戻る
「早戻しボタン」を押すと検索画面に戻ります。 [閉じる]

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             This analysis predicts that both extensional and breathing vibrational modes of the rods
2 e develop finite-element models subjected to extensional and gravitational forces to study time-varyi
3 omain above this platform enables a range of extensional and rotational motions without precedent in
4                                        Using extensional and shear rheology we found that cervical mu
5 cre grows in a dynamic two-step process with extensional and space-filling growth components.
6 ween these characteristics and the inherited extensional architecture remains enigmatic.
7 tectonic cycle), accompanied by inversion of extensional basins and reactivation of faults and other
8  arid climate and the presence of landlocked extensional basins in thickened orogenic settings.
9  - form through inversion of pre-collisional extensional basins.
10 inct plates, separated from each other by an extensional Bellingshausen plate boundary active in the
11 etamorphic phase of the Orogeny lasted 8 my, extensional collapse and exhumation of midcrustal rocks
12 ting, following slab rollback, promoted this extensional collapse.
13  the Pn anisotropy directions agree with the extensional component of the right-lateral shear strains
14 tivated structures with strike-slip and even extensional components, thus providing a valid mechanism
15 ka Thrust after this small fluid-loss by the extensional crack formation does not exceed 0.15.
16   It is thought that extensional structures (extensional cracks and normal faults) generated during t
17 d pressure reduction due to the post-seismic extensional cracks contributes little to increase the fa
18 in formation indicates that the formation of extensional cracks only releases up to ~ 7-8% of the tot
19 c lower-crustal and upper-mantle lithosphere extensional deformation, suggesting a pure-shear rifting
20 ompressional deformation followed by Neogene extensional deformation, the Colorado plateau is largely
21 on of anisotropic crustal minerals caused by extensional deformation.
22 e or overlapping phases of contractional and extensional deformation.
23         In the scarcely-treated mucus-sputum extensional deformations, BMP+[Formula: see text] predic
24 ng of sediment in the Guaymas Basin, a young extensional depression, causes mass production and disch
25 ctors controlling direction and magnitude of extensional deviatoric stresses that produced topographi
26                                         This extensional direction matches perfectly also with the so
27  this large underthrusting event, intraplate extensional earthquakes commenced in the outer rise regi
28 roducing one of the largest recorded shallow extensional earthquakes.
29 ation for reverse-faulting earthquakes in an extensional environment.
30 crustal thinning can be accomplished in such extensional environments by a system of conjugate concav
31 nt scission during the same high strain rate extensional event in which it is formed and furthermore
32  layers along a carbonate-hosted seismogenic extensional fault in the central Apennines, Italy.
33 s of the Earth's crust deform by distributed extensional faulting and complex fault interactions are
34 ithosphere, resulting in a global network of extensional faults that closely replicate the observed f
35      The presence of spatial confinement and extensional flow also enhances entropic fluctuations, lo
36 rmation index (DI) of the cells stretched by extensional flow at the stagnation point of a cross-slot
37 shear flow deformability cytometry (sDC) and extensional flow deformability cytometry (xDC).
38 ces protein aggregation after exposure to an extensional flow field for 0.36-1.8 ms, at concentration
39  that are stretched and oriented in a strong extensional flow field resulting from the streamwise gra
40                                         This extensional flow is promoted by shear thinning, a typica
41 arge conformational fluctuations of rings in extensional flow long after the initial transient stretc
42 fined and quantified flow field dominated by extensional flow on the aggregation of BSA, beta2-microg
43                                              Extensional flow properties of polymer solutions in vola
44        Together, these data indicate that an extensional flow readily unfolds thermodynamically and k
45 ble Escherichia coli DNA molecules in planar extensional flow were visualized in dilute solution by f
46 g to uniformly deliver cells to a stretching extensional flow where cells are deformed at high strain
47 x chemistry) and physical (mechanical shear, extensional flow) stimuli to trigger the transition from
48        Such forces have been generated using extensional flow, ultrasonic irradiation, receding menis
49  nanostructures is accomplished using planar extensional flow, which induces alignment of underlying
50  cells near the stagnation point of a planar extensional flow.
51 section occurs in a region with considerable extensional flow.
52  LCE inks are subjected to coupled shear and extensional flows that can be harnessed to spatially con
53 hysical cytometry under tunable viscoelastic extensional flows to modulate the geometry for cell defo
54 expectoration processes, with mixed shear-to-extensional flows.
55 folded tubes were severed when an additional extensional force was applied, consistent with a frictio
56 recent studies of single DNA molecules under extensional force.
57 luorocyclopropanated polybutadiene using the extensional forces generated by pulsed sonication of dil
58 ecular spring that resists microtubule-based extensional forces in mitosis.
59                                The inherited extensional history can either suppress or enhance melt
60 nd deep lithospheric structures, showing how extensional inheritance influences mountain building on
61                                Surprisingly, extensional integrity is unaffected by an inhibitor of t
62   The set of alignments can be considered an extensional interpretation of the sentence.
63 s the onset of elastic instabilities in both extensional (irrotational) and torsional (rotational) vi
64 r force increased to a certain level, sudden extensional jumps that signify domain unfolding were oft
65 force interplay exists between predominantly extensional microtubule-based spindle forces and restori
66        However, because the frequency of the extensional mode is much lower than that of the breathin
67 h lower than that of the breathing mode, the extensional mode will dominate the response for a real e
68 cles from the nonlinear optical response: an extensional mode with longitudinal expansion and transve
69 d agreement with the expected values for the extensional modes of the rods.
