ライフサイエンスコーパス: arc

1 which now runs at a spatial resolution of 10 arc-seconds (~300 m), contains new modules for downscali

2 and chromatin conformation-based data as 2D-arcs accompanied by interactive network analyses is valu

3 s of the lensed supernova, approximately 0.3 arc seconds from the center of the foreground galaxy.

4 used to develop a global erosivity map at 30 arc-seconds( 1 km) based on a Gaussian Process Regressio

5 At 5 x 5 arc-minute spatial resolution, we quantify WF(g) and the

6 Defective stereoacuity (>60 arc second) was noted in 20 subjects (67%) in childhood

7 Neuronal expression of human Abeta42(arc) in adult flies results in robust Abeta accumulation

8 eam of Draper in glia in response to Abeta42(arc) exposure.

9 The ablation arc followed an asymptotic function with a half-maximum

10 anochemical behavior of stress fibers, actin arcs, and cortical actin-based structures.

11 etween magma and crustal carbonate at active arc volcanoes has recently been proposed as a source of

12 olcanoes in subduction zones indicates along-arc variation in the physical condition of the underlyin

13 mantle flow pattern that amplifies the along-arc variations in the sub-arc mantle temperature, provid

14 tation that are found in the South American 'arc of deforestation', but which have been neglected in

15 ast, the Fe distribution is smeared along an arc corresponding to the proposed path from the ferroxid

16 factors, which are enriched in two areas: an arc region extending from the central protuberance to th

17 each side of the beta(2) dimer, creating an arc, which binds on its concave side to the mitochondria

18 Here we try to draw an arc from initiation of acute inflammatory reactions to m

19 manikin, and stimuli were presented from an arc of loudspeakers inside an anechoic chamber.

20 Nr2f2) transcription factor expression in an arc-shaped progenitor domain within the MGE promotes tim

21 MAR] 0.4) and stereoacuity 800 seconds of an arc or better.

22 elopment and ongoing neuroplasticity with an arc toward appreciating neuron-glial interactions and th

23 uorescence sensor using a light stop with an arc-shaped aperture for enhancing the flexibility of qui

24 edges, graded Fibronectin 'adhesive' and an arced adhesive spew filet.

25 ry and noble gas compositions of forearc and arc front springs in Costa Rica to show that the structu

26 elation between the extent of glaciation and arc-continent collisions in the tropics.

27 Stable and reliable arc operation and arc synthesis were achieved with the boron-rich anode an

28 ived volcanic complex in the Lesser Antilles arc, were integrated to track the preeruptive thermal an

29 rom Martinique Island in the Lesser Antilles arc, which displays one of the most extreme geochemical

30 Processes related to eruptions at arc volcanoes are linked by structures that transect the

31 ts of clinically relevant plaque attributes (arc angle and length), compared favorably to those from

32 esponsible for discrete longitudinal auroral arcs that move equatorward at a velocity of about 1km/s.

33 asin serves as a natural laboratory for back-arc basin studies in the Mediterranean region.

34 Urashima field on the southern Mariana back-arc, and at the Hafa Adai site in the central Mariana ba

35 e Hafa Adai site in the central Mariana back-arc.

36 erical model to quantify the effects of back-arc temperature perturbations on the mantle wedge flow p

37 e sub-arc mantle is brought in from the back-arc largely by slab-driven mantle wedge flow.

38 kely to cause lateral variations in the back-arc mantle temperature.

39 small temperature perturbations in the back-arc result in vigorous inflow of hotter mantle and subdu

40 Dynamic processes in the back-arc, such as small-scale mantle convection, are likely t

41 -continent collision between the Sunda-Banda arc system and Australia has increased the area of subae

42 sediment and peridotite, or assimilation by arc crust sediment, unlikely to be the main mechanism to

43 edicted hardnesses with alloys fabricated by arc-melting, identifying alloys having very high measure

44 y investigate the membrane shapes induced by arc-shaped scaffolds such as proteins and protein comple

45 ides Mo2 B, alpha-MoB, beta-MoB, and MoB2 by arc-melting.

46 12) and Zr(0.5)U(0.5)B(12), were prepared by arc melting from pure elements.

47 able concentration of boron were prepared by arc-melting and investigated for their mechanical proper

48 s on the determinants of membrane shaping by arc-shaped scaffolds.

