コーパス検索結果 (１語後でソート)
通し番号をクリックするとPubMedの該当ページを表示します
1 block structures (bends, folds, d-cones, and ridges).
2 ed and how it reaches the Greenland-Scotland Ridge.
3 ajor overflows across the Greenland-Scotland Ridge.
4 hydrothermal vent fauna at the Mid-Atlantic Ridge.
5 ed whenever the avatar's fingertip crossed a ridge.
6 l structure similar to the apical ectodermal ridge.
7 s migrate through circulation to the genital ridge.
8 ble sample collection site on the equatorial ridge.
9 ridge and the suppression of the lower leaf ridge.
10 ronary sinus and septally at the left atrial ridge.
11 ydrothermal vents along the Southwest Indian Ridge.
12 io wavelengths that illuminates the magnetic ridge.
13 creasing deposition cause the formation of a ridge.
14 ers or in dimensional change of the alveolar ridge.
15 ed melt inclusions from the Gakkel mid-ocean ridge.
16 localized above the Munger-Saharsa basement ridge.
17 shape, with a prominent circular equatorial ridge.
18 nique residues align along the outer helical ridge.
19 is Massif oceanic core complex, Mid-Atlantic Ridge.
20 les beneath the water table under valley and ridge.
21 ridge systems towards the Greenland-Scotland Ridge.
22 ev-1 hydrothermal fields on the Mid-Atlantic Ridge.
23 bsurface sediments from the Arctic Mid-Ocean Ridge.
24 ological feature is the continuous, elevated ridge.
25 rea (49.7 degrees E) on the Southwest Indian Ridge.
26 along the western flank of the Mid-Atlantic Ridge.
27 g of the developing agents to the fingermark ridges.
28 ion of these inbricated boulder clusters and ridges.
29 eric mantle, at least at ultraslow-spreading ridges.
30 rature hydrothermal circulation at mid-ocean ridges.
31 sponding to "greasy hollows" between protein ridges.
32 ridge defects were created to form atrophic ridges.
33 generally available for ultra-slow spreading ridges.
34 depth increased in the vicinity of seafloor ridges.
35 of the lung through the formation of septal ridges.
36 e located largely in hollows between protein ridges.
38 anthus, telecanthus, a wide nasal bridge and ridge, a broad and smooth philtrum, and a thin upper lip
40 ologically by strong interdigitation of rete ridges, abundant organized fibrillar collagen, and plent
41 (Fgf8) is produced by the apical ectodermal ridge (AER) at the distal tip of the limb bud to direct
43 gical swirling flow, while the height of the ridge also significantly contributed to the enhanced per
44 stepwise procedure identifying the coumadin ridge and 2 vascular landmarks in ECG-gated computed tom
45 (5%) had lesions above the superior orbital ridge and below the proximal third of the femur, respect
48 ly three lobed axis with an elevated central ridge and regularly spaced transverse furrows that conve
50 feature of the western and central Lomonosov Ridge and that perennial sea ice remained present throug
51 get epitopes within the E domain III lateral ridge and the domain I-II hinge region, respectively(3).