70 margins of the Gulf display largely dip-slip extensional movement and accompanying footwall uplift.
71 ed westward, and a dike propagated along the extensional north rift.
72  that centromere chromatin loops generate an extensional/poleward force sufficient to release nucleos
73 oparticles as bright low-drag rotational and extensional probes, which are monitored by instrumentati
74  (DW) which significantly enhanced the dough extensional properties, increased the bread specific vol
75 us liquids" and "gels", and also had varying extensional properties.
76                       In the Basin and Range extensional province of the western United States, cosei
77 mented normal faults in the western Anatolia Extensional Province, to quantify the role of rock uplif
78 idence of crustal radial anisotropy with the extensional provinces of the western United States sugge
79                           Microtubules exert extensional pulling force on sister chromatids toward op
80                    The poro-elastic model of extensional quartz vein formation indicates that the for
81                            Here we show that extensional quartz veins at the Garrcon deposit in the A
82 c melts primarily ascend westward due to the extensional regime in the west and physical barrier effe
83 ng how alluvial fans respond to tectonics in extensional regions.
84      Evaporation substantially increased the extensional relaxation time [Formula: see text] for PEO
85  exponentially-slow thinning of neck radius (extensional relaxation time is determined from the delay
86 rrelated with the corresponding variation in extensional relaxation time.
87 d multimer contours, and large variations in extensional response behaviors.
88                                   Third, the extensional response strongly depends upon the initial p
89 ic resonance characterization, and shear and extensional rheology consistent with highly branched pol
90 oration during dripping-onto-substrate (DoS) extensional rheology measurements, we developed a chambe
91  the first to control evaporation during DoS extensional rheology, and provide guidelines establishin
92 0 mg/mL) density fibrin gels using shear and extensional rheology.
93 by a microfluidic optimized-shape cross-slot extensional rheometer (OSCER).
94  to a liquid bridge (e.g., capillary breakup extensional rheometer).
95 ures, which manifests as migrating swarms of extensional seismicity along the ridge axis, can provide
96 verall morphology of alluvial fan systems in extensional settings by influencing sediment flux and ac
97 how evidence for tectonically neutral and/or extensional settings.
98 mas typically associated with rift zones and extensional settings.
99 aphene sheets by tuning the elongational and extensional shear rates, respectively.
100 emberment with or without the development of extensional shear zones is proposed to have induced foun
101 dy a ~ NNE-SSW transect, sub-parallel to the extensional strain direction, constrained by two permane
102 the first-time insight into the rift-related extensional strain fabric in the crust and upper mantle
103 show that the spacing initially decreases as extensional strain increases in the direction perpendicu
104 ze the covariation between tectonic history (extensional strain rates, paleotopography, and ruggednes
105 er which these alternate mechanisms localize extensional strain remain controversial.
106 es result from competition between shear and extensional strains in the flowing granular bed.
107 and slab steepening due to rollback, causing extensional stress and back-arc rifting in the past 2.5
108              The statistical distribution of extensional stress as it applies on models of the vWF mo
109  in cross-linked actin networks subjected to extensional stress depends on the interplay between netw
110  role in driving deformation, modulating the extensional stress field generated by internal buoyancy
111 the intrusions indicate a globally isotropic extensional stress state arising from an increase in the
112 g of a buried cysteine residue in BSA during extensional stress.
113 ven by a deep magmatic heat source, and high extensional stresses ahead of the ridge tip have created
114                      While often overlooked, extensional stresses can affect the structure of vWF at
115 eigh wave motion was dominated by horizontal extensional stresses reaching 25 kilopascals.
116                           It is thought that extensional structures (extensional cracks and normal fa
117 r of the lower crust may help to explain the extensional structures observed in the Basin and Range p
118 nic District (MSVD), Italy, coupled with the extensional tectonics of the region, pose both volcanic
119 anan margin; (ii) tectonic transformation to extensional tectonics within the Gondwanan interior; (ii
120 ocal base-level changes and Miocene regional extensional tectonics.
121 o be currently active, but experienced major extensional tectonism and resurfacing (probably cryovolc
122         We define the conditions under which extensional thinning or liquid break-up can be expected.
123 nsion curves showed temperature-independent, extensional transitions that could not be fitted with a
124 ndary tectonic landforms that include narrow extensional troughs or graben, splay faults, and multipl
125  landforms, contractional wrinkle ridges and extensional troughs, have distributions and age relation
126                            The viscosity and extensional viscosity are increased markedly, leading to
127        We deduce that the plots of transient extensional viscosity vs. Hencky strain (scaled by the r
128 rved and used for measuring terminal, steady extensional viscosity.
129 ical signature as augmented strain-hardening extensional-viscosity peaks: an additional source of flo
130 es meaningful implications beyond the simple extensional visit pattern and lends weight to the growin

 
Page Top