ライフサイエンスコーパス: facies

1 ivided into three units based on sedimentary facies.

2 microbialites and associated biogeochemical facies.

3 s flow facies, channel facies and floodplain facies.

4 between oxidized and reduced biogeochemical facies.

5 , but may be enhanced through more permeable facies.

6 of fossils in mixed fluvial and gravity flow facies.

7 Some patients have myopathic facies.

8 l hyperplasia, acne, alopecia, or cushingoid facies.

9 stems, as evidenced by preserved sedimentary facies.

10 classical lissencephaly and a characteristic facies.

11 time and space in the different sedimentary facies across the Donbas Fold Belt, illustrating a domin

12 Facies analysis of published carbon-isotopic records ind

13 c reconstructions, palaeotidal modelling and facies analysis suggest that elevated tidal range and be

14 or generalized dystonia and a characteristic facies and body habitus, in an Australian family.

15 ess in both lower limbs, ataxia and abnormal facies and diagnosed on Computed Tomography.

16 imentary facies: debris flow facies, channel facies and floodplain facies.

17 Relationships between facies and hydrobiogeochemical properties enable facies-

18 , and an overgrowth disorder with dysmorphic facies and psychosis, none of which overlaps with the cl

19 w that the organization of high-permeability facies and their connectivity control the dynamics of gr

20 microbial taxa-was lower within the reduced facies and was well-explained by a combination of pH and

21 t, with coal deposition, subordinate fluvial facies, and abundant lower and middle shoreface facies,

22 he interphalangeal joints, by characteristic facies, and by deafness.

23 ding lymphoid hyperplasia, coarsening of the facies, and increased body fat.

24 role in the development of the heart, limb, facies, and other neural crest-derived structures.

25 ples were characterized to define geological facies, and the relationships among physical properties

26 en a group with layers of fossils in fluvial facies, and third a group with a layer of fossils in mix

27 affected individuals with similar dysmorphic facies, and three of them had either complete situs inve

28 by a Markov Chain approach, which represent facies architecture by commonly observed characteristics

29 e chitinozoans differ between limestone/marl facies are deemed insufficient for the identification of

30 tely 2.4 GPa, then exhumed back to granulite facies at approximately 0.9 GPa before approximately 1.8

31 ly 1.90 Ga when it was subducted to eclogite facies at approximately 2.4 GPa, then exhumed back to gr

32 n-diffusion transport of CO2 with a focus on facies-based bimodal heterogeneity.

33 es and hydrobiogeochemical properties enable facies-based conditional simulation/mapping of these pro

34 As the eclogite facies boundary has a positive dP/dT, cooling from supra

35 r propagation is reduced in low permeability facies, but may be enhanced through more permeable facie

36 ll length, cannot be explained by Waltherian facies change, host availability, salinity, diversity, t

37 tudy of stratigraphic relationships, such as facies changes and hiatuses, within the deposit.

38 d subsidence were hence in pace, with subtle facies changes likely representing relative sea-level ch

39 ee different sedimentary facies: debris flow facies, channel facies and floodplain facies.

40 ies, and abundant lower and middle shoreface facies, comprising an intercalated package of potential

41 h were thoroughly dehydrated under granulite facies conditions during a Neoproterozoic event (about 9

42 Classic features are dysmorphic facies, conotruncal cardiac defects, hypocalcemic hypopa

43 However, our analysis of climate and facies considerations shows that the effects of bolide i

44 ppear related to three different sedimentary facies: debris flow facies, channel facies and floodplai

45 recessive disorder characterized by unusual facies, dental anomalies, hypotrichosis, palmoplantar hy

46 vidence for palaeosols comes from non-marine facies, dilation cracks, soil nodules, sand crystals, st

47 l findings (i.e., a male with characteristic facies, dysostosis multiplex, and mental retardation) an

48 ithofacies and elucidate relationships among facies features and microbial community biomass, richnes

49 from the spatial organization of sedimentary facies, finger propagation is reduced in low permeabilit

50 ental motifs based on changes in sedimentary facies, fossil assemblages, geochemistry, and paleotempe

51 High-pressure (0.8 gigapascals) granulite facies garnet from Gore Mountain, New York, hosts multip

52 drome (C for cognitive impairment and coarse facies, H for heart defects, O for obesity, P for pulmon

53 Nine sedimentary facies have been defined.

54 h psychomotor retardation and characteristic facies (IHPRF).

55 sixfold increase in the flux of U to anoxic facies, implying a corresponding increase in the extent

56 y be explained by initial deposition of this facies in a freshwater setting.

57 plantar subcutaneous nodules and distinctive facies in a number of consanguineous Saudi Arabian famil

58 ed in stable carbon isotopes and sedimentary facies in lacustrine strata.

59 Sedimentary facies indicate a paleodepth range from below storm wave

60 The connectivity of facies is critical in determining the large-scale transp

61 aracterized by short stature, characteristic facies, learning problems and leukemia predisposition.

62 rgan developmental abnormalities, dysmorphic facies, limb malformations and mental retardation.

63 on in a representative oil-prone black shale facies may be more closely related to patterns of contin

64 cal and lateral changes of these sedimentary facies may be the result of temporal and spatial changes

65 conditions to produce eclogites and eclogite facies metamorphic rocks.

66 interest in relationships between blueschist-facies metamorphism and seismicity, particularly through

67 probe data that dates the timing of eclogite facies metamorphism in eastern Papua New Guinea at 4.3 +

68 dvection of heat by melt generates granulite facies metamorphism, and widespread andalusite-sillimani

69 erate dozens of previously documented common facies models and a variety of property assignments.

70 Thermally distinct ejecta facies occur around some craters with variations associa

71 he Cambrian and are preserved where suitable facies occur.

72 Here, we characterize three biogeochemical facies-oxidized, reduced, and transition-within one lith

73 lationships among physical properties of the facies, physicochemical attributes of the local environm

74 al melting of hydrous basalt in the eclogite facies produces granitoid liquids with major- and trace-

75 te degree of mental retardation (MR), coarse facies, puffy eyelids, narrow palpebral fissures, promin

76 A distinct sediment facies recovered from a bedrock basin in Pine Island Bay

77 However, lithologies, facies relations, geomorphology, and paleotopography of

78 ubsurface biogeochemical facies with biomass-facies relationships revealed here.

79 n genetic disorder, characterized by typical facies, short stature, developmental delay, and cardiac

80 The main features are pugilistic facies, skeletal deformities, and muscular hypertrophy d

81 ntary characteristics of these allochthonous facies suggest.

82 ind elevated biomass within a biogeochemical facies that occurred at the transition between oxidized

83 ng the relationships between the sedimentary facies, the clasts and archaeo-palaeontological remains.

84 ed to as CATCH-22 (cardiac defects, abnormal facies, thymic hypoplasia, cleft palate, hypocalcemia, a

85 portunity to use the spatial distribution of facies to predict spatial variation in biogeochemically

86 al distribution of subsurface biogeochemical facies with biomass-facies relationships revealed here.