49 eogeographic reconstruction of the Calabrian arc in time.

50 s the most active volcano within the Cascade arc; however, its location is unusual because it lies 50

51 fracture zones subducted beneath the central arc over approximately the past ten million years.

52 t supplier of subducted water to the central arc.

53 This chronological arc establishes that bison first entered North America d

54 ss with the lowest Nb/Ta seen in continental arc magmas.

55 nhouse climates, whereas reduced continental arc activity corresponds with icehouse climates of the C

56 atic differentiation, such as in continental arcs and other magmatic orogens, is thus necessary for m

57 magmatism and differentiation in continental arcs, like the Andes, reach greater Li contents than the

58 a(13)C and are located in mature continental arcs that have accreted carbonate platforms, indicating

59 major climate shifts: Widespread continental arcs correspond with prominent early Paleozoic and Mesoz

60 Copper arc zircons have juvenile epsilonHf (+7.6 to +11.5) and

61 in greater crustal contributions than copper arc rocks.

62 from deeply sourced springs along two cross-arc transects to show that about 91 per cent of carbon r

63 nance is visualized by the number of cycloid arcs.

64 BNNTs) were successfully synthesized by a dc arc discharge using a boron-rich anode as synthesis feed

65 Deep arc cumulates (arclogites) are found to have high Nb/Ta

66 anisms required to induce foundering in deep arc crust are assessed using an example of representativ

67 These relationships suggest that the deep arc crust must have primarily involved significant igneo

68 (i.e., the presence or absence of a directed arc connecting two nodes) in the presence of noise, spar

69 gative ionization, such as corona discharge, arcing, and electrospray destabilization, because of the

70 e mechanisms, solidification cracking during arc welding of steel are investigated in situ with high-

71 Here, we show that during arc magma differentiation, the extent of Nb/Ta fractiona

72 lated from the raw soot obtained by electric arc vaporization of graphite rods packed with Sc2O3 and

73 N isotope compositions of emitted arc gases (9-11 N degrees ) imply less subducted pelagic

74 dation of polysaccharides forms an essential arc in the carbon cycle, provides a percentage of our da

75 the cusp singularity of multiple exceptional arcs (EAs).

76 Dirac and Weyl semimetals both exhibit arc-like surface states.

77 with large topological charge and long Fermi arc (FA) surface states inspires the investigation of th

78 The length of the Fermi arc gives a measure of the topological strength, because

79 We show that the Fermi arc length can be changed as a function of Mo concentrat

80 ng condensate, and for cuts inside the Fermi arc region.

81 of Cooper pairs inside and outside the Fermi arc region.

82 PES) to directly observe a topological Fermi arc above the Fermi level, demonstrating a Weyl semimeta

83 ensures the formation of topological "Fermi arc" surface bands whose existence is guaranteed by bulk

84 However, the Weyl points and Fermi arcs live entirely above the Fermi level, making them in

85 g unique Weyl fermions in the bulk and Fermi arcs on the surface, TWSs offer a rare platform for real

86 energy range, experimentally detecting Fermi arcs in an energy window of more than 1.6 eV that is sym

87 opological invariant protecting double Fermi arcs in DSMs, using a K-theory analysis for space groups

88 rough the crystal's boundary by exotic Fermi arcs.

89 as do the surface states that feature Fermi arcs.

90 e topological conductors exhibit giant Fermi arcs of maximum length (pai), which are orders of magnit

91 ne-dimensional (1D) higher-order hinge Fermi arcs (HOFAs) as universal, direct consequences of their

92 lored to the special case of identical Fermi arcs on top and bottom surfaces.

93 s a characteristic feature, nontrivial Fermi arcs, connecting between topologically distinct Fermi su

94 The Weyl orbits consist of Fermi arcs (open arc-like surface states) on opposite surfaces

95 hey are connected by different sets of Fermi arcs for each of the two surface terminations.

96 no direct experimental observation of Fermi arcs in momentum space has been reported so far.

97 of these fermions are the presence of Fermi arcs in non-Weyl systems and the existence of Dirac line

98 illouin zone Weyl node connectivity of Fermi arcs, whereas on cobalt (Co) termination, the connectivi

99 Owing to the coupling between open Fermi arcs on opposite surfaces, topological Dirac semimetals

100 observed in doped cuprates-pseudogaps, Fermi arcs and marginal-Fermi-liquid-like electronic scatterin

101 Surface Fermi arcs (SFAs), the unique open Fermi-surfaces (FSs) discov

102 n of quantum oscillations from surface Fermi arcs and chiral modes in Weyl semimetals.

