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Journal articles on the topic 'Chōon'

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Published: 4 June 2021

Last updated: 12 February 2022

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1

Oms, Oriol, Jaume Dinarès-Turell, Jordi Agustı́, and Josep M. Parés. "Refinements of the European Mammal Biochronology from the Magnetic Polarity Record of the Plio–Pleistocene Zújar Section, Guadix-Baza Basin, SE Spain." Quaternary Research 51, no. 1 (January 1999): 94–103. http://dx.doi.org/10.1006/qres.1998.2018.

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AbstractThe magnetobiostratigraphy study of the 130-m-thick Zújar section (Negratı́n clays unit, Guadix-Baza Basin, Spain) provides a remarkable opportunity to improve the correlation of European mammal biostratigraphy to the Geomagnetic Polarity Time Scale. The occurrence of 12 well-defined magnetozones and four paleontological sites with diagnostic faunas ranging from the MN 15 biozone (Ruscinian) to the MN 17 biozone (Villanyian), leads to an unambiguous correlation to chrons spanning from the Gilbert to the Matuyama epochs. This provides two new time constraints: (1) the boundary between MN 15 (Ruscinian) and MN 16 (Villanyian) biozones is recorded between chron C2An.3n and the base of chron C2An.2n and (2) the boundary between the upper and lower MN 16 subzones (Villanyian) is located between chron C2An.2n and the base of chron C2An.1n. The correlation between the Ruscinian–Villanyian boundary and the 3.3-myr-B.P. cooling event seems to be confirmed, while the early/late Villanyian boundary could be tentatively correlated to the glacial event at 2.6 myr B.P. Furthermore, MN 15 faunas are found in the lowermost part of chron C2Ar, which is in agreement with and reinforces the emplacement of the MN 14–MN 15 Ruscinian zones boundary at the reversal from chron 3n.1n to chron C2Ar.

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2

Cressey, Daniel. "Choon Fong Shih." Nature 461, no. 7262 (September 2009): 326. http://dx.doi.org/10.1038/461326a.

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3

Selmeczi, Ildikó, Miklós Lantos, Margit Bohn-Havas, András Nagymarosy, and Éva Szegő. "Correlation of bio- and magnetostratigraphy of Badenian sequences from western and northern Hungary." Geologica Carpathica 63, no. 3 (June 1, 2012): 219–32. http://dx.doi.org/10.2478/v10096-012-0019-1.

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Correlation of bio- and magnetostratigraphy of Badenian sequences from western and northern HungaryLithological, magnetostratigraphic and paleontological (nannoplankton, foraminifers, molluscs) studies were carried out on the Badenian successions of boreholes Sopron-89, Nagylózs-1 and Sáta-75 in Hungary. The correlations with the ATNTS2004 scale show that the Badenian sedimentation began during Chron C5Br thus the earliest Badenian deposits are missing in the sections. The first occurrence ofOrbulina suturalisBrönnimann has been observed in Subchron C5Bn.1r, at 14.9 Ma. Although it is older than the interpolated age of 14.74 Ma in Chron C5ADr in the ATNTS2004, it is consistent with the age of 15.1 Ma obtained from recent calibration of planktonic foraminiferal bioevents. The base of the Bulimina-Bolivina Zone has been determined at 13.7 Ma in Chron C5ABr, and the Badenian/Sarmatian boundary is recorded within Chron C5AAn, at 13.15 Ma.

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4

Prothero, Donald R., Elizabeth Draus, and Casey Burns. "Magnetostratigraphy and Tectonic Rotation of the Eocene-Oligocene Makah and Hoko River Formations, Northwest Washington, USA." International Journal of Geophysics 2009 (2009): 1–15. http://dx.doi.org/10.1155/2009/930612.

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The Eocene-Oligocene Makah Formation and subjacent middle Eocene Hoko River Formation of the northwestern Olympic Peninsula, Washington, yield mollusks, crustaceans, foraminifera, and early neocete whales; their age has never been precisely established. We sampled several sections; most samples showed a stable single-component remanence held largely in magnetite and passed a Class I reversal test. The upper Refugian (late Eocene) and lower Zemorrian (early Oligocene) rocks at Baada Point correlate with Chron C13r (33.7–34.7 Ma) and Chron C12r (30–33 Ma). The Ozette Highway section of the Makah Formation spanned the early Refugian to late Refugian, with a sequence that correlates with Chrons C15r-C13r (33.7–35.3 Ma), and a long reversed early Zemorrian section that correlates with Chron C12r (30–33 Ma). The type section of the Hoko River Formation correlates with Chron C18r (40.0–41.2 Ma). The area sampled shows about45∘of post-Oligocene counterclockwise tectonic rotation, consistent with results obtained from the Eocene-Oligocene rocks in the region.

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5

Wyatt, Justin. ": David Lynch . Michel Chion." Film Quarterly 50, no. 1 (October 1996): 43–44. http://dx.doi.org/10.1525/fq.1996.50.1.04a00120.

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6

김병학. "Gyeong-cheon-a-il-rok(Gyeong-cheon Daily News) and the Life of Anti-Japan Partisan Commander Kim Gyeong-cheon." Institute for Humanities and Social Sciences 14, no. 1 (April 2013): 191–218. http://dx.doi.org/10.15818/ihss.2013.14.1.191.

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7

Penwill, J. L. "Evolution of An Assassin: The Letters of Chion of Heraclea." Ramus 39, no. 1 (2010): 24–52. http://dx.doi.org/10.1017/s0048671x00000527.

