ライフサイエンスコーパス: arc

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

2 MC2 was run over the conterminous USA at 30 arc sec (~800 m) to simulate the impacts of nine climate

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

4 High-resolution (0.33-arc second) observations with NASA's Interface Region Im

5 At a spatial resolution of 5 by 5 arc minute, we estimate anthropogenic nitrogen (N) loads

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

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

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

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

10 top of the cell, which is composed of actin arcs and myosin IIA filaments.

11 onstrate that CK666 treatment produces actin arcs in other cells with broad LP regions, namely fish k

12 We hypothesize that the actin arcs made visible by Arp2/3 complex inhibition in coelom

13 enotype in coelomocytes was transverse actin arcs, and arc generation was arrested by a formin inhibi

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

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

16 ariable size, ellipses, and spirals and also arcs that could be assembly products.

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

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

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 ne is severely nonlinear; it is bent into an arc with an angle of 155.6(1) degrees between the termin

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

23 coelomocytes was transverse actin arcs, and arc generation was arrested by a formin inhibitor.

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

25 phase are associated with the arc length and arc area of the cycloid on a Bloch sphere, respectively.

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

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

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

29 nic gases show sulphur flux of 720 Gmol/y at arc volcanoes (ARC) with a contribution from the mantle

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

31 ormation and the tectonic escape of the back arc region, is imaged here for the first time.

32 f melt generation and transport beneath back-arc spreading centres are controlled by two endmember me

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

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

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

36 he mechanism for tectonic escape of the back-arc region.

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

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

39 re extend deeper and westwards into the back-arc, suggesting that these spreading centres are fed by

40 ges and flux melting resembling that beneath arcs.

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

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

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

44 % on a metals basis) were synthesized by arc-melting in order to study their mechanical propertie

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

46 itanium oxide films grown by pulsed cathodic arc had been investigated by XRD, SEM and Raman spectros

47 A room temperature cathodic arc deposition technique is used to produce high-mobilit

48 phoresis, gel bands display a characteristic arc pattern; this turns into a straight line when the de

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

50 (3) +/- 542 and 1857 cm(3) +/- 571 at closed arc and open arc cone-beam CT, respectively.

51 tead of -120 degrees to +120 degrees (closed arc cone-beam CT).

52 slightly lower compared with that of closed arc cone-beam CT (-5.1%).

53 e partially or completely outside the closed arc cone-beam CT field of view.

54 een February 2013 and March 2014 with closed arc and open arc cone-beam CT (during the first and seco

55 as significantly higher compared with closed arc cone-beam CT (97% vs 86% of the MR imaging liver vol

56 Continental arc magmatism in southern Tibet during 80-40 Ma migrated

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

58 beneath Yellowstone compared to continental arc volcanoes.

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

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

61 ading edge assembled into dorsal contractile arcs, a substantial subset assembled in or was captured

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

63 in greater crustal contributions than copper arc rocks.

64 nance is visualized by the number of cycloid arcs.

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

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

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

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

74 The evolutionary arcs of these ecologically important clades are framed a

75 ion, lubricating plate tectonics and feeding arc volcanism.

76 tal realization of Weyl semimetals and Fermi arc surface states in real materials.

77 The observed Fermi arc surface states open research frontiers in fundamenta

78 tally observe a pair of spin-polarized Fermi arc surface states on the surface of the Dirac semimetal

79 erimental signatures of their possible Fermi arc states.

80 pological classification that protects Fermi arc surface states on the boundary of a bulk sample.

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

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

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

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

85 momentum-dependent propagation of the Fermi arc surface states into the bulk.

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

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

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

89 gments of zero-energy states, known as Fermi arcs, and a gap as large as 80 millielectron volts.

90 topological surface states, so-called Fermi arcs, which have no counterparts in high-energy physics

91 ir band structures with characteristic Fermi arcs of TWSs.

92 yl nodes in the bulk and corresponding Fermi arcs in the surface Brillouin zone.

93 Weyl semimetals with distinctly curved Fermi arcs on the two surfaces.

94 s show up in the form of disconnected "Fermi arcs", reminiscent of those reported recently in surface

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

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

97 as do the surface states that feature Fermi arcs.

98 quasiparticle excitations and features Fermi arcs on its surface.

