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Journal articles on the topic 'Avaloka'

Author: Grafiati

Published: 28 July 2024

Last updated: 30 July 2024

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1

Potter, Joanna, Frederick J. Longstaffe, Sandra M. Barr, Margaret D. Thompson, and Chris E. White. "Altering Avalonia: oxygen isotopes and terrane distinction in the Appalachian peri-Gondwanan realmLaboratory for Stable Isotope Science (LSIS), The University of Western Ontario, Contribution 236." Canadian Journal of Earth Sciences 45, no. 7 (July 2008): 815–25. http://dx.doi.org/10.1139/e08-024.

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Distinct 18O depletion is characteristic of a large majority of the 620–550 Ma felsic igneous rocks of Avalonia in the northern Appalachian orogen. Neoproterozoic rocks in the Boston Avalon terrane have the lowest δ18OWR values (≥–3.1‰), followed by the Mira terrane in Cape Breton Island and the Caledonia terrane in New Brunswick (≥–1.2‰), the Avalon terrane in Newfoundland (≥+2.8‰), and the Antigonish Highlands in Nova Scotia (≥+5.3‰). In contrast, this depletion of 18O is observed in very few of the Paleozoic felsic igneous rocks from these Avalonian terranes, and also in very few of the Neoproterozoic and Paleozoic felsic igneous rocks from the inboard Ganderian terranes. The low-18O character of the Neoproterozoic igneous rocks is related to regional pervasive, post-magmatic alteration by predominantly meteoric-hydrothermal fluids (δ18OH2O ∼–6‰ to –4‰) at 200–450 °C. The alteration likely occurred during late Neoproterozoic transtensional extension of Avalonia. Large-scale fluid infiltration and circulation within the Avalonian crust accompanied this extension with development of pull-apart sedimentary basins and extension-related magmatism that were the prelude to Cambrian submergence of Avalonia. This regional 18O depletion provides a geochemical fingerprint by which Avalonia can be distinguished from other peri-Gondwanan terranes. These data suggest that Avalonia existed as a composite terrane on the Gondwanan margin in the Neoproterozoic, separate from Ganderia.

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2

Kaur, Dr Ramandeep. "Kadambari Ke Gadhyabaddh Sankshep : Ek Avalokan." Indian Journal of Applied Research 3, no. 11 (October 1, 2011): 260–61. http://dx.doi.org/10.15373/2249555x/nov2013/85.

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3

Pisarevsky, Sergei A., Phil J. A. McCausland, Joseph P. Hodych, Sean J. O’Brien, Jennifer A. Tait, and J. Brendan Murphy. "Paleomagnetic study of the late Neoproterozoic Bull Arm and Crown Hill formations (Musgravetown Group) of eastern Newfoundland: implications for Avalonia and West Gondwana paleogeography1This article is one of a series of papers published in CJES Special Issue: In honour of Ward Neale on the theme of Appalachian and Grenvillian geology." Canadian Journal of Earth Sciences 49, no. 1 (January 2012): 308–27. http://dx.doi.org/10.1139/e11-045.

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A paleomagnetic study of subaerial volcanic rocks and associated siltstones of the Ediacaran Bull Arm Formation in the Avalon Zone of Newfoundland revealed a stable bipolar, hematite-borne primary remanence supported by positive conglomerate, contact, and fold tests. Mean remanence directions in two distal areas (Bonavista and Argentia) are similar, indicating a low paleolatitude position of Avalonia at ∼570 Ma. Redbeds of the overlying ∼550 Ma Crown Hill Formation also carry a primary bipolar hematite-borne remanence with moderate inclination, indicating that Avalonia remained at low to medium paleolatitudes through the end of the Ediacaran. Combining our results with previously published paleomagnetic data of Avalonia suggests moderate-scale drift of Avalonia through low southern paleolatitudes through the latter half of the Ediacaran, providing a paleogeographic context for the development of the first complex metazoan life.