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In 364 BCE Clearchus, a former student of Isocrates and Plato, staged a coup d'état in his native city of Heraclea Pontica and made himself tyrant. Twelve years later in 352 Clearchus fell victim to a conspiracy led by another former student of Plato and native Heraclean, by the name of Chion. Some centuries later an author whose name we do not know and about whose date and place of residence we can only speculate fixed on this event as the basis of a historical epistolary novel, which comprises a sequence of seventeen letters purportedly written by Chion himself. The novel survives in a number of manuscripts, the majority of which give it the title Letters of Chion. It is with this text that this article is concerned.The sequence tracks Chion's progress from the time he leaves home in order to pursue his studies at the Academy to two days before the assassination. Most of the letters are addressed to Chion's father Matris, and so fall into the category of ‘letters home’ in which Chion narrates and reflects on his encounters and thoughts at various stages of his sojourn abroad. The final one however is written from Heraclea back to Athens; it is addressed to Plato, and from its tone and content Chion clearly expects of his master that he regard the upcoming assassination as his student's graduation summa cum laude in the field of political ethics. Critical opinion on the Letters is largely unanimous in maintaining that the author shares this view; that the whole sequence is designed to show Chion developing the philosophical acumen needed to make the right decision on the on the ethical issues that confront him and the emotional maturity needed to take decisive political action at the appropriate time.

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8

Darewych, J. W. "Some exact solutions of reduced scalar Yukawa theory." Canadian Journal of Physics 76, no. 7 (June 3, 1998): 523–37. http://dx.doi.org/10.1139/p98-036.

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The scalar Yukawa model, in which a complex scalar field, ϕ, interacts via a real scalar field, χ, is reduced by using covariant Green functions. It is shown that exact few-particle eigenstates of the truncated QFT Hamiltonian can be obtained in the FeshbachVillars formulation if an unorthodox "empty" vacuum state is used. Analytic solutions for the two-body case are obtained for massless chion exchange in 3+1 dimensions and for massive chion exchange in 1+1 dimensions. Comparison is made to ladder BetheSalpeter, FeynmanSchwinger, and quasipotential results for massive chion exchange in 3+1. Equations for the three-body case are also obtained. PACS Nos.: 11.10.Ef, 11.10.Qr, and 03.70.+k

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9

Lane, Patrick. "A Conversation with Dan Chaon." Missouri Review 34, no. 3 (2011): 64–77. http://dx.doi.org/10.1353/mis.2011.0065.

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10

Wolfsteiner, Andreas. "SYNC.(CHRON)I(ZI)TÄT." Sprache und Literatur 36, no. 1 (December 17, 2005): 120–37. http://dx.doi.org/10.30965/25890859-036-01-90000010.

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11

Starossek, Uwe. "Shin Chon Bridge, Korea." Structural Engineering International 19, no. 1 (February 2009): 79–84. http://dx.doi.org/10.2749/101686609787398227.

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12

Chon, Margaret. "Remarks by Margaret Chon." Proceedings of the ASIL Annual Meeting 114 (2020): 314–16. http://dx.doi.org/10.1017/amp.2021.53.

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Thanks to Professor Dreyfuss for this invitation and to Professor Rutschman for her thought-provoking paper. Professor Rutschman is deeply engaged with the law of pharmaceutical innovation. And she is also deeply committed to a public health perspective. For many reasons, the two domains often speak past each other. Her paper provides a basis for shared vocabulary if not a common language.

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13

Cheon, Deok Hee, So Young Yim, and Gwang Ock Lee. "The Influence of Mentoring on the Mentee's Self-Efficacy and Job Engagement in the Travel Industry: Focusing on the Mediating Effect of Self-Efficacy in the System Converged with Information Technology." Convergence Tourism Contents Society 7, no. 2 (August 31, 2021): 149–62. http://dx.doi.org/10.22556/jctc.2021.7.2.149.

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14

WIERZBOWSKI, Andrzej. "The Lower Kimmeridgian of the Wieluń Upland and adjoining regions: lithostratigraphy, ammonite stratigraphy (upper Planula/Platynota to Divisum zones), palaeogeography and climate-controlled cycles." Volumina Jurassica, no. 1 (December 27, 2017): 41–120. http://dx.doi.org/10.5604/01.3001.0010.5659.

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The Early Kimmeridgian of the Wieluń Upland and adjoining regions, after the decline of sedimentation of the deep-neritic sponge megafacies (Częstochowa Sponge Limestone Fm.) and associated limestones and marls with poor benthic fauna (Pilica Fm.) during the Planula Chron, showed the subsequent development of moderately shallow-water biostromal chalky limestones with siliceous sponges and corals, replaced laterally by micritic limestones and marls (Prusicko Fm.) during the Platynota Chron and the earliest Hypselocyclum Chron. Towards the north and south shallow-marine carbonate platforms occurred (represented by deposits of the “oolitic” fm.), whereas towards the north-west and west deeper marine facies, represented initially by limestones with siliceous sponges (Częstochowa Sponge Limestone Fm.), and later during the Hypselocyclum Chron by bedded limestones and marls with ammonites (Burzenin Fm.) were deposited. This palaeogeographic pattern was controlled by the synsedimentary tectonics. The detailed biostratigraphical classification of the deposits studied from the Platynota to the Divisum zones, and their lithological character, enable the recognition of the primary sedimentary cyclicity by comparison with the well dated short eccentricity cycles in the coeval succession of south-eastern France. The two appendixes enclosed give the characteristics of: (1) the characteristics of the ammonite faunas especially of the families Ataxioceratidae and Aulacostephanidae (where two new species are established – Balticeras samsonowiczi sp. nov., and Rasenioides glazeki sp. nov.); (2) the newly established lithostratigraphical units: the Prusicko Fm., and the Burzenin Fm., and the smaller rank units (members, beds) recognized therein.

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15

Jeon, Young J., Jaeuk U. Kim, Hae J. Lee, Jeon Lee, Hyun H. Ryu, Yu J. Lee, and Jong Y. Kim. "A Clinical Study of the Pulse Wave Characteristics at the Three Pulse Diagnosis Positions of Chon, Gwan and Cheok." Evidence-Based Complementary and Alternative Medicine 2011 (2011): 1–9. http://dx.doi.org/10.1093/ecam/nep150.