103 he Weyl points themselves, the surface Fermi arcs in Dirac semimetals are not directly related to the

104 However, whereas the surface Fermi arcs in Weyl semimetals are topological consequences of

105 (ARPES), we unravel the unique surface Fermi arcs, in good agreement with our ab initio calculations

106 are connected by exactly four surface Fermi arcs, thus proving that they carry the maximal Chern num

107 On the sulfur (S) surface, Fermi arcs overlap with nontopological bulk and surface states

108 pairs of Weyl points connected by the Fermi arcs.

109 rface, leading to the formation of the Fermi arcs.

110 ous lines of massless excitations- the Fermi arcs.

111 ie temperature, we observe topological Fermi arcs that correspond to projected topological charges of

112 natures of Weyl points and topological Fermi arcs.

113 momentum space) in the bulk and unique Fermi arcs generated by topological surface states, but also e

114 mimetal such as the chiral anomaly and Fermi-arc surface states.

115 ctions and possibly enhanced by robust fermi-arc type surface states.

116 hree different terminations modify the Fermi-arc contour and Weyl node connectivity.

117 iomers, we observe a reversal of their Fermi-arc velocities, which demonstrates that the handedness o

118 cyclotron motion that weaves together Fermi-arc and chiral bulk states.

119 discovered its characteristic surface Fermi-arcs and linear bulk band dispersions across the Weyl po

120 rmions and have characteristic surface Fermi-arcs in their electronic structure.

121 like this may be the primary reservoirs for arc volcanism, influencing compositional variations and

122 ion 352, which drilled a segment of the fore-arc of the Izu-Bonin-Mariana subduction system, revealin

123 , and of CO2 addition to the atmosphere from arc volcanism in the Neo-Tethys, between 100 and 40 Ma.

124 The carbon dioxide emitted from arc volcanoes is largely recycled from subducted microfo

125 inct calcite in calc-silicate xenoliths from arc volcanics in a case study from Merapi volcano (Indon

126 by comparing it with heat-treated fullerene arc-soot.

127 nstrate a direct relationship between global arc activity and major climate shifts: Widespread contin

128 um basaltic rocks; notably, these TTGs have 'arc-like' signatures of trace elements and thus resemble

129 aux Ridge collision against the New Hebrides arc, lead to progressive subsidence of Ambrym's caldera

130 The helicoid arcs that we observe on the surface characterize the top

131 ucturally chiral crystals featuring helicoid-arc quantum states.

132 0 m above sea level (masl)] of the Himalayan arc from Arunachal Pradesh to Ladahk were among the last

133 tic variation on both sides of the Himalayan arc, remains only partially elucidated.

134 of the earliest inhabitants of the Himalayan arc.

135 This commentary examines the historical arc of the 1918 influenza pandemic, focusing on black Am

136 has limited contribution to Li enrichment in arc magmas.

137 owever, the exact origin of Li enrichment in arc magmatic systems is not clear.

138 The method can be implemented in arc-scan, which may include volumetric-modulated arc the

139 produce the positive delta(34)S signature in arc settings.

140 Incorporation of subducted slab in arc volcanism plays an important role in producing the g

141 g the geochemical and isotopic variations in arc lavas.

142 These enrichment effects are favored in arcs with thick crust, which explains why magmatism and

143 e up of different actin structures including arcs, bundles and single filaments, which are often asso

144 the causes of ubiquitous and dramatic intra-arc variations in volcanic flux and composition remain l

145 ons can be produced in both plume and island arc settings.

146 ractionated in Ti than differentiated island arc rocks (mainly calc-alkaline).

147 arc parental melts, and thus igneous island arc rocks.

148 mantle, increasing the redox state of island arc parental melts, and thus igneous island arc rocks.

149 ut also influenced the redox state of island arc rocks, which are building blocks of continental crus

150 ence that the more oxidized nature of island arc vs. midocean-ridge basalts is related to the subduct

151 mpiled data that indicate Phanerozoic island arc igneous rocks are more oxidized (Fe(3+)/SigmaFe rati

152 Average V/Sc ratios of Phanerozoic island arc rocks are elevated (by +1.1) compared with Precambri

153 reach greater Li contents than their island arc counterparts.