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4

Simpson, Louis. "Avalon." Hudson Review 56, no. 1 (2003): 101. http://dx.doi.org/10.2307/3852907.

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5

Nevins, A., and P. McCallion. "Avalon." Gerontologist 35, no. 2 (April 1, 1995): 285–86. http://dx.doi.org/10.1093/geront/35.2.285.

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6

Erckens, Hendrik, Gion-Andri Beusser, Cedric Pradalier, and Roland Siegwart. "Avalon." IEEE Robotics & Automation Magazine 17, no. 1 (March 2010): 45–54. http://dx.doi.org/10.1109/mra.2010.935792.

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7

Rao, K. V., M. K. Seguin, and E. R. Deutsch. "Paleomagnetism of Early Cambrian redbeds on Cape Breton Island, Nova Scotia." Canadian Journal of Earth Sciences 23, no. 9 (September 1, 1986): 1233–42. http://dx.doi.org/10.1139/e86-120.

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Results are reported from steeply dipping red sandstones collected at nine sites (45 samples) of the Lower Cambrian Morrison River and MacCodrum formations on southeast Cape Breton Island, which forms part of the Avalon terrane. Demagnetization studies indicate minimal overlap of stability spectra in thermal, alternating-field, and chemical treatments. A stable component (hematite) with high unblocking temperatures (680 °C) is dominant at all sites. Its mean direction corrected for geologic tilt is D = 281°, I = +32°, k = 97, giving a paleomagnetic pole (pole M) at 20°N, 146°W (dp, dm = 3°, 6°). The corresponding in situ direction is D = 147°, I = +59°, k = 97, with a pole M′ at 2°S, 39°W (dp, dm = 6°, 8°). Poles M and M′ were compared with published Paleozoic poles for the Avalon Zone and cratonic North America to test whether the magnetization originated before or after the Taconic (Ordovician) folding. It could have been acquired during deposition or early diagenesis (Early to Middle Cambrian), in which case the paleolatitude differences between Morrison River–MacCodrum and age-equivalent cratonic sites require a minimum 20° post-Early Cambrian displacement between Avalon Zone and craton. This is, however, difficult to verify, since a fold test is not possible and well-dated Cambrian poles from Avalonia are lacking. Three or four of the many post-Cambrian results from the Avalon and Gander zones were found to be comparable with pole M′, so that alternatively the Morrison River–MacCodrum magnetization could be a postfolding, Late Ordovician–Early Silurian or Late Devonian overprint.

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8

Stevenson, Deborah. "Avalon High." Bulletin of the Center for Children's Books 59, no. 6 (2006): 261. http://dx.doi.org/10.1353/bcc.2006.0123.

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9

Kamble, Sayali B., and Vedvati Bhapkar. "REVIEW ON AVALEHA KALPANA." International Journal of Research in Ayurveda and Pharmacy 9, no. 4 (September 8, 2018): 112–14. http://dx.doi.org/10.7897/2277-4343.094123.

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10

COCKS, L. R. M., W. S. MCKERROW, and C. R. VAN STAAL. "The margins of Avalonia." Geological Magazine 134, no. 5 (September 1997): 627–36. http://dx.doi.org/10.1017/s0016756897007425.