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In this work, we analyze the baseline, signal strength, aortic augmentation index (AIx), radial AIx, time to reflection and P_T2 at Chon, Gwan, and Cheok, which are the three pulse diagnosis positions in Oriental medicine. For the pulse measurement, we used the SphygmoCor apparatus, which has been widely used for the evaluation of the arterial stiffness at the aorta. By two-way repeated measures analysis of variance, we tested two independent measurements for repeatability and investigated their mean differences among Chon, Gwan and Cheok. To characterize further the parameters that were shown to be different between each palpation position, we carried out Duncan's test for the multiple comparisons. The baseline and signal strength were statistically different () among Chon, Gwan and Cheok, respectively, which supports the major hypothesis of Oriental medicine that all of the three palpation positions contain different clinical information. On the other hand, aortic AIx and time to reflection were found to be statistically different between Chon and the others, and radial AIx and P_T2 did not show any difference between pulse positions. In the clinical sense, however, the aortic AIx at each palpation position was found to fall within the 90% confidence interval of normal arterial compliance. The results of the multiple comparisons indicate that the parameters of arterial stiffness were independent of the palpation positions. This work is the first attempt to characterize quantitatively the pulse signals at Chon, Gwan and Cheok with some relevant parameters extracted from the SphygmoCor apparatus.

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16

Montoya, David. "Hostilidad perpetua, transformaciones transitorias: Persona, cuerpo y moralidad entre los tsotsiles de Chamula, Chiapas / Perpetual hostility, transitory transformations: Person, body and morality between the tsotsiles of Chamula, Chiapas." Revista Trace, no. 78 (July 31, 2020): 67. http://dx.doi.org/10.22134/trace.78.2020.735.

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El actual estudio etnográfico da cuenta de que lo chon –un aspecto de la persona, generalmente, asociado a lo animal– está relacionado con un estado de permanente hostilidad, presente en el mundo desde tiempos primordiales. Este aspecto, a la vez que potencia la vulnerabilidad entre los humanos, resalta la fortaleza de otros seres, como Dios y el Pukuj. En la búsqueda de lidiar con esa atmósfera de hostilidad y, de mitigar su propia vulnerabilidad, la humanidad experimenta múltiples transformaciones morales-corporales.Abstract: This ethnographic study shows that the chon –an aspect of the person, generally associated with the animal– is related to an state of permanent hostility, given in the world since primordial times. Although this aspect, while enhancing vulnerability among humans, highlights the strength of other beings such as God and the Pukuj. Therefore, to deal with this atmosphere of hostility and, therefore, to mitigate its own vulnerability, humanity undergoes multiple transformations moral-bodily. Keywords: chon; tsotsiles; humanity; vulnerability; morale.Résumé : Cette étude ethnographique montre que le chon –un aspect de la personne, généralment associé à l’animal– est lié à l’état d’hostilité qui caractérise le monde. Cet aspect, tout en renforçant la vulnérabilité des humains, met en évidence la force d’autres êtres tels que Dieu et les Pukuj. Dans sa quête pour faire face à cette atmosphère d’hostilité et, par conséquent, pour atténuer sa propre vulnérabilité, l’humanité subit de multiples transformations morales-corporelles.Mots-clés: chon ; tsotsiles ; vulnérabilité ; humanité ; moral.

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17

Cho, K. H., E. J. Lee, T. Tsuge, A. Jo, J. C. Kim, G. W. Cheong, H. S. Yoon, and G. T. Kim. "Comparative genomic analysis of Korean and Japanese green tea trees by using molecular markers." Canadian Journal of Plant Science 90, no. 3 (May 1, 2010): 293–98. http://dx.doi.org/10.4141/cjps09065.

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Although green tea is one of the most popular beverages in many countries, the evolutionary origin of Korean and Japanese green tea trees has not been extensively elucidated in a molecular level. Lineages of the five Korean green tea populations and cultivars growing in Hadong area were examined in comparison with the six Japanese and one Chinese cultivars using phylogenetic analysis and restriction fragment length polymorphism (RFLP) analysis with cleaved amplified polymorphic sequence (CAPS) markers. Molecular phylogenetic analyses using the non-transcribed region (NTS) region of the 5S rRNA suggested that the Korean Hadong cultivar was a minor variant of the Korean Hadong Cheon-nyeon wild tea plant, which has grown in the Hadong area more than 800 years. RFLP analysis with CAPS markers of the genes in phenylpropanoid biosynthetic pathway showed that all of the Korean Hadong wild tea populations and cultivar had unique polymorphism patterns, when compared with those of the six Japanese and one Chinese cultivars. In addition, Hadong Cheon-nyeon wild tea showed unique CAPS patterns in the phenylalanine ammonia-lyase (PAL) locus, indicating that the three CAPS markers in the PAL gene are sufficient to distinguish Hadong Cheon-nyeon wild tea from the others. Thus, our genetic analyses suggested that the Korean Hadong Cheon-nyeon wild tea plant might have evolved as a different lineage from the other wild green tea populations in the Hadong area or the Japanese tea cultivars. Key words: Restriction fragment length polymorphism, cleaved amplified polymorphic sequence marker, green tea, Hadong wild tea, evolutionary origin

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Lerbekmo, J. F., L. M. Heaman, H. Baadsgaard, K. Muehlenbachs, M. E. Evans, and A. R. Sweet. "Normal polarity magnetosubchrons in 24r and the age of the Paleocene–Eocene boundary." Canadian Journal of Earth Sciences 45, no. 7 (July 2008): 781–93. http://dx.doi.org/10.1139/e08-025.