53 borehole observations in a well-constrained ridge and valley landscape and then interpreted spatial
54 show that a sequence of increasingly complex ridge and valley networks is produced by a system of par
56 ures on the shell exterior, such as external ridges and changes in growth direction, and also that th
58 identified, with complete flattening of rete ridges and marked depletion of elastic fibers and fibril
59 ning (MTM) is a form of surface mining where ridges and mountain tops are removed with explosives to
61 ll populations at the top and bottom of rete ridges and transitional positions between the basal and
62 nid, strongly developed P(3) mesial marginal ridge, and a P(3) > P(4) size relationship) that disting
64 lyamide thin-film composite membranes with a ridge-and-valley structure and an emerging type of smoot
66 g task, participants indicated which surface ridges appeared to be caused by the hidden object and wh
67 ing processes associated with slow-spreading ridges are a complex interplay of volcanic accretion and
68 agments as large as 20 cm suggest that these ridges are antidunes: a type of sedimentary structure th
69 eir causes, to distinguish whether lumps and ridges are due to the shrouded object or to the ripples
70 s rapidly increased, whereas nonaxisymmetric ridges are favored when the curvature is slowly increase
71 s the appearance of the respiratory eggshell ridges, are caused by changes in the spatial distributio
72 ontradistinction, the southeastern Lomonosov Ridge area experienced seasonally sea-ice-free condition
74 Likewise, buccal-lingual width of alveolar ridge as well as thickness of buccal wall was compared w
75 l disorder among the identical, multilayered ridges as the critical factor for producing angular inde
78 inferred to have caused breaching of a rock ridge at the Dover Strait, although this hypothesis rema
79 e considered that lead to the formation of a ridge at the slime-substrate-air interface, thereby crea
80 retrospective chart review of 73 horizontal ridge augmentation cases was completed to assess the cli
81 successfully expanded before bone graft for ridge augmentation even at sites with a history of prior
82 an effect on clinical outcomes of horizontal ridge augmentation including implant placement and chara
86 line hydrothermal vents off the Mid-Atlantic Ridge axis nearly 20 y ago, the observation that serpent
87 om Mauna Kea are more oxidized than midocean ridge basalt (MORB) magmas, suggesting that the upper ma
88 topes in Yellowstone compared with mid-ocean ridge basalt (MORB) samples, this confirms that the deep
89 isplacement process of the Pacific mid-ocean ridge basalt (MORB)-type mantle by the Indian MORB-type
95 an order of magnitude relative to mid-ocean ridge basalts and contain two Cl-bearing components with
96 e oxidized nature of island arc vs. midocean-ridge basalts is related to the subduction of material o
97 r (3)He/(4)He ratios identified in mid-ocean-ridge basalts that form by melting the upper mantle (abo
99 the convective mantle provided by mid-ocean-ridge basalts(11), consistent with subducted nitrogen be
100 ontents and Li/Y ratios similar to mid-ocean ridge basalts, indicating that the subducting slab has l
101 ios between deep mantle plumes and mid-ocean-ridge basalts, which is best explained by addition of a
102 tructure as the possible source of Mid-Ocean Ridge Basalts- and Ocean Island Basalts- type magmatic r
103 introducing a deep-subwavelength dielectric ridge between a dielectric slab and a metallic substrate
104 ormer shorelines preserved in beach-foredune ridges (BFR) within a protected embayment to reconstruct
105 romoted socket bone fill, preserved alveolar ridge bone, and reduced postoperative pain in vivo with
106 fingerprints showing statistically distinct ridge breadth measurements for juveniles, males, and fem
107 sed increased growth at the positions of the ridges, but emerges from an elastic instability during h
112 non-sensory cells of the greater epithelial ridge cause, via ATP-induced activation of P2X(3) recept
113 trial was to compare three-dimensional (3D) ridge changes after immediate implant placement with and
117 red by stress induced by the D'Entrecasteaux Ridge collision against the New Hebrides arc, lead to pr
118 where the low marsh replaces the high marsh ridge community and the high marsh ridge community repla
119 igh marsh ridge community and the high marsh ridge community replaces the mid-marsh grasses on the ma
121 action socket may partly reduce the alveolar ridge contraction and that several factors like the thic
122 n decreased Lama5 protein in the LN cortical ridge (CR) and around high endothelial venules (HEVs).