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During Cambrian and earliest Ordovician times, Avalonia was an area forming an integral part of the huge Gondwanan continent, probably along the northern margin of Amazonia, until in early Ordovician (late Arenig or Llanvirn) time it split off from Gondwana, leaving a widening Rheic Ocean to its south. Today, its southern margin with Gondwana extends northeast from east of Cape Cod, Massachusetts, through Nova Scotia north of the Meguma terrane, and thence below sea level to the south of Newfoundland. On the eastern side of the present Atlantic, the southern margin may separate southwest Portugal from the rest of the Iberian Peninsula; it can be traced eastwards with more certainty from the south Cornwall nappes to a line separating the Northern Phyllite Belt (on the southern margin of the Rhenohercynian terrane) and the Mid-German Crystalline High. There is no certain evidence of Avalonian crust to the northeast of the Elbe Line. The northern margin of Avalonia extends westwards from south of Denmark to the British Isles, where it merges with the Iapetus Ocean suture between Scotland and England. Traced westwards, it crosses Ireland and reappears in northern Newfoundland to the east of New World Island, where it may follow the trace of the Dog Bay Line and the Cape Ray Fault. Recent work suggests that the northern margin of Avalonia may clip the northern tip of Cape Breton Island in Nova Scotia, and then enter the North American mainland at the Bay of Chaleur; it may then be traced from north and west of the Popelogan and Bronson Hill arcs to Long Island Sound near Newhaven, Connecticut. The Cambrian to Devonian faunas reflect the history of Avalonia: initially they were purely Gondwanan but, as Ordovician time proceeded, more genera crossed firstly the Tornquist Ocean as it narrowed between Avalonia and Baltica to close in latest Ordovician and early Silurian times, and secondly the Iapetus Ocean, so that by the early Silurian most of the benthic shelly faunas, apart from the ostracods, were the same round the adjacent margins of all three palaeocontinents.

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11

Landing, Ed, and Gerd Geyer. "Comment on ‘New evidence for the Baltican cratonic affinity and Tonian to Ediacaran tectonic evolution of West Avalonia in the Avalon Peninsula, Newfoundland, Canada’." Precambrian Research 410 (August 2024): 107489. http://dx.doi.org/10.1016/j.precamres.2024.107489.

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12

Zemgulys, Andrea, Susan McCabe, and Bryher. "Visa for Avalon." Modern Language Studies 35, no. 1 (April 1, 2005): 91. http://dx.doi.org/10.2307/30039814.

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13

Manton, Jonathan. "Avalon Media System." Notes 74, no. 2 (2017): 296–99. http://dx.doi.org/10.1353/not.2017.0126.

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14

Darack, Ed. "Avalon Peninsula, Canada." Weatherwise 59, no. 5 (January 2006): 14–15. http://dx.doi.org/10.3200/wewi.59.5.14-15.

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15

Avalos, David. "The Avalos Chapel." Aztlán: A Journal of Chicano Studies 24, no. 1 (1999): 201–2. http://dx.doi.org/10.1525/azt.1999.24.1.201.

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16

Haspel, Paul. "Avalon Lost: Suburbanization and Its Discontents in Barry Levinson's Avalon." Journal of American Culture 31, no. 4 (October 29, 2008): 383–92. http://dx.doi.org/10.1111/j.1542-734x.2008.00685.x.

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17

Jaluthriya, Vasundhara, Swapnil Chaudhari, Biswajyoti Patgiri, and Prashant Bedarkar. "Pharmaceutical standardization of Agastyaharitaki Avaleha." Medical Journal of Dr. D.Y. Patil Vidyapeeth 13, no. 5 (2020): 541. http://dx.doi.org/10.4103/mjdrdypu.mjdrdypu_151_19.

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18

Badyal, Sakshi, Pramod Yadav, and PradeepKumar Prajapati. "Kamsaharitaki Avaleha – A critical review." Journal of Ayurveda 17, no. 2 (2023): 160. http://dx.doi.org/10.4103/joa.joa_146_21.

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19

Atkinson, Amy. "Avalon by Mindee Arnett." Bulletin of the Center for Children's Books 67, no. 7 (2014): 348–49. http://dx.doi.org/10.1353/bcc.2014.0210.

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20

Harty, Kevin J. "The Mists of Avalon." Arthuriana 11, no. 3 (2001): 121–22. http://dx.doi.org/10.1353/art.2001.0057.

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21

Freedman, Ariela. "Visa for Avalon (review)." Modernism/modernity 12, no. 3 (2005): 523–25. http://dx.doi.org/10.1353/mod.2005.0084.