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A late Paleocene to early Eocene sequence of flat-lying continental strata occurs in an area known as Obed Mountain, west-central Alberta. The upper 110 m consist of interbedded fluvial channel sandstones and overbank mudrocks containing five back swamp coal seams. Two coreholes, 3.5 km apart, that extend through the entire coal zone were sampled for magnetostratigraphy and 13C isotope analysis. Bentonites in the No. 1 (lowest) and No. 5 coal seams and a tuff in the No. 3 coal seam were sampled for U–Pb and (or) Rb–Sr dating of zircon and biotite, respectively. Magnetostratigraphic analysis of 520 samples identified the younger part of chron 25r, the whole of chron 25n and the older half of chron 24r. We find six normal polarity subzones in this part of chron 24r, which we correlate to tiny wiggles 6 to11 in marine magnetic profiles. Carbon isotope analysis of 14 samples from two cores revealed a negative shift of about 2‰ peaking near the base of 24r.8r. We interpret this as the carbon isotope excursion (CIE), the base of which is now accepted as defining the Paleocene–Eocene boundary. The thickness of the CIE in the Obed Mountain section implies that it lasted between 210 000 and 254 000 years. Radiometric dates of 58.4 ± 0.2, 57.7 ± 0.3, and 56.9 ± 0.8 Ma are obtained for the No. 1, No. 3, and No. 5 coals, respectively. Combining these with magnetostratigraphy and cyclostratigraphy yields an age of 57.1 ± 0.1 Ma for the Paleocene–Eocene boundary.

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HUSSON, DOROTHEE, BRUNO GALBRUN, NICOLAS THIBAULT, SILVIA GARDIN, EMILIA HURET, and RODOLFO COCCIONI. "Astronomical duration of polarity Chron C31r (Lower Maastrichtian): cyclostratigraphy of ODP Site 762 (Indian Ocean) and the Contessa Highway section (Gubbio, Italy)." Geological Magazine 149, no. 2 (November 25, 2011): 345–51. http://dx.doi.org/10.1017/s0016756811000999.

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AbstractThe duration of polarity Chron C31r is estimated with a cyclostratigraphic approach. Two sites are investigated: ODP Site 762 (Indian Ocean) and the Contessa Highway section (Gubbio, Italy). Cyclostratigraphic analysis is performed on greyscale variations (Site 762) and magnetic susceptibility variations (Contessa section). Both sites reveal an astronomical control of the sedimentation, highlighted by the identification of all the orbital periodicities. Cyclostratigraphic signals are tuned on 405 ka eccentricity cycles extracted from the La04 astronomical solution. In both sites, cycle counting gives an estimate of the duration of polarity Chron C31r of about 2.09 ± 0.03 Ma.

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20

Alvim, Luíza Beatriz. "Contraponto audiovisual? De Eisenstein a Chion." Revista FAMECOS 24, no. 2 (March 24, 2017): 24688. http://dx.doi.org/10.15448/1980-3729.2017.2.24688.

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Consideramos o termo musical “contraponto” tal como utilizado nos textos sobre cinema e teoria cinematográfica, a partir dos escritos de Eisenstein do final dos anos 20, passando por autores como Adorno e Eisler, Kracaeur e Jean Mitry até os estudos de som no audiovisual de Michel Chion. Temos como base o questionamento da possibilidade e pertinência ou não de sua aplicação às relações entre som e imagem em produtos audiovisuais, já que esta aplicação deu origem a diversos mal-entendidos, muitas vezes provocados por um uso genérico do termo. Fazemos referências a exemplos audiovisuais nos textos desses autores e acrescentamos outros, como o primeiro volume de As mil e uma noites (Miguel Gomes, 2015), Um filme como os outros (Jean-Luc Godard, 1968) e em filmes de Robert Bresson.

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21

Wyatt, Justin. "Review: David Lynch by Michel Chion." Film Quarterly 50, no. 1 (1996): 43–44. http://dx.doi.org/10.2307/1213332.

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22

Chang, Jamie. "A Conversation with Cheon Myeong-gwan." Azalea: Journal of Korean Literature & Culture 11, no. 1 (2018): 101–3. http://dx.doi.org/10.1353/aza.2018.0005.

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23

Rangan, Pooja. "Words on Screen by Michel Chion." Film Quarterly 71, no. 1 (2017): 119–21. http://dx.doi.org/10.1525/fq.2017.71.1.119.

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24

Poulakis, Nick. "Review of Audio-Vision: Sound on Screen." CINEJ Cinema Journal 8, no. 2 (December 3, 2020): 457–62. http://dx.doi.org/10.5195/cinej.2020.289.

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25

Alvim, Luíza. "O campo dos estudos de som no audiovisual, observação como método e audio-logo-visão: entrevista com Michel Chion." Revista Brasileira de Música 33, no. 1 (August 2, 2020): 465–86. http://dx.doi.org/10.47146/rbm.v33i1.37018.

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26

Haltia, E. M., and N. R. Nowaczyk. "Magnetostratigraphy of sediments from Lake El'gygytgyn ICDP Site 5011-1: paleomagnetic age constraints for the longest paleoclimate record from the continental Arctic." Climate of the Past 10, no. 2 (March 26, 2014): 623–42. http://dx.doi.org/10.5194/cp-10-623-2014.