123 Hibiscus richardsonii flowers, which have a ridged cuticle in the proximal region and a smooth cutic
124 sferase6 (gpat6), and defective in cuticular ridges (dcr) were grouped in three separate classes base
130 sufficient and economic way to preserve the ridge dimension without interfering with the amount of n
132 dPTFE membranes and FDBA result in favorable ridge dimensions for dental implant placement in most ca
133 d healing, sites were surgically re-entered, ridge dimensions were again measured using the previousl
136 nimally traumatic tooth extraction, alveolar ridge dimensions were measured using a custom-fabricated
138 robe sonifier was placed on the supraorbital ridge directly above the entrance of the optic nerve int
140 ctors moieties apparently contact the 'basic ridge' domain of DnaG, but not the DNA template base at
142 own that the avian visual dorsal ventricular ridge (DVR) is organized as a trilayered complex, in whi
144 The strong tidal triggering of mid-ocean ridge earthquakes has remained unexplained because the e
145 features present include a circum-equatorial ridge, east-west dichotomy, high boulder abundances acro
148 oincident orientations revealed by steerable ridge filtering in an adaptive manner that balances orie
150 ic assessment of the changes in the alveolar ridge for the E group showed a slight decrease (68.3 +/-
155 ion of marine water beyond the crest of this ridge, forming an ocean cavity beneath the ice shelf, oc
156 domain modeling that expanded trabeculae and ridges, found across ultra-black butterflies, reduce ref
158 ths after an experimental fire at the Jasper Ridge Global Change Experiment site in California, USA.
159 ames consisting of interconnected, ultrathin ridges have received considerable attention in the field
164 between the groups for mean change in buccal ridge height, lingual ridge height, and ridge width.
166 ered western flank of the Northern Knipovich Ridge, host extensive gas hydrate and related fluid flow
167 rison with the SARS-CoV RBD, an ACE2-binding ridge in SARS-CoV-2 RBD has a more compact conformation;
168 active submarine volcano on the Juan de Fuca Ridge in the NE Pacific Ocean, from 2013 to 2015 at thre
171 ithm can successfully repair and reconstruct ridges in single or multiple damaged regions of incomple
172 striped patterning of the rugae (transverse ridges) in the mammalian oral palate, focusing on multip
173 trabeculae, compared to lower values on the ridges, in the wild type suggest oscillatory forces as a
175 w clearly that the bending in the stretching ridge is responsible for the strength of both elastic an
176 andslide and show that the wavelength of the ridges is 2-3 times the average thickness of the landsli
177 averaged interfacial structure consists of a ridged lateral arrangement of adsorbed water molecules h
179 scular retina, visible vitreous condensation ridge-like interface with residual traction, and prematu
181 h both the thickness of the Gakkel mid-ocean ridge lithosphere and with pressures reconstructed from
184 The landforms are delicate sets of up to 90 ridges, <1.5 meters high and spaced 20 to 25 meters apar
188 de mineral precipitation occurs at mid-ocean ridge (MOR) spreading centers, both in the form of plume
189 anic lithosphere (<10 Ma) near the Mid-Ocean Ridge (MOR), we construct a box model of this environmen
191 ecapitulate the transition from two to three ridges observed during embryonic development of the drag
194 lian Hb cooperativity values all reside on a ridge of maximum cooperativity along this landscape that
196 f reef fishes that are endemic to a volcanic ridge of seamounts and islands to understand their relat
197 , we analyse the morphometry of longitudinal ridges of a martian landslide and show that the waveleng
198 n layer-which appear as temporal patterns of ridges of hot upwelling and cold downwelling fluid, incl
203 d cell surface topography (which forms micro-ridges on the neutrophil surface) provides the resource
204 hrough cartilages, cartilaginous cristae and ridges on the plantar side of the distal tibiotarsus and
205 teral, both buccal-lingually in the alveolar ridge (P = 0.007) and in buccal wall thickness (P = 0.00
209 Rapid plume motion was likely produced by ridge-plume interaction and deeper influence of the Paci
215 needing a single rooted tooth extraction and ridge preservation in preparation for dental implant pla
216 ed clinical trial, in which 53 patients with ridge preservation indications were selected and randoml
217 t material, and connective tissue/other when ridge preservation is accomplished using a bovine versus
218 vorable effects of PRF membranes in alveolar ridge preservation may be attributed, at least in part,