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22

Rollston, Chris. "Hector Avalos: In Memoriam." Maarav 26, no. 1-2 (January 1, 2022): 5–6. http://dx.doi.org/10.1086/mar202226101.

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23

Roose, Antti, Helen Sooväli-Sepping, and Anni Müüripeal. "Avaliku ruumi mõiste areng ja tähendusväljad." Keel ja Kirjandus 63, no. 8-9 (September 2020): 677–90. http://dx.doi.org/10.54013/kk754a3.

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24

N M, Anusree, and M. S. Krishnamurthy. "PHARMACEUTICAL STUDY OF ARDRAKA MATHULUNGA AVALEHA." International Journal of Research in Ayurveda and Pharmacy 13, no. 01 (February 23, 2022): 32–35. http://dx.doi.org/10.7897/2277-4343.13018.

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The main objective of this study is to prepare Ardraka Mathulunga Avaleha according to the method prescribed in the authoritative reference, Yogaratnakara, Purvardha, Arochaka chikitsa 38-42 and its organoleptic and physio-chemical analysis. Methods: Ardraka Mathulunga Avaleha is prepared as per the classical method of Avaleha Kalpana using guda as the sweetening agent. Ardraka Mathulunga Avaleha contains Ardraka, Mathulunga and Guda as the major ingredients. It also contains 15 other drugs, which are added as prakshepa dravya. Results: The final product was of desired consistency and quality. Discussion: This research article deals with the pharmaceutical preparation of Ardraka Mathulunga Avaleha in four steps, its paka lakshana and organoleptic characteristics of the formulation. It also discusses the formulation's haematinic action and its ability to cure iron deficiency anaemia. Conclusion: From the pharmaceutical study, proper paka lakshanas of avaleha, the right consistency, time is taken for the preparation etc., are understood.

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25

Bande, Rushali, and Lalita patole. "Efficacy of Kushmanda avaleha in Karshya." International Journal of Herbal Medicine 11, no. 4 (January 1, 2023): 21–22. http://dx.doi.org/10.22271/flora.2023.v11.i4a.875.

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26

Kimpel, Richard. "The Mists of Avalon/Die Nebel von Avalon: Marion Zimmer Bradley's German Bestseller." Journal of American Culture 9, no. 3 (September 1986): 25–28. http://dx.doi.org/10.1111/j.1542-734x.1986.0903_25.x.

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27

Susruth, Priyanka, and Rohini Purohit. "A BOOK REVIEW ON VEERASIMHA AVALOKAM- CLASSICAL TEXT ON MEDICAL ASTROLOGY." International Ayurvedic Medical Journal 8, no. 9 (September 23, 2020): 4541–43. http://dx.doi.org/10.46607/iamj3908092020.

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Medical astrology is an ancient medical system that associates various parts of the body, diseases, drugs as under the influence of the sun, moon and planets along with twelve astrological signs. Each of the astrological sign is associated with different parts of the human body. Since there are not much text available regarding Medical Astrology, Veerasimha Avalokanam is treatise meant for the Vaidyas for the astrological diagnosis and treat-ment. This text is not much popular across India. Actual text is in sanskrit language. Translations are available in Malayalam, Hindi and English. It is because of this that the translation of the work done by Sri. K Narayan is noteworthy. Though Veerasimhans treatise is titled as astrological diag-nosis and treatment, its mainly meant for daily use by Vaidyas and useful for all students of Indian traditional medicine as a reference book for both diagnosis and treatment .yet at the same time it can also be used very effectively used by all the astrol-ogers who are keen on diagnosing the diseases with planetary positions and then prescribe the Prayaschitha Karmas and directing to appropriate Siddha or Ayurveda doctor, for timely medications and treatment. Thus, Veerasimha Avalokanam is a treatise on medical astrology that collects, corre-lates and present quotes related to various diseases and their astrology, karma Vipaka, Prayaschittas and Ayurveda presents them in one place, truly a courageous lions’ efforts.