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Abstract. Paleomagnetic measurements were performed on sediments drilled from ICDP Site 5011-1 in Lake El'gygytgyn (67°30' N, 172°05' E) located in Far East Russian Arctic. The lake partly fills a crater formed by a meteorite impact 3.58 ± 0.04 Ma ago. Sediments from three parallel cores (5011-1A, 5011-1B and 5011-1C), recovered from the middle part of the lake, yield a total of 355 m of sediment. Sediments are characterized by a variable lithology, where intervals of homogenous and laminated sediments alternate, and mass movement deposits occur frequently along the sediment profile. Mineral magnetic investigation made on sediments enclosed in core catchers suggests that magnetic carrier in these sediments is partly maghemitized Ti-rich pseudo-single domain magnetite. Its detrital origin can be shown by mineral magnetic measurements and SEM-EDS analyses performed on mini-sized cylindrical rock samples, polished rock sections and creek sediments. The intensity of the natural remanent magnetization in the sediments is high with a range from about 1 to 1000 mA m−1. Most of the sediments carry a stable magnetization interpreted as primary depositional remanent magnetization. Characteristic inclination data show alternating intervals of steep positive and negative inclinations that are used to assign magnetic polarity to the lake sediment profile. This is a rather straightforward procedure owing to the mainly high quality of data. The Matuyama/Gauss (M/G) (2.608 Ma) and Brunhes/Matuyama (B/M) (0.780 Ma) reversals were recognized in the sediments. The Mammoth and Kaena reversed subchrons were identified during the Gauss chron, and the Olduvai and Jaramillo normal subchrons as well as the Réunion and Cobb Mountain cryptochrons were identified during the Matuyama chron. Sediments also provide a record of the Olduvai precursor and Intra-Jaramillo geomagnetic excursions. Sediment deposition rate is highest at the base of the sequence laid down in the early Gauss chron, when the deposition rate is approximately 44 cm kyr−1. Sediment deposition decelerates upcore and it is an order of magnitude lower during the Brunhes chron in comparison with the early Gauss chron. Decrease in sediment deposition in the late Pliocene probably relates to atmospheric and oceanic reorganization heralding the onset of Quaternary climate change. The high-quality magnetostratigraphy reconstructed from Lake El'gygytgyn sediments provides 12 first-order tie points to pin down the age of the longest paleoclimate record from the continental Arctic.

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Wangkumhang, Pongsakorn, Alisa Wilantho, Philip J. Shaw, Laurence Flori, Katayoun Moazami-Goudarzi, Mathieu Gautier, Monchai Duangjinda, Anunchai Assawamakin, and Sissades Tongsima. "Genetic analysis of Thai cattle reveals a Southeast Asian indicine ancestry." PeerJ 3 (October 27, 2015): e1318. http://dx.doi.org/10.7717/peerj.1318.

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Cattle commonly raised in Thailand have characteristics ofBos indicus(zebu). We do not know when or how cattle domestication in Thailand occurred, and so questions remain regarding their origins and relationships to other breeds. We obtained genome-wide SNP genotypic data of 28 bovine individuals sampled from four regions: North (Kho-Khaolampoon), Northeast (Kho-Isaan), Central (Kho-Lan) and South (Kho-Chon) Thailand. These regional varieties have distinctive traits suggestive of breed-like genetic variations. From these data, we confirmed that all four Thai varieties areBos indicusand that they are distinct from other indicine breeds. Among these Thai cattle, a distinctive ancestry pattern is apparent, which is the purest within Kho-Chon individuals. This ancestral component is only present outside of Thailand among other indicine breeds in Southeast Asia. From this pattern, we conclude that a uniqueBos indicusancestor originated in Southeast Asia, and native Kho-Chon Thai cattle retain the signal of this ancestry with limited admixture of other bovine ancestors.

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Park, Kyung. "Hyeon Cheon-muk‘s National movement and Daejonggyo." Journal of Studies on Korean National Movement 90 (March 31, 2017): 213–50. http://dx.doi.org/10.19162/knm.90.2017.3.06.

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SaemioKim. "Yeon Cheon Hong Seok-Joo's Biji Scripts." Journal of Korean Literature in Classical Chinese ll, no. 47 (June 2011): 679–710. http://dx.doi.org/10.30527/klcc..47.201106.021.

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Shin, Jong-Ho, and In-Kun Lee. "Cheong Gye Cheon restoration in Seoul, Korea." Proceedings of the Institution of Civil Engineers - Civil Engineering 159, no. 4 (November 2006): 162–70. http://dx.doi.org/10.1680/cien.2006.159.4.162.

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Han, J., S. I. Gheyas, Y. Wang, D. R. Strongin, A. P. Graham, B. J. Hinch, and A. P. Wright. "Thermal Chemistry of CH3on Si/Cu(100)†." Journal of Physical Chemistry B 104, no. 14 (April 2000): 3078–84. http://dx.doi.org/10.1021/jp9928863.

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32

Moore, Matthew Dwight. "Review: Words on Screen, by Michel Chion." Afterimage 45, no. 1 (July 1, 2017): 27. http://dx.doi.org/10.1525/aft.2017.45.1.27.1.

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Prince, Stephen. ": Audio-Vision: Sound on Screen . Michel Chion." Film Quarterly 48, no. 4 (July 1995): 40–42. http://dx.doi.org/10.1525/fq.1995.48.4.04a00070.

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Em, Henry, Christine Hong, and Kim Dong-Choon. "Coda: A Conversation with Kim Dong-Choon." positions 23, no. 4 (November 2015): 837–49. http://dx.doi.org/10.1215/10679847-3148427.

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Moon, Cheon Woo, Geonyoung Kim, and Jerome Kartham Hyun. "Correction: Enhancing the plasmonic component of photonic–plasmonic resonances in self-assembled dielectric spheres on Ag." Journal of Materials Chemistry C 9, no. 5 (2021): 1836. http://dx.doi.org/10.1039/d1tc90014e.

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Correction for ‘Enhancing the plasmonic component of photonic–plasmonic resonances in self-assembled dielectric spheres on Ag’ by Cheon Woo Moon et al., J. Mater. Chem. C, 2021, DOI: 10.1039/d0tc05742h.

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36

Park, Young-Goo, Keun-Hyung Park, Seon Ha Lee, Sang-Lyong Oh, and Byeong-Choon Jeong. "Condemnation of Cheon-nyeon Cha Terminology in “Chloroplast Genome Analysis of Hadong Cheon-nyeon Cha (Camellia sinensis L.)”." Korean Tea Society 25, no. 4 (December 31, 2019): 87–88. http://dx.doi.org/10.29225/jkts.2019.25.4.87.