154 whether plumes (mafic in average) or island arcs (intermediate in average) can all produce sediments

155 or young lavas from southwest Pacific island arcs, Eyjafjallajokull, Iceland, and Terceira, Azores.

156 orth of New Zealand on the southern Kermadec arc.

157 baudi, finding that dying mice trace a large arc in red blood cells (RBCs) by reticulocyte space as c

158 duration of a single pluton within a larger arc plutonic complex.

159 Low-latitude arc-continent collisions are hypothesized to drive cooli

160 rous cap thickness <65 mum overlying a lipid arc >90 degrees .

161 The ICC for the maximal lipid arc assessment before and after was 0.76 and 0.82 respec

162 Assessment of the maximal lipid arc was also undertaken similarly before and after the d

163 ersus 13.5, P<0.001), and greater mean lipid arc (191.8 degrees versus 84.2 degrees , P<0.001) compar

164 .2 versus 19.2, P<0.001), greater mean lipid arc (203.8 degrees versus 84.5 degrees , P<0.001), and m

165 f 21 IVOCT TCFAs (fibrous cap <65 mum, lipid arc >1 quadrant), only 8 were true histological TCFA.

166 .6% versus 0.3%; P=0.03) and a smaller lipid arc (163.1+/-71.4 degrees versus 211.2+/-71.2 degrees ;

167 Disregarding the lipid arc >1 quadrant requirement enhances the ability of IVOC

168 ficity (95% CI, 86%-96%) to detect all lipid arcs (both obtuse and acute, <1 quadrant) TCFA, and we a

169 OCT for TCFA detection (47% for obtuse lipid arcs).

170 doxin-like (TRXL) domains arranged in a long arc that terminates in two beta-sandwiches tightly clasp

171 spatial distribution of continental magmatic arc systems from the Cryogenian period to the present.

172 se obtained from subduction-related magmatic arcs, confirm that geochemistry can be used to track cha

173 rmorphic mutant of FtsA (FtsA*) forms mainly arcs instead of minirings and enhances lateral interacti

174 g bias for the loss of sequence in the major arc between, but not including, the heavy and light stra

175 majority of deletions removed only the major arc but approximately 10% of all deletions extended into

176 active submarine volcano NW Rota-1, Mariana arc and subaerial volcano Stromboli suggest that charact

177 eavy Mg isotopic signature of the Martinique arc lavas requires that the overall composition of the m

178 products were increased markedly by mercury arc UV photolysis, which covers the zinc atomic absorpti

179 is constrained to be smaller than 2.5 milli-arc seconds at the 90% confidence level.

180 ature-superposition analysis using a minimum-arc-length-based algorithm.

181 10% of all deletions extended into the minor arc removing the origin of light strand replication (OL)

182 sing a single-isocenter volumetric modulated arc therapy (VMAT) has been shown to decrease treatment

183 ge-guided radiotherapy, volumetric modulated arc therapy, helical tomotherapy, and adaptive radiother

184 cal tomotherapy (TOMO), volumetric-modulated arc therapy (VMAT), and fixed-field intensity-modulated

185 scan, which may include volumetric-modulated arc therapy (VMAT).

186 local spillover impacts, estimates for most arc states either are not significant or are not robust;

187 tion interrupts the anti-inflammatory neural arc, resulting in the expansion of MDSCs and colorectal

188 a HER in the recently identified Dirac nodal arc semimetal PtSn(4) .

189 n can account for both the prevalence of non-arc magmatism and the enhanced erosion.

190 als, and zircons result from significant non-arc magmatism during the mid-Proterozoic, while fewer oc

191 cause it lies 50 km west of the main axis of arc volcanism.

192 Clustering of arc volcanoes in subduction zones indicates along-arc va

193 pendent on reach distance, while decoding of arc-length is independent.

194 changes with the latitudinal distribution of arc-continent collisions.

195 n of the underlying mantle where majority of arc magmas are generated.

196 training to a value of 176.7 +/- 152.4 s of arc after training (p < 0.01).