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28

Venot-Tisserand, Claire. "Vernègues (Bouches-du-Rhône). Avalon." Archéologie médiévale, no. 45 (December 1, 2015): 197. http://dx.doi.org/10.4000/archeomed.7661.

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29

Lemos, Antonio A. Briquet de. "E quem avalia os índices?" Cadernos de Saúde Pública 13, no. 3 (September 1997): 352–53. http://dx.doi.org/10.1590/s0102-311x1997000300001.

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30

Orelli, Brian. "GSK shares spoils with Avalon." Nature Biotechnology 31, no. 7 (July 2013): 579. http://dx.doi.org/10.1038/nbt0713-579a.

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31

Aygun, Ayla. "The Romantic Shadows of Avalon." Children's Literature Association Quarterly 17, no. 4 (1992): 38. http://dx.doi.org/10.1353/chq.0.0980.

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32

Sistermann, Rolf. "Der gehörnte Gott von Avalon." Zeitschrift für Pädagogik und Theologie 40, no. 1 (January 1, 1988): 87–99. http://dx.doi.org/10.1515/zpt-1988-400110.

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33

Murphy, J. Brendan, J. Duncan Keppie, Mary Pat Cude, Jarda Dostal, and John W. F. Waldron. "Geochemical and isotopic characteristics of Early Silurian clastic sequences in Antigonish Highlands, Nova Scotia, Canada: constraints on the accretion of Avalonia in the Appalachian – Caledonlde Orogen." Canadian Journal of Earth Sciences 33, no. 3 (March 1, 1996): 379–88. http://dx.doi.org/10.1139/e96-028.

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Avalonia is a terrane that accreted to Laurentia–Baltica during the development of the Appalachian–Caledonide Orogen. Interpretations of the timing of accretion have been constrained by comparing faunal affinities, overstep sequences, age and kinematics of inferred accretionary deformational events, and controversial paleomagnetic data. We show that the time of accretion of Avalonia may also be constrained by contrasts in the geochemical and isotopic signatures of its igneous rocks (which reflect the characteristics of the underlying continental basement and mantle) and sedimentary rocks (which reflect provenance). Early Silurian clastic sedimentary rocks of the Beechill Cove Formation, Antigonish Highlands, Nova Scotia, were deposited on Avalonian crust. The formation predominantly consists of approximately 80 m of siltstones and shales deposited in a nearshore environment and derived from the northeast. Their age is constrained by paleontological data and by directly underlying Late Ordovician – Early Silurian bimodal volcanic rocks that have typically Avalonian geochemical signatures. In comparison with typical Avalonian rocks, the Beechill Cove sediments are characterized by high SiO2, Ce/Yb, and initial 87Sr/86Sr, low Fe2O3, MgO, and TiO2, and strongly negative εNd(ur). These characteristics cannot be attributed to erosion of underlying Avalonian basement or coeval volcanic rocks and are consistent with derivation via significant transport from radiogenically enriched continental crust. εNd data are typical of Grenvillian basement compositions and suggest that the Beechill Cove sedimentary rocks were derived from an adjacent landmass with Grenvillian crust. The data, in conjunction with paleocontinental reconstructions and recent geochronological and structural data from the northern Appalachians, suggest that the Caledonide orogenic belt is the most likely source. Deposition of the Beechill Cove Formation is inferred to have occurred in an intracontinental basin associated with strike-slip tectonics during the oblique collision of the Avalon with Laurentia–Baltica.

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34

McCONNELL, BRIAN, and JOHN MORRIS. "Initiation of Iapetus subduction under Irish Avalonia." Geological Magazine 134, no. 2 (March 1997): 213–18. http://dx.doi.org/10.1017/s0016756897006626.