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37

Aubry, Marie-Pierre, Benjamin S. Cramer, Kenneth G. Miller, James D. Wright, Dennis V. Kent, and Richard K. Olsson. "Late Paleocene event chronology; unconformities, not diachrony." Bulletin de la Société Géologique de France 171, no. 3 (May 1, 2000): 367–78. http://dx.doi.org/10.2113/171.3.367.

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Abstract The chronology of the events associated with the late Paleocene thermal maximum (LPTM, Chron C24r) has been established through the construction of a composite reference section that involved chemomagnetobiostratigraphic correlations and assumed minimum diachrony of biostratigraphic events. On this basis, discrepancies between correlations in different sections were explained by inferred unconformities. However, diachrony between distant sections cannot be ruled out. We report here on two geographically close sections drilled onshore New Jersey that yield different records of chemomagnetobiostratigraphic correlations in the interval representing Chron C24r. Because of their proximity ( approximately 40 km apart), diachrony of biostratigraphic events between the two sections can be ruled out. In contrast, the marked lithologic disconformities in the sections explain well the different records of events. We thus conclude that the current relative chronology for Chron C24r is firmly based and that the upper Paleocene-lower Eocene stratigraphic record yields multiple unconformities, with Subzone NP9b rarely sampled. We examine the implications that undeciphered unconformities may have on the identification of proxies for paleoceanographic reconstruction, in particular with regard to the identification of the carbon isotope excursion (CIE) that reflects a dramatic latest Paleocene disturbance of the carbon cycle. We propose biostratigraphic means (short-lived calcareous nannoplankton and planktonic foraminifera taxa) that permit the unequivocal identification of the CIE not only in the oceanic realm but also in neritic settings.

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Fulton, R. J., E. Irving, and P. M. Wheadon. "Stratigraphy and paleomagnetism of Brunhes and Matuyama (>790 ka) Quaternary deposits at Merritt, British Columbia." Canadian Journal of Earth Sciences 29, no. 1 (January 1, 1992): 76–92. http://dx.doi.org/10.1139/e92-009.

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A succession of Quaternary deposits in the Merritt basin of south-central British Columbia contains evidence for four glaciations and two interglaciations. Paleomagnetic signatures in these sediments are of three types: normal polarity, proposed to have been acquired during the Brunhes Normal Polarity Chron; reversed polarity, proposed to have been acquired during the Matuyama Reversed Polarity Chron; and reversed polarity (Matuyama age) all but obscured by a normally magnetized overprint (Brunhes age).Reversely magnetized deposits at the base of the succession include glacial lacustrine deposits, interpreted as representing two different glaciations, and a paleosol and a succession of nonglacial sediments, which are evidence of two interglaciations. As the reversed polarity of these deposits is proposed to have been acquired during the Matuyama Reversed Polarity Chron, they are older than 790 ka.Normally magnetized deposits, which make up the rest of the succession, contain evidence for only two glaciations, but traces of other glaciations may have been removed during the erosion interval encompassed by a major unconformity that underlies deposits of the last glaciation. All are referred to the Brunhes Normal Polarity Zone. In addition to these glacial and interglacial deposits, a series of normally magnetized Quaternary basalt flows forms a bench 90 m above the floor of the basin. These basalts were extruded after 790 ka but before the penultimate glaciation.

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39

Koller, Jürgen. "Chon Tejedor: The Early Wittgenstein on Metaphysics, Natural Science, Language and Value." Zeitschrift für philosophische Literatur 3, no. 2 (May 27, 2015): 65–72. http://dx.doi.org/10.21827/zfphl.3.2.35363.

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40

Tao, Tao, Yunkun Zhang, Hui Wei, and Ke Heng. "Downregulation of IRAK3 by miR-33b-3p relieves chondrocyte inflammation and apoptosis in an in vitro osteoarthritis model." Bioscience, Biotechnology, and Biochemistry 85, no. 3 (December 10, 2020): 545–52. http://dx.doi.org/10.1093/bbb/zbaa105.

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ABSTRACT Interleukin-1 receptor-associated kinase-3 (IRAK3) has a distinctive role in regulating inflammation. However, the functional role of IRAK3 and regulatory mechanism underlying the pathogenesis of osteoarthritis (OA) remain unclear. Here, we first found that IRAK3 was upregulated, while miR-33b-3p was downregulated in the cartilage of OA patients and IL-1β-induced CHON-001 cells. IRAK3 was confirmed as the direct target of miR-33b-3p and negatively regulated by miR-33b-3p. There was an inverse correlation between IRAK3 mRNA expression and miR-33b-3p expression in OA cartilage tissues. The in vitro functional experiments showed that miR-33b-3p overexpression caused a remarkable increase in viability, a significant decrease in inflammatory mediators (IL-1β and TNF-α), and apoptosis in IL-1β-induced CHON-001 cells. Importantly, IRAK3 knockdown imitated, while overexpression reversed the effects of miR-33b-3p on IL-1β-induced inflammation and apoptosis in CHON-001 cells. Collectively, miR-33b-3p significantly alleviated IL-1β-induced inflammation and apoptosis by downregulating IRAK3, which may serve as a promising target for OA.

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Sea Ling Cheng. "Commentary on Hughes, Chon, and Ellerman." Violence Against Women 14, no. 3 (March 2008): 359–63. http://dx.doi.org/10.1177/1077801208314078.

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Burri, Josef, and Bernhard Uehleke. "Andrographis paniculata – Kalmegh, Fah thalai chon." Zeitschrift für Phytotherapie 40, no. 03 (July 2019): 120–21. http://dx.doi.org/10.1055/a-0827-8841.