220 effect of different surgical techniques for ridge preservation on soft tissue parameters has seldom
221 the histologic difference in healing between ridge preservation sites treated with a combination allo
222 y was to compare the effect of two different ridge preservation techniques on soft and hard tissue di
224 Patients were then randomized 1:1 to receive ridge preservation using either bovine or porcine xenogr
226 Forty-four patients requiring extraction and ridge preservation were randomized into two groups: FDBA
230 to three groups: extraction alone (control); ridge preserved using FDBA; and either dPTFE (Test1) or
231 he amber match the hadrosaur's alveolar bone ridges, providing some insight into the taphonomic proce
232 zation procedure was more pronounced for the ridged/proximal cuticle, which is thicker and richer in
233 present study demonstrates that the lateral ridge region of the envelope protein is likely an immuno
238 ar unbiased predictor (RR-BLUP), generalized ridge regression (GRR), and Bayes-B GS methods were used
239 ote that the test statistics of the ordinary ridge regression (ORR) have the same patterns across the
240 ti-layer perception neural network (MMLPNN), Ridge regression (RR), Boosting generalized linear model
242 ts, support vector machines (regression) and ridge regression applied to 25 diverse high-quality stru
243 Genomic selection was implemented through a ridge regression best linear unbiased prediction model i
245 ler, traditional statistical methods such as ridge regression can outperform state-of-the-art machine
248 al algorithms (e.g. support vector machines, ridge regression), holds much promise for the improvemen
249 several feature-selection methods, including ridge regression, lasso regression, support vector machi
250 entations of atomic neighborhoods and Kernel Ridge Regression, we show that an accurate and transfera
254 ity, intensity, and depth of the subtropical ridge resulted in the establishment of a low-sheared env
256 during 26 Ma at a 11 degrees N Mid-Atlantic Ridge segment, and exposed along the Vema Transform.
258 opulations occupying the plains and mountain ridges separating Europe from Asia has been eventful, as
260 ane pits are unstable and 2) nonaxisymmetric ridge-shaped structures are energetically favorable.
262 nflorescence meristem formed a normal double-ridge structure, but then the lateral meristems generate
263 s from ultraslow- to fast-spreading midocean ridges, subduction zones, and ophiolites revealed that h
265 the water progresses southward along several ridge systems towards the Greenland-Scotland Ridge.
266 ctive population of two soil depths from Oak Ridge (Tennessee, USA) and find that a maximum of 25-70%
269 brine lake on the floor of the Mediterranean Ridge that underlies a 3500-m water column, and name it
270 The device uses a channel with repeated ridges that are diagonal with respect to the direction o
271 roplets during the destabilization of liquid ridges that form during the late stages of the dewetting
272 re a series of symmetrical, 10 m-high gravel ridges that occur in the Hummocky Plains Unit (HPU).
273 The gratings consisted of evenly spaced ridges that were signaled through individual ICMS pulses
274 and detectable, the CO2 fluxes at mid-ocean ridges, the depth of the lithosphere-asthenosphere bound
275 ets, we show here that, for dewetting liquid ridges, this property can be dramatically altered by the
276 ted over the TAG Segment of the Mid-Atlantic Ridge to constrain the tectonic evolution of these block
278 ecause waters depressurize as they flow from ridge to valley and because pores have dilated as the de
279 itol polyphosphate-5-phosphatase E (Inpp5e), ridge top (rdg), with expanded ventral neural cell fates
280 ng individual nuclei using a tree-structured ridge-tracing method followed by shape ranking according
282 nt odontodes that are added lingually to the ridges turn into conical teeth and undergo cyclic replac
284 at the ultraslow-spreading Gakkel mid-ocean ridge under the Arctic Ocean, where the lithosphere is t
285 onHf = 15.11) whereas those from the Valu Fa ridge (VFR) vary from 0.283221 (epsilonHf = 15.88) to 0.
286 rmed surface structures such as wrinkles and ridges via sequential polymerization on paper substrates
287 ions, our results demonstrate that mid-ocean-ridge volcanoes may have magmatic roots deep in the lith
289 ork and the trailing edge orientation of the ridge was identified as the most important parameter to
295 radiographic dimensional changes in alveolar ridge width with an average horizontal bone gain of 3.6
296 The effects of sex, age, estimated baseline ridge width, number of missing teeth in site, site type
299 c, and was accompanied by effacement of rete ridges with reduced deposition of both elastic fibers an