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The Dowery Hill Member of metamorphosed basalt, dolerite and siltstone is here recognized as the oldest exposed volcanic unit of the Lower Ordovician Ribband Group, with a minimum age of early Arenig. Peperites and resedimented hydroclastic breccia demonstrate a volcanic origin for the basalts. The igneous rocks are tholeiitic, with a trace element geochemistry indicative of a subduction-modified fertile mantle source, which we interpret as recording an early stage of volcanic arc evolution. The member is therefore the oldest known component of the volcanic arc generated by subduction of Iapetus oceanic lithosphere under southeastern Ireland. Subduction started earlier than predicted by current plate tectonic models, and these should be re-evaluated.

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35

Torsvik, Trond H., and Emma F. Rehnström. "The Tornquist Sea and Baltica–Avalonia docking." Tectonophysics 362, no. 1-4 (February 2003): 67–82. http://dx.doi.org/10.1016/s0040-1951(02)00631-5.

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36

Hingson, Jesse. "“Savages” into Supplicants: Subversive Women and Restitution Petitions in Córdoba, Argentina During the Rosas Era." Americas 64, no. 1 (July 2007): 59–85. http://dx.doi.org/10.1353/tam.2007.0106.

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In response to an anti-Federalist insurgency within the province of Córdoba in 1840, Manuel López, the governor (r. 1835-1852) and staunchally to Juan Manuel de Rosas, issued a directive to all provincial judges to round up all suspected Unitarians and their families, seize their property, and strip them of their citizenship. In following these orders, Pedro José García, the local juez de paz (Justice of the Peace), the principle law enforcement body of Pueblo de la Toma in the heart of Córdoba province, proceeded to the farmhouse of Faustino Avalo, who had recently been “classified” as a “savage Unitarian,” a political label describing any person opposing Federalist rule. García charged Avalos with secretly aiding and abetting Unitarian armies, which had passed through the province during the anti-Federalist uprisings in the previous year. As evidence of his guilt, according to the confiscation order, Avalos went missing for weeks and was nowhere to be found. Indeed, when García arrived, only Avalos's wife, María Juana Villafáñez, and their ten children remained. Nevertheless, García, along with two other “trusted” witnesses, read the order and confiscated the entire family's property. Villafáñez and her children could only watch helplessly as their clothes, toys, furniture, and livestock were taken away in wagons and their house boarded up. Yet, García did not arrest nor imprison Villafáñez and her children; instead, they were allowed to stay with her brother, Gervasio, a well-known Federalist and one of the “trusted” witnesses to his sister's material loss and public humiliation.

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37

Mori, Bhumi, Cholera Mira, Patel K. S., and Kori V. K. "STABILITY STUDY OF MODIFIED MUSTA-TRIPHALADIAVALEHA WITH RESPECT TO BASELINE MICROBIAL PROFILE USED IN THALASSEMIA MAJOR." International Ayurvedic Medical Journal 8, no. 10 (October 18, 2020): 4578–86. http://dx.doi.org/10.46607/iamj0208102020.

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Introduction: stability study of Modified Musta- Triphaladi Avaleha was done for 12 months (1 year) to know the stability of formulation in reference of its phyto-constituents and microbial growth therein. Modi-fied Musta-Triphaladi Avaleha have been used in Thalassemia children as an adjuvant therapy prepared with various herbal product. Methods: Modified Musta-Triphaladi Avaleha was made in Pharmacy with standard classical method (Avaleha Kalpana) as per AFI part-1 (The Ayurvedic formulary of India, part-1 part- A) In present study, stability with respect to its Microbial profile of Modified Musta-Triphaladi Ava-leha carried out. Avaleha was stored in 2 plastic containers during different climatic condition. Avaleha were studied at regular intervals for a period of 1 month to analysis Mycological findings and presence of Microorganisms by wet mount preparation and Gram stain test respectively. Results: At the end of study both Avaleha container has not present of microbes after 1 year of preparation, even in different climate and temperature. Conclusion: Since it is traditional Avaleha kalpana, the shelf life period was about one year (Sharangdhar Samhita) The presented study reflects that Microbiological findings of Modified Musta-Triphaladi Avaleha was negative at room temperature, warm and cold, dry and humid condition.