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Andrographis paniculata (Wall), ein Akanthusgewächs, stammt ursprünglich aus Indien und Sri Lanka, ist mittlerweile in ganz Südostasien und etlichen anderen Ländern verbreitet. Als sehr bittere Medizin ist die Pflanze bei Kindern verhasst. Dennoch wird sie in den traditionellen Medizinsystemen Indiens, Chinas, Tibets, Thailands und Malaysias recht häufig verwendet. Sie wird auch als „indische Echinacea“ bezeichnet. In Thailand trägt sie den Namen „Fah thalai chon“, was ungefähr so viel bedeutet wie „Der Himmel vertreibt den Eindringling“ oder „Der Himmel schlägt den Räuber“, was durchaus der erwünschten medizinischen Wirkung entspricht. Sogar ein thailändischer Spielfilm trägt diesen Originaltitel, wohl weil Pflanze und Titel den Seelenzustand des Protagonisten treffend beschreiben („Tears of the Black Tiger“ von Wisit Sasanatieng, 2000). Warum Großmütter sehr viel Überzeugungsarbeit leisten müssen, um ihren kranken Enkelkindern den Kalmegh-Tee aufzuschwatzen, liegt in dessen Bitterkeit. Der Kalmegh hat also durchaus dramaturgische Qualitäten. Er ist die Bitterpflanze par excellence und darf in keinem häuslichen Kräutergarten Thailands fehlen.

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Oh, Bo-ra. "A Study on the Hong-cheon Poetry Society : Focused on the Linked Verses of the Hong-cheon Poetry Society." STUDY OF THE EASTERN CLASSIC 66 (March 31, 2017): 35–73. http://dx.doi.org/10.16880/sec.2017.66.02.035.

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이한영. "The Theological Understanding of ‘Bul-yeon-gi-yeon’ and ‘Yi-cheon-sig-cheon’ — Life, Justice, Peace and Daily Food." THEOLOGICAL THOUGHT ll, no. 186 (September 2019): 398–422. http://dx.doi.org/10.35858/sinhak.2019..186.014.

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45

Pardo Siabato, Camilo. "Cine para los oídos. Un estudio de caso: análisis de la propuesta sonora de la película Babel." Anuario electrónico de estudios en Comunicación Social "Disertaciones" 12, no. 2 (July 20, 2019): 197. http://dx.doi.org/10.12804/revistas.urosario.edu.co/disertaciones/a.6419.

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Este artículo busca mostrar la expresividad del sonido dentro del discurso narrativo de la propuesta sonora de la película Babel (2006) con un análisis basado en la metodología de Michel Chion y un diálogo con los diversos componentes cinematográficos.

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46

RILEY, TEAL R., and PHILIP T. LEAT. "Large volume silicic volcanism along the proto-Pacific margin of Gondwana: lithological and stratigraphical investigations from the Antarctic Peninsula." Geological Magazine 136, no. 1 (January 1999): 1–16. http://dx.doi.org/10.1017/s0016756899002265.

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Jurassic magmatism in western Gondwana produced the most voluminous episode of continental volcanism in the Phanerozoic era. During the Early to Middle Jurassic, some 2.5–3 million km3 of dominantly basalt, and to a lesser extent rhyolite, were erupted onto a supercontinent in the early stages of break-up. The major silicic portion of the Gondwana magmatic province is exposed in Patagonian South America. The volcanic rocks of Patagonia have been collectively termed the Chon-Aike Province and constitute one of the world's most voluminous silicic provinces. The volcanic rocks are predominantly pyroclastic, dominated by ignimbrite units of rhyolite composition. Volcanic rocks crop out sporadically across much of the once contiguous Antarctic Peninsula, and are considered to form an extension of the Chon-Aike Province. A continuation of the province to include the Antarctic Peninsula would extend its strike length along the active Pacific margin by c. 2000 km.Volcanic rocks exposed along the east coast of the Antarctic Peninsula, defined here as the Mapple Formation, are also dominated by rhyolitic ignimbrite flows, with individual units up to 80 m in thickness, and a total thickness of c. 1 km. The ignimbrites vary in degree of welding, from high-grade rheomorphic ignimbrites with parataxitic textures, to unwelded, lithic-rich ignimbrites. Rhyolite lava flows, air-fall horizons, debris flow deposits and epiclastic deposits are volumetrically minor, occurring as interbedded units within the ignimbrite succession.The lithology and stratigraphy of the Jurassic volcanic rocks of the Mapple Formation are presented, and comparisons are made to the Chon-Aike Province. A consistent stratigraphy of Permo-Triassic metasedimentary rocks, unconformably overlain by terrestrial mudstone–siltstone sequences, which are in turn conformably overlain by largely silicic, subaerial volcanic rocks, is present at several localities along the Antarctic Peninsula, and at localities in the Chon-Aike Province. Precise (zircon U–Pb) Middle Jurassic ages exist for two volcanic formations from the Antarctic Peninsula, and a Middle–Lower Jurassic age has been suggested for the underlying sedimentary formations based on fossil flora analysis. The Antarctic Peninsula chronostratigraphy, coupled with lithological similarities, indicate a close relationship to those sequences of the Chon-Aike province.

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47

Barendregt, René W., Randolph J. Enkin, Alejandra Duk-Rodkin, and Judith Baker. "Paleomagnetic evidence for multiple late Cenozoic glaciations in the Tintina Trench, west-central Yukon, CanadaThis article is a companion paper to Duk-Rodkin et al., also in this issue." Canadian Journal of Earth Sciences 47, no. 7 (July 2010): 987–1002. http://dx.doi.org/10.1139/e10-021.

