast and modern systems of fair resolution of conflicts that arise between the rightholders of various classic means of individualisation (usually trademarks) and domain names. In today's hightech world, the role and importance of domain names cannot be underestimated. They control destinies, prepare revolutions, crush cults and shape national po

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