ライフサイエンスコーパス: creeping

1 he spectrum of fault coupling from locked to creeping.

2 bly as a result of strain dissipation along (creeping?

3 mically active portion of the fault includes creeping and transitional segments with some of the most

4 The results of this study indicate that creeping attachment (i.e., soft tissue recovery) might o

5 o additional root coverage was gained due to creeping attachment between 2 and 12 months.

6 o additional root coverage was gained due to creeping attachment between 2 and 6 months for either gr

7 inized tissue; and 4) evaluate the amount of creeping attachment obtained.

8 age between 6 months and 2 years, exhibiting creeping attachment of 0.7 +/- 0.6 mm.

9 nalysis reveals that fault groups exhibiting creeping behaviour show smaller misalignment in their fa

10 Two variants of creeping bentgrass (Agrostis stolonifera cv palustris),

11 e-specific expression of both genes in rice, creeping bentgrass (Agrostis stolonifera L.) and Arabido

12 ocuments gene flow on a landscape level from creeping bentgrass (Agrostis stolonifera L.), one of the

13 za sativa) miR528 (Osa-miR528) in transgenic creeping bentgrass (Agrostis stolonifera) alters plant d

14 wn patch (Rhizoctonia solani) and stem rust; creeping bentgrass (Agrostis stolonifera) for resistance

15 response to abiotic stress using transgenic creeping bentgrass (Agrostis stolonifera) overexpressing

16 from heterozygous populations of the species creeping bentgrass (Agrostis stolonifera).

17 Most individual creeping bentgrass plants examined are lacking Crs-1.

18 The Crs-1 locus in creeping bentgrass provides a rare example of the evolut

19 the three parental lines used to develop the creeping bentgrass variants.

20 ntified as two putative targets of miR528 in creeping bentgrass.

21 ent land plant lineage and have a flattened, creeping body (the thallus), which grows from apical cel

22 emic may not be a sudden event, but a slow, 'creeping catastrophe', impacting the most impoverished r

23 cipients with deteriorating renal function ("creeping creatinine") secondary to chronic allograft nep

24 chromatin compaction by step-like and slow "creeping" dynamics consistent with a loop-extrusion mech

25 collectively, such as when confronted with "creeping" environmental problems.

26 Creeping fat (CF) is the wrapping of mesenteric adipose

27 d the potential mechanisms involved, such as creeping fat (Clostridium innocuum) and impaired wound h

28 D) is the extra-intestinal manifestation of "creeping fat" (CrF), defined as expansion of mesenteric

29 ically adapted to the MAT contribute to the "creeping fat" of Crohn's disease.

30 kine networks, host-microbiome interactions, creeping fat, and their translation for endpoint develop

31 In areas of creeping fat, which characterizes inflammation-affected

32 sites of intestinal inflammation is known as creeping fat.

33 enteries is associated with the formation of creeping fat.

34 d ultramafic rocks have been associated with creeping faults in central and northern California, and

35 adderwort traps avoid the adverse effects of creeping flow by generating strong, fast-onset suction p

36 Whitehead paradox need be encountered in the creeping flow regime and (ii) the flux of the factor wil

37 ated streamers in a microfluidic device in a creeping flow regime using both experimental observation

38 on, a mechanism that is not effective in the creeping-flow regime where viscous forces prevent the ge

39 anding the evolution of biofilm streamers in creeping flows.

40 This creeping fluid flow has been shown to affect the morphol

41 servations suggest a new model for soil as a creeping glass, wherein environmental disturbances maint

42 Creeping grains beneath the bed-load layer give rise to

43 ding velocity and pore water pressure at two creeping landslides are explained by velocity-strengthen

44 deal, linearly polarizable sphere undergoing creeping motion in viscous medium, we have shown that bo

45 Creeping motion of a Jeffrey fluid in a small width poro

46 dditionally, we found no correlation between creeping or locked faults and tremor, contrary to predic

47 sms of the complex processes involved in the creeping porous air and water flow in the presence of ca

48 that deformation of the mechanically unusual creeping portions of the San Andreas fault system is con

49 y development was the only factor related to creeping proteinuria (hazard ratio, 2.946; 95% confidenc

50 Creeping proteinuria during the first year was associate

51 ths, variation <50%, and increase >/=50% or "creeping proteinuria") (n = 283).

52 Creeping proteinuria, which was present in 35 patients (

53 cue grass Festuca rubra subsp. rubra (strong creeping red fescue) infected with E. festucae.

54 resistance seen in endophyte-infected strong creeping red fescue.

55 n indicates that the surface fault traces of creeping regions tend to be simple, whereas locked regio

56 rancisco' and 'Los Angeles' repeaters on the creeping section of the San Andreas Fault.

57 terizing the northwest ~75 kilometers of the creeping segment as a transition zone, with potential im

58 equences to constrain friction properties of creeping segments.

59 identification of a gene, designated Crs-1 (creeping specific-1), that appears to be in the process

60 nset is instead a continuous transition from creeping to granular flow.

61 ces an instantaneous deformation followed by creeping to the asymptotic response.

62 nstantaneous deformation followed by gradual creeping to the long-term response.

63 ger a broad range of slip events, from slow, creeping transients to dynamic earthquake ruptures.

64 K is not a direct (two-state) process, but a creeping transition that takes place through at least on

65 As the blood pressure trajectory continues creeping upward in LMICs, contextual research on effecti

66 The sex chromosome karyotype of the creeping vole (Microtus oregoni) represents a long-stand

67 In the creeping vole, Microtus oregoni, females are X0 and male

68 ld, California, near the southern end of the creeping zone.

69 historical times, separated by a 150-km-long creeping zone.

70 the region of coseismic slip and the up-dip creeping zone.