197 lary) or near stereoacuity of 240 seconds of arc or worse (-8.6, P < 0.001 for total score; -5.3, P <

198 or reduced near stereoacuity (240 seconds of arc or worse) in 4- and 5-year-old children enrolled in

199 ively; and 4 circles correct (140 seconds of arc) indicated VA of at least 20/110 and 20/570, respect

200 ly with VA: 9 circles correct (40 seconds of arc) indicated VA of at least 20/40 with 95% confidence

201 confidence; 6 circles correct (80 seconds of arc) indicated VA of at least 20/62 and 20/180, respecti

202 ed by subduction and strike-slip stacking of arc material mostly by precollisional coastwise transpor

203 first set of Mg isotopic data for a suite of arc lava samples from Martinique Island in the Lesser An

204 tly by precollisional coastwise transport of arc fragments rifted from the Congo/Tanzania cratonic nu

205 ducted N to the mantle and past the zones of arc magma generation.

206 Ongoing arc-continent collision between the Sunda-Banda arc syst

207 The Weyl orbits consist of Fermi arcs (open arc-like surface states) on opposite surfaces of the sam

208 ents due to strong electromagnetic fields or arcing.

209 s, the divisome appears as multiple rings or arcs that drive lateral PGN incorporation, leading to ce

210 sions are consistent with results from other arc volcanic reservoirs and suggest that arc magmas are

211 geographic position of all major Phanerozoic arc-continent collisions was reconstructed and compared

212 e oxidized source for the genesis of primary arc magmas that release gases to the atmosphere during v

213 Here, we show that, globally, primitive arc magmas have Li contents and Li/Y ratios similar to m

214 ibuting to the previously established reflex arc resulting in efferent vagal activity and asthmatic b

215 is important to the anti-inflammatory reflex arc and plays an essential role in arresting MDSC prolif

216 nt, unstimulated skin through a nerve reflex arc.

217 The neuromuscular reflex arc is the system that integrates the proprioceptive inf

218 lopment of a functional neuromuscular reflex arc.

219 model and its incorporation into the reflex arc allows for a more accurate recapitulation of neuromu

220 neurons form the final element of the reflex arc that integrates visuovestibular inputs into temporal

221 vestibulo-ocular and vestibulo-collic reflex arcs.

222 ated with bladder filling and voiding reflex arcs.

223 ge depth variations, this buoyant refractory arc mantle is likely compensated at depth by denser, lik

224 Our results suggest that highly refractory arc mantle relicts are entrained in the upper mantle and

225 this study with that from subduction-related arcs can provide the crustal thickness evolution of an o

226 Stable and reliable arc operation and arc synthesis were achieved with the b

227 xhibit a normal transition into F-actin-rich arcs, and drug inhibition is consistent with aura functi

228 s measured ray path geometries in the Ryukyu arc can constrain the distribution, orientation and amou

229 Outside the region's "arc of deforestation," we confirm little internal impact

230 Here, we show that AA7075 can be safely arc welded without hot cracks by introducing nanoparticl

231 y ice-free areas of the Beaufort-to-Kara Sea arc.

232 an hyperopic children (40 sec arc vs 120 sec arc, P < .001).

233 opic than in than hyperopic children (40 sec arc vs 120 sec arc, P < .001).

234 However, some arc volcanic centers have been active for tens of thousa

235 The high delta(98/95)Mo(NIST 3134) of some arc lavas is the complement to this process.

236 seismicity, the links between closely spaced arc volcanoes, and the potential for cascading hazards.

237 yl point manifests in terms of surface state arcs in the synthetic space that exhibit one-way frequen

238 vation of photonic topological surface-state arcs connecting topologically distinct bulk states in a

239 s directly observe topological surface-state arcs in momentum space by near-field scanning the surfac

240 ons on the mantle wedge flow pattern and sub-arc mantle temperature.

241 richment is enhanced by lower degrees of sub-arc mantle melting and higher extents of intracrustal di

242 rovide negligible sulfate to oxidize the sub-arc mantle and cannot deliver (34)S-enriched sulfur to p

243 dification of the oxidation state of the sub-arc mantle by hydrous, oxidizing sulfate and/or carbonat

244 The sub-arc mantle is brought in from the back-arc largely by sl

245 mplifies the along-arc variations in the sub-arc mantle temperature, providing a simple mechanism for

246 idered to result in the oxidation of the sub-arc mantle.