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The Tintina Trench in west-central Yukon has preserved an extensive record of late Cenozoic preglacial, glacial, and interglacial deposits. These deposits comprise multiple sequences of tills, outwash, loesses, and paleosols. The sediments that were laid down directly by ice (tills) are of both local (montane) and regional (Cordilleran) provenance. The Tintina Trench area was impacted repeatedly by montane ice from the southern Ogilvie Mountains to the northwest (2500 m above sea level (asl)), and also repeatedly along its southern extent by Cordilleran ice from the Selwyn Mountains to the east (2759 m asl), the latter forming the continental divide in this region. We report here the magnetostratigraphy of three sections: Rock Creek (64°13′N, 139°07′W), West Fifteenmile River (64°29′N, 139°55′W), and East Fifteenmile River (64°23′N, 139°48′W). The majority of the units identified at these sections record late Pliocene to mid-Pleistocene glaciations, although relatively thin surficial sequences of late middle Pleistocene to late Pleistocene loesses and tills are present as well. Of the 11 units described in the Tintina Trench, seven have normal polarity, three have reversed polarity, and one has an undefined polarity. These units span about 3.0 million years. It appears that most of the polarity chrons and subchrons of the late Cenozoic are present and that the sequence of six reversals record at least 10 glaciations (three in the Brunhes Chron and seven in the Matuyama Chron), and 11 interglaciations (four in the Brunhes Chron and seven in the Matuyama Chron). The interglacials are recorded as either paleosols or unconformities between glacial or loess units having opposite polarity. While not all Matuyama Chron glacial and interglacial cycles recorded in marine isotopic records are seen on land, the terrestrial records found in the Tintina Trench have thus far proven to be the most complete in terms of the polarity record. While no absolute ages were obtained from the sediments in the trench, the extensive polarity sequence constrains the timing of glaciations to a considerably greater degree than was previously possible for this region. The magnetostratigraphy of the trench sites are compared with the glacial, glaciofluvial, and loessic deposits at the nearby Klondike River valley and Fort Selkirk sites, central Yukon, where tephras and basalts provide absolute ages, and stratigraphic units contain an extensive late Cenozoic climate proxy for northwestern North America (eastern Beringia). In this study, we present new paleomagnetic polarity data and establish a magneto-lithostratigraphy describing preglacial, glacial, and interglacial deposits in the Tintina Trench. These deposits are referred to as the West Tintina Trench Allogroup and provide a broad framework for establishing a paleoclimate record for the northern Canadian Cordillera.

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Riley, Teal R., and Philip T. Leat. "Chapter 2.2a Palmer Land and Graham Land volcanic groups (Antarctic Peninsula): volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 121–38. http://dx.doi.org/10.1144/m55-2018-36.

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AbstractThe break-up of Gondwana during the Early–Middle Jurassic was associated with flood basalt volcanism in southern Africa and Antarctica (Karoo–Ferrar provinces), and formed one of the most extensive episodes of continental magmatism of the Phanerozoic. Contemporaneous felsic magmatism along the proto-Pacific margin of Gondwana has been referred to as a silicic large igneous province, and is exposed extensively in Patagonian South America, the Antarctic Peninsula and elsewhere in West Antarctica. Jurassic-age silicic volcanism in Patagonia is defined as the Chon Aike province and forms one of the most voluminous silicic provinces globally. The Chon Aike province is predominantly pyroclastic in origin, and is characterized by crystal tuffs and ignimbrite units of rhyolite composition. Silicic volcanic rocks of the once contiguous Antarctic Peninsula form a southward extension of the Chon Aike province and are also dominated by silicic ignimbrite units, with a total thickness exceeding 1 km. The ignimbrites include high-grade rheomorphic ignimbrites, as well as unwelded, lithic-rich ignimbrites. Rhyolite lava flows, air-fall horizons, debris-flow deposits and epiclastic deposits are volumetrically minor, occurring as interbedded units within the ignimbrite succession.

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49

Castelli, Andrea, and Maria Júlia Paes da Silva. ""Faz isso, faz aquilo, mas eu tô caindo...": compreendendo a Doença de Chron." Revista da Escola de Enfermagem da USP 41, no. 1 (March 2007): 29–35. http://dx.doi.org/10.1590/s0080-62342007000100004.

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Buscando compreender o significado e o impacto da doença de Chron na vida de seu portador, desenvolvemos este estudo, de natureza qualitativa, optando pela História Oral de Vida como referencial metodológico, tendo como base filosófica a corrente monista, advinda de Hipócrates, em que a prática médica tem por objeto a pessoa doente em sua totalidade, levando em conta seu temperamento e a sua história. A terapêutica deve restabelecer a harmonia da pessoa com seu ambiente e consigo mesma , trata-se de uma medicina integradora e dinâmica, que corresponde aos primórdios da medicina psicossomática. O estudo da doença de Chron, por meio da compreensão psicossomática, permitiu que analisássemos os sintomas, não como corpos estranhos a serem erradicados, mas como mensageiros de um apelo a ser compreendido. Por intermédio deles, pode ser resgatada a história de um indivíduo que, se conscientemente vivida e analisada, permite o desenvolvimento até níveis mais evoluídos de entendimento.

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Yang, Wen, Yanyan Feng, and Wei Chu. "Comparative Study of Textural Characteristics on Methane Adsorption for Carbon Spheres Produced by CO2Activation." International Journal of Chemical Engineering 2014 (2014): 1–7. http://dx.doi.org/10.1155/2014/916913.

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Resorcinol-formaldehyde resin polymer was used as raw material for preparation of carbon spheres. Samples were treated with CO2flow at 850°C by varying activation times. The CO2activation granted better pore development of pore structure. The experimental data of CH4adsorption as a function of equilibrium pressure was fitted by Langmuir and Dubinin-Astakhov (D-A) models. It was concluded that the high surface area and micropore volume of carbon spheres did unequivocally determine methane capacities. In addition, a thermodynamic study of the heat of adsorption of CH4on the carbon spheres was carried out. Adsorption of CH4on carbon spheres showed a decrease in the adsorption heat with CH4occupancy, and the heat of adsorption fell from 20.51 to 12.50 kJ/mol at 298 K and then increased to a little higher values at a very high loading (>0.70), indicating that CH4/CH4interactions within the adsorption layer became significant.

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