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

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

101 sion spectroscopy, we directly observe Fermi arcs on the surface, as well as the Weyl fermion cones a

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

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

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

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

106 Here, we find that the open Fermi arcs participate in unusual closed magnetic orbits by tr

107 l semimetals consist of disjoint, open Fermi arcs raising the question of whether they can be observe

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

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

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

111 of Weyl nodes and topological surface Fermi arcs.

112 ts bulk Weyl fermion cones and surface Fermi arcs.

113 We find that Fermi arcs terminate on the Weyl fermion nodes, consistent wit

114 the spectrum consists of holes on the Fermi arcs and an electronic pocket.

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

116 ous lines of massless excitations- the Fermi arcs.

117 natures of Weyl points and topological Fermi arcs.

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

119 r radiation incident on a surface with Fermi arcs, there is no Kerr or Faraday rotation but the elect

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

121 ators of contractility (i.e., stress fibers, arcs, and focal adhesions) and are primed to differentia

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

123 red filaments, whereas Shs1-capped rods form arcs, spirals, and rings.

124 ence of chiral magnon surface states forming arcs at finite energy.

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

126 e overlying plate is larger than output from arc volcanoes plus diffuse venting, and substantial quan

127 opology undergoes an abrupt transition, from arcs to closed contours, at the same p(c).

128 ate (ca. 20,000 mumol h(-1) g(-1) under full arc), which leads to a high turnover number (TON) of ove

129 the promoter of the activity-dependent gene arc to express the photosensitive ion channel, channelrh

130 a and the Alboran slab beneath the Gibraltar arc region; the anomalies are under, and are aligned wit

131 y under both South America and the Gibraltar arc, and to delamination of the entire lithospheric mant

132 lithospheric mantle, as around the Gibraltar arc.

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

134 ividual's response to a stimulus on a graded arc that moved from the periphery to the center of the v

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

136 0 m above sea level (masl)] of the Himalayan arc from Arunachal Pradesh to Ladahk were among the last

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

138 of the earliest inhabitants of the Himalayan arc.

139 Myosin II is concentrated in arc-like regions of the leading edge in between FLPs, an

140 se in the traction forces and an increase in arc radius, indicating that both line tension and surfac

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

142 g the geochemical and isotopic variations in arc lavas.

143 rged in the form of colliding oceanic island arcs, continental fragments and the Papuan Peninsula, as

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

145 ning, for initial Hikurangi Plateau-Kermadec arc collision ~250 km north of its present position.

146 urangi Plateau beneath the southern Kermadec arc, offshore New Zealand.

147 Here we show that Kermadec arc lavas south of ~32 degrees S have elevated Pb and Sr

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

149 n 11-unit FliG:FliM complex produces a large arc with a curvature consistent with the dimensions of t

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

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

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

153 Maximum lipid arc on OCT was an excellent discriminator of fibroathero

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

155 .6% versus 0.3%; P=0.03) and a smaller lipid arc (163.1+/-71.4 degrees versus 211.2+/-71.2 degrees ;

156 ith acute coronary syndrome, a smaller lipid arc (171.6+/-53.2 degrees versus 235.8+/-86.4 degrees ;

157 If the lipid arc >1 quadrant (obtuse) criterion was disregarded, 45 I

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

159 ugh OCT accuracy may be improved using lipid arc >/=80 degrees and fibrous cap thickness </=85 mum ov

160 confidence interval, 0.81-0.92), with lipid arc >/=80 degrees the optimal cut-off value.

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

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

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

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

165 Andes, as well as various Mesozoic magmatic arc segments currently exposed in the Coast Mountains, B

166 ocks from modern subduction-related magmatic arcs formed around the Pacific.

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

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

169 Most mtDNA deletions are major arc deletions with breakpoints located between the origi

170 ear mtDNA fragment spanning the entire major arc of the mitochondrial genome is generated.

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

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

173 ously amplifies the MT-ND4 gene in the major arc, the MT-ND1 gene in the minor arc, and the non-codin

174 avy strand (OH) replication within the major arc.

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

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

177 rianal edema than did control patients (mean arc angle of anal canal involved, 220 degrees vs 60 degr

178 Aleutian, Andean, Cascades and Trans-Mexican arcs.

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

180 fication of a broad range of major and minor arc mtDNA deletions with the potential to investigate th

181 der certain disease conditions, rarer, minor arc deletions are detected.

182 10% of all deletions extended into the minor arc removing the origin of light strand replication (OL)

183 the major arc, the MT-ND1 gene in the minor arc, and the non-coding D-Loop region.