247 re zones may increase water transport to sub-arc depths.

248 Investigating such arc-scale issues requires greater quantitative compariso

249 er unveil the exotic double-helicoid surface arcs that emanate from a projected quadratic Weyl point

250 formed on an island within the Trans-Tethyan arc(10).

251 We find that arc-shaped scaffolds induce membrane tubules at membrane

252 her arc volcanic reservoirs and suggest that arc magmas are generally stored warm.

253 nella species sampled exhibit tracheids that arc backward from the stem and side branch into the rhiz

254 The arc lavas have significant (238)U and (226)Ra excesses,

255 suggest distinct roles for pUL103 across the arc of lytic infection, including interactions with prot

256 medicinal chemists, has been hailed as "the arc of a medical triumph" but may equally well be descri

257 h" but may equally well be described as "the arc of a medicinal chemistry triumph".

258 he Earth's mantle is either stored below the arc crust, is efficiently consumed by microbial activity

259 subdued inflow of colder mantle beneath the arc due to the temperature dependence of the mantle visc

260 tion for flash sintering, is provided by the arc electrodes which heat the sample to 1400 degrees C.

261 al suggesting that under such conditions the arc operates in so-called anodic mode with the anode mat

262 gical implications of these findings for the arc formation in lamellipodium-to-lamellum architectural

263 ence of root-growth of BNNTs produced in the arc discharge.

264 oncentrations of synthesis conditions in the arc periphery.

265 e directly connected to the evolution of the arc and its associated seismic and volcanic hazards.

266 The sensory portion of the arc is composed of proprioceptive sensory neurons and th

267 ntify and study the helicoid topology of the arc states.

268 reshold, in contrast, strongly depend on the arc angle.

269 lation of current magnitudes covary over the arc of development, while rapidly responding to changes

270 atment, while still being sustained over the arc of time.

271 To sustain the arc current by thermionic electron emission, the cathode

272 the same boron-rich alloy, we found that the arc operation unstable due to frequent sticking between

273 agnesium basaltic rocks, suggesting that the arc-like signature in Archaean TTGs was inherited from a

274 ial being consumed by evaporation due to the arc heating.

275 groups of Na3Bi and Cd3As2 Generically, the arcs deform into a Fermi pocket, similar to the surface

276 In the "arc," we test impacts by state, as states are large and

277 n a threshold of ~40%, irrespective of their arc angle.

278 of higher volcanic productivity and thicker arc crust.

279 ide a historical perspective, following this arc of inquiry from neuronal to neuron-glial mechanisms

280 nitrogen (N) back to the atmosphere through arc volcanism has been advocated for the Central America

281 ample of contractile bundles is a transverse arc that forms via actomyosin-driven condensation of act

282 l unblocked area for each specific treatment arc, and (e) generates a treatment plan with the optimiz

283 may be the main source of fluids triggering arc magma generation.

284 iently high temperature, which for a typical arc current density of 100 A/cm(2), is above the boron m

285 to monitor the growth of nanoparticles under arc discharge conditions.

286 oding performance for discrete BMIs by using arc-length between reach end-points rather than the angl

287 nary project in the Lesser Antilles volcanic arc(3), we studied boron trace element and isotopic fing

288 ver includes most of the Guanacaste volcanic arc, herein the Guanacaste Volcanic Arc Sliver.

289 entration, and delta(34)S values in volcanic arc rocks have been attributed to significant sulfate ad

290 lift during collision of the Panama volcanic arc with South America.

291 trained compared to fluxes from the volcanic arc front.

292 lab's mantle dehydrates beneath the volcanic arc, and may be the main source of fluids triggering arc

293 rogens, particularly in continental volcanic arcs.

294 for carbon and helium isotopes from volcanic arcs and demonstrated that the carbon isotope compositio

295 scale frontier geologic problems in volcanic arcs.

296 Decades of study on volcanic arcs have provided insight into the overarching processe

297 uggest enhanced erosion of Rodinian volcanic arcs and orogens.

298 dance, or as a bilevel partition graph, with arc size indicating abundance.

299 tubulation threshold, whereas scaffolds with arc angles larger than about 120 degrees induce double-m

300 Scaffolds with arc angles of about 60 degrees , akin to N-BAR domains,

301 topologically protected surface states, with arced Fermi surface contours that are predicted to propa