ライフサイエンスコーパス: extensional

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 tectonic cycle), accompanied by inversion of extensional basins and reactivation of faults and other

6 inct plates, separated from each other by an extensional Bellingshausen plate boundary active in the

7 etamorphic phase of the Orogeny lasted 8 my, extensional collapse and exhumation of midcrustal rocks

8 the Pn anisotropy directions agree with the extensional component of the right-lateral shear strains

9 c lower-crustal and upper-mantle lithosphere extensional deformation, suggesting a pure-shear rifting

10 ompressional deformation followed by Neogene extensional deformation, the Colorado plateau is largely

11 on of anisotropic crustal minerals caused by extensional deformation.

12 e or overlapping phases of contractional and extensional deformation.

13 ng of sediment in the Guaymas Basin, a young extensional depression, causes mass production and disch

14 This extensional direction matches perfectly also with the so

15 this large underthrusting event, intraplate extensional earthquakes commenced in the outer rise regi

16 roducing one of the largest recorded shallow extensional earthquakes.

17 crustal thinning can be accomplished in such extensional environments by a system of conjugate concav

18 layers along a carbonate-hosted seismogenic extensional fault in the central Apennines, Italy.

19 s of the Earth's crust deform by distributed extensional faulting and complex fault interactions are

20 ithosphere, resulting in a global network of extensional faults that closely replicate the observed f

21 The presence of spatial confinement and extensional flow also enhances entropic fluctuations, lo

22 ces protein aggregation after exposure to an extensional flow field for 0.36-1.8 ms, at concentration

23 This extensional flow is promoted by shear thinning, a typica

24 fined and quantified flow field dominated by extensional flow on the aggregation of BSA, beta2-microg

25 Together, these data indicate that an extensional flow readily unfolds thermodynamically and k

26 ble Escherichia coli DNA molecules in planar extensional flow were visualized in dilute solution by f

27 g to uniformly deliver cells to a stretching extensional flow where cells are deformed at high strain

28 Such forces have been generated using extensional flow, ultrasonic irradiation, receding menis

29 nanostructures is accomplished using planar extensional flow, which induces alignment of underlying

30 cells near the stagnation point of a planar extensional flow.

31 section occurs in a region with considerable extensional flow.

32 recent studies of single DNA molecules under extensional force.

33 luorocyclopropanated polybutadiene using the extensional forces generated by pulsed sonication of dil

34 ecular spring that resists microtubule-based extensional forces in mitosis.

35 The inherited extensional history can either suppress or enhance melt

36 Surprisingly, extensional integrity is unaffected by an inhibitor of t

37 The set of alignments can be considered an extensional interpretation of the sentence.

38 s the onset of elastic instabilities in both extensional (irrotational) and torsional (rotational) vi

39 r force increased to a certain level, sudden extensional jumps that signify domain unfolding were oft

40 force interplay exists between predominantly extensional microtubule-based spindle forces and restori

41 However, because the frequency of the extensional mode is much lower than that of the breathin

42 h lower than that of the breathing mode, the extensional mode will dominate the response for a real e

43 cles from the nonlinear optical response: an extensional mode with longitudinal expansion and transve

44 d agreement with the expected values for the extensional modes of the rods.

45 margins of the Gulf display largely dip-slip extensional movement and accompanying footwall uplift.

46 ed westward, and a dike propagated along the extensional north rift.

47 that centromere chromatin loops generate an extensional/poleward force sufficient to release nucleos

48 oparticles as bright low-drag rotational and extensional probes, which are monitored by instrumentati

49 In the Basin and Range extensional province of the western United States, cosei

50 idence of crustal radial anisotropy with the extensional provinces of the western United States sugge

51 Microtubules exert extensional pulling force on sister chromatids toward op

52 Third, the extensional response strongly depends upon the initial p

53 0 mg/mL) density fibrin gels using shear and extensional rheology.

54 by a microfluidic optimized-shape cross-slot extensional rheometer (OSCER).

55 emberment with or without the development of extensional shear zones is proposed to have induced foun

56 show that the spacing initially decreases as extensional strain increases in the direction perpendicu

57 er which these alternate mechanisms localize extensional strain remain controversial.

58 es result from competition between shear and extensional strains in the flowing granular bed.

59 in cross-linked actin networks subjected to extensional stress depends on the interplay between netw

60 role in driving deformation, modulating the extensional stress field generated by internal buoyancy

61 the intrusions indicate a globally isotropic extensional stress state arising from an increase in the

62 g of a buried cysteine residue in BSA during extensional stress.

63 ven by a deep magmatic heat source, and high extensional stresses ahead of the ridge tip have created

64 eigh wave motion was dominated by horizontal extensional stresses reaching 25 kilopascals.

65 r of the lower crust may help to explain the extensional structures observed in the Basin and Range p

66 ocal base-level changes and Miocene regional extensional tectonics.

67 o be currently active, but experienced major extensional tectonism and resurfacing (probably cryovolc

68 nsion curves showed temperature-independent, extensional transitions that could not be fitted with a

69 ndary tectonic landforms that include narrow extensional troughs or graben, splay faults, and multipl

70 landforms, contractional wrinkle ridges and extensional troughs, have distributions and age relation

71 The viscosity and extensional viscosity are increased markedly, leading to