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38

Hamer, D. W., C. R. Blecher, and R. W. Duell. "Registration of ‘Avalon’ Salt Meadow Cordgrass." Crop Science 28, no. 1 (January 1988): 193. http://dx.doi.org/10.2135/cropsci1988.0011183x002800010058x.

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39

Kennedy, Elizabeth. "Artifacts from Careel Bay and Avalon." Mankind 1, no. 9 (February 10, 2009): 229–31. http://dx.doi.org/10.1111/j.1835-9310.1934.tb00076.x.

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40

Ratzlaff, Robert A., Juan G. Ripoll, Kristin A. Cushenbery, Philip E. Lowman, and José L. Díaz-Gómez. "Transthoracic Echocardiogram-Guided Avalon Catheter Repositioning." Anesthesia & Analgesia 125, no. 1 (July 2017): 48–51. http://dx.doi.org/10.1213/ane.0000000000001909.

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41

Kahloon, Rehan, Muhammad Asif Mangi, and George V. Moukarbel. "Migrated Avalon Elite Venovenous ECMO Cannula." JACC: Cardiovascular Interventions 12, no. 18 (September 2019): e161-e162. http://dx.doi.org/10.1016/j.jcin.2019.05.023.

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42

NEWMAN, A. T., and P. J. HAWKER. "The Avalon Lakes: An Environmental Opportunity." Water and Environment Journal 5, no. 1 (February 1991): 66–71. http://dx.doi.org/10.1111/j.1747-6593.1991.tb00589.x.

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43

Yewale, Prasad Gajanan, Swapnali Mate, and Utkarsha Khaire. "A Comparative Clinical Study on the effect of Vachadi Avaleha versus Mustakadi Avaleha in the management of Pratishyaya (~Recurrent Rhinitis) in school going children: A Single-blind Randomized Control Trial." International Journal of Ayurvedic Medicine 14, no. 3 (October 3, 2023): 734–40. http://dx.doi.org/10.47552/ijam.v14i3.3665.

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Background: In Ayurveda, Pratishyaya (~Recurrent Rhinitis) is described in Shiro-roga (Head disease).Pratishyaya (~Recurrent Rhinitis) is a common disease of childhood and it is well known for its recurrence. Immature Dhatu (tissues) state in children makes them more susceptible to recurrent infections. Clinical features of Pratishyaya (~Recurrent Rhinitis) can be correlated with rhinitis. Aim & Objective: To study the effect of vachadi avaleha and mustakadi avaleha in management of pratishyaya (~recurrent rhinitis). To study comparative efficacy of vachadi avaleha and mustakadi avaleha in management of pratishyaya(~recurrent rhinitis). Material & Method: Study comprises total 60 patients of Pratishyaya (~recurrent rhinitis) randomly divided into two equal groups. Group A (Experimental group) was treated with Vachadi avaleha two times a day after meal with honey and Group B (Control group) was treated with Mustakadi Avaleha administered two times a day after meal for 90 days. Patients were assessed for subjective parameters like rhinorrhoea, sneezing, nasal congestion, recurrence of rhinitis, duration of rhinitis per episode. Patients were assessed on every 30th day till completion of study period. Result- The effect of Mustakadi Avaleha (Group B) is significant at p<0.05 for subjective criteria such as nasastrava (rhinorrhoea), kshavathu (sneezing), and nasavarodha (nasal congestion) of pratishyaya (~Recurrent Rhinitis). Conclusion: Vachadi Avaleha is not as significant as Mustakadi avaleha in Pratishyaya (~Recurrent Rhinitis).

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Milovanović, Branko, Slavko Vasiljević, and Petko Vranić. "Designing and realization of the control networks of the telecommunication tower Avala." Tehnika 75, no. 6 (2020): 703–8. http://dx.doi.org/10.5937/tehnika2006703m.