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

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

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

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

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

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

190 rc plasma torch and with a DC nontransferred arc plasma torch.

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

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

195 IXT and near stereoacuity of 400 seconds of arc or better were enrolled.

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

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

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

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

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

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

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

203 nd wing morphology predicted only the use of arcing turns and high centripetal accelerations.

204 against membrane tension advances the web of arcs between FLPs.

205 Open arc cone-beam CT allowed for a significantly improved in

206 2013 and March 2014 with closed arc and open arc cone-beam CT (during the first and second transarter

207 nd 1857 cm(3) +/- 571 at closed arc and open arc cone-beam CT, respectively.

208 tates from +55 degrees to -185 degrees (open arc cone-beam CT) instead of -120 degrees to +120 degree

209 The coverage of open arc cone-beam CT was significantly higher compared with

210 All tumors were within the open arc cone-beam CT field of view.

211 The open arc cone-beam CT radiation exposure by means of weighted

212 ents due to strong electromagnetic fields or arcing.

213 evealed the presence of incomplete rings, or arcs.

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

215 of an intervening seaway, between the Panama arc and South America in middle Miocene times; the Centr

216 taneously monitor the dynamics of peripheral arc radii and traction forces.

217 imple physical model in which the peripheral arc line tension is due to the combination of myosin II

218 rce contributes to tension in the peripheral arcs.

219 anced TW myosin light chain phosphorylation, arc formation, and brush border fanning coincided with i

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

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

222 An anti-inflammatory reflex arc involving the vagus nerve and memory T cells is nece

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

224 lopment of a functional neuromuscular reflex arc.

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

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

227 vestibulo-ocular and vestibulo-collic reflex arcs.

228 thought of as cortical sensory-motor reflex arcs.

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

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

231 o the interface was well below 1 W and no rf arcing was observed for two different rf generator desig

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

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

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

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

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

237 50807) that we directly localize to 9 square arc minutes.

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

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

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

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

242 plete with twist or torsional motions on sub-arc second scales, occurring in active regions, quiet Su

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 work to accurately predict the shape of such arcs as a function of molecule length and topological co

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

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

251 Here we show that arcs, which serve as precursors for ventral stress fiber

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

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

254 ng the papillomacular bundle, defined as the arc from -15 degrees to +15 degrees on the axis from the

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

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

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

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

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

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

261 from the balance of the line tension in the arc and of the surface tension in the cell bulk.

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

263 oncentrations of synthesis conditions in the arc periphery.

264 uggests that pulsed microdischarge is in the arc regime while DC microdischarge belongs to glow.

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

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

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

268 Here we show that the arc-discharge synthesis of mixed titanium-lutetium metal

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

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

271 tions of elasticity and contractility to the arc line tension.

272 the geometric phase are associated with the arc length and arc area of the cycloid on a Bloch sphere

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

274 The radius of curvature of these arcs results from the balance of the line tension in the

275 causes curved cells to orient such that they arc over the surface, thereby decreasing the distance be

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

277 tent with higher than normal fluid inputs to arc magma sources.

278 actors were assembled: with a DC transferred arc plasma torch and with a DC nontransferred arc plasma

279 gnatures reveal the presence of a transpolar arc.

280 ellent correspondence between the transpolar arc and the trapped closed flux at high altitudes provid

281 rapping mechanism as the cause of transpolar arcs.

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

283 underlies the organization of the transverse arc and radial (dorsal) stress fibers at the leading lam

284 sion than dorsal stress fibers or transverse arcs.

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

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

287 ells with IFN-gamma caused MLCK-dependent TW arc formation and brush border fanning, which preceded c

288 ith the sample to be sintered is made by two arc plasma electrodes, one on either side, allowing curr

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

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

291 logies of manufacturing carbon nanotubes via arc discharge, laser ablation and chemical vapor deposit

292 Variations in continental volcanic arc emissions have the potential to control atmospheric

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

294 e use enrichment of boron (B/Zr) in volcanic arc lavas as a proxy to evaluate relative along-strike i

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

296 enhances fluid introduction beneath volcanic arcs.

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

298 uggest enhanced erosion of Rodinian volcanic arcs and orogens.

299 For some volcanic arcs, the geochemistry of volcanic rocks erupting above

300 uggestive for the future realization of Weyl arcs, condensed matter supersymmetry and other fascinati

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