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The Avala telecommunication tower was destroyed during the NATO bombing in 1999. The construction of the new tower at the same place started in 2007. The new tower consists of reinforced concrete part, with a total height of 142 m, and the antenna part with the height of 70 m. The body shape of the construction is a triangular prism with the equilateral triangle base with sides of 7 m. Civil engineering experts defined structure tolerance of 10 mm in the horizontal plane and 2 mm in the vertical plane. The design was produced pursuant to the principles of surveying profession and the conditions set. The paper describes the complexity of designing the control networks for high-rise buildings. The main tasks presented in this article are as follows: choosing the position of the control network points, defining the measuring plan, the network datum and the precision of measurements, calculation of the network quality criteria, and technical conditions for the realization of measurement.

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Patalia, AbhishekY, VirendraKumar Kori, KalpanaS Patel, and S. Rajagopala. "Efficacy of Triphaladi Avaleha on Beejadushtijanya Pandu (Thalassemia)." AYU (An International Quarterly Journal of Research in Ayurveda) 35, no. 1 (2014): 15. http://dx.doi.org/10.4103/0974-8520.141898.

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Rajagopala, S., B. Ravishankar, and BK Ashok. "Immunomodulatory activity of Vachadhatryadi Avaleha in albino rats." AYU (An International Quarterly Journal of Research in Ayurveda) 32, no. 2 (2011): 275. http://dx.doi.org/10.4103/0974-8520.92546.

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Woodcock, N. H., M. A. Awan, T. E. Johnson, A. H. Mackie, and R. D. A. Smith. "Acadian tectonics of Wales during Avalonia/Laurentia Convergence." Tectonics 7, no. 3 (June 1988): 483–95. http://dx.doi.org/10.1029/tc007i003p00483.

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Nance, R. Damian, J. Brendan Murphy, and J. Duncan Keppie. "A Cordilleran model for the evolution of Avalonia." Tectonophysics 352, no. 1-2 (July 2002): 11–31. http://dx.doi.org/10.1016/s0040-1951(02)00187-7.

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Zheng, Gong Ming, and Hai Zhang. "PWM Component Design Based on Avalon Specification." Applied Mechanics and Materials 229-231 (November 2012): 1994–97. http://dx.doi.org/10.4028/www.scientific.net/amm.229-231.1994.

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It could improve the design efficiency and shorten the development cycle by the means of integrating various user-defined peripheral driver in the rule of Avalon bus in the SOPC system. The PWM component with adjusted period and duty ratio has been achieved with hardware and software co-design method according to the Avalon bus specification in Nios Ⅱ embedded systems, and it had been tested to meet the application requirements completely

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Vilas Boas Reis, Émilien, and Vanessa Lemgruber. "As Brumas de Avalon: uma leitura ecofeminista." Revista Ártemis 29, no. 1 (July 16, 2020): 88–106. http://dx.doi.org/10.22478/ufpb.1807-8214.2020v29n1.52441.

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As teorias ecofeministas buscam responder sobre projeto de futuro e modelos de sociedade, respaldando-se em um futuro ancestral. A literatura, enquanto expressão cultural de uma época, traduz paradigmas de pensamento do seu tempo de gestação. O ecofeminismo cresce na década de 1970, mesmo período em que As Brumas de Avalon, de Marion Zimmer Bradley, são lançadas. Tal obra rememora um passado narrando estruturas matriarcais na sociedade e na religião. O objetivo deste artigo consiste em analisar os pontos ecofeministas presentes na referida ficção, utilizando autoras como Mary Mellor, Mary Daly e Ynestra King. Inicialmente, são apresentadas as bases do ecofeminismo. Em ato contínuo, explana-se o enredo para, finalmente, discutir e apontar os pontos de intersecção ecofeminista presente no livro. A metodologia utilizada é de base exploratória e hipotético-dedutiva, por meio de técnicas bibliográficas. As reflexões indicam que é possível o entendimento da manifestação ecofeminista em As Brumas de Avalon.

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