ライフサイエンスコーパス: facies

1 kstone, packstone-grainstone, and grainstone facies).

2 al mosaic (Gravettian) with several regional facies.

3 problems, bone abnormalities and dysmorphic facies.

4 nd interchannel facies being the predominant facies.

5 ivided into three units based on sedimentary facies.

6 microbialites and associated biogeochemical facies.

7 s flow facies, channel facies and floodplain facies.

8 between oxidized and reduced biogeochemical facies.

9 , but may be enhanced through more permeable facies.

10 of fossils in mixed fluvial and gravity flow facies.

11 Some patients have myopathic facies.

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

13 stems, as evidenced by preserved sedimentary facies.

14 classical lissencephaly and a characteristic facies.

15 ), sclerodermoid features (91%), and leonine facies (39%).

16 r whose major features include a distinctive facies, a wide spectrum of cardiac defects, short statur

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

18 Facies analysis of published carbon-isotopic records ind

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

20 ted workflow for reservoir characterization, facies analysis, and rock typing.

21 We hypothesized, based on the interpretive facies analysis, that the Chittagong Tripura fold belt r

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

23 the critical interplay between depositional facies and diagenetic processes in determining reservoir

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

25 Notably, coarse facies and distal skeletal anomalies, as defined by OMIM

26 d into several environments depending on the facies and electrofacies characteristics of the formatio

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

28 are characterized by Na-Cl hydrogeochemical facies and high total dissolved solids.

29 Relationships between facies and hydrobiogeochemical properties enable facies-

30 osis (non-fatigable in adulthood), myopathic facies and marked axial weakness, especially of neck fle

31 use "neurodevelopmental disorder with coarse facies and mild distal skeletal abnormalities." Here, by

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

33 Seven main facies and several secondary facies have been deposited

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

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

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

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

38 parallel laminated bed, cumulative sandstone facies, and cumulative shale facies shows around 10.8%,

39 The study includes petrographic, facies, and depositional models for the study area.

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

41 , walking and speech impairments, dysmorphic facies, and neutropenia.

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

43 deposits), channelized sandstone contourite facies, and shallow marine sandstone.

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

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

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

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

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

49 The facies are distinguished according to the grain or mud s

50 nalog for the microbialite-micritic sediment facies associations that are so prevalent in the geologi

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

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

53 nd physical properties to define sedimentary facies at seven core sites.

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

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

56 oss 4 Ma of stratigraphy, and coincides with facies-based markers of flooding, such as mass-preservat

57 to illite particles that are abundant in the facies bearing MRS, but not in the host sandstone and bl

58 with braided river channels and interchannel facies being the predominant facies.

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

60 -2 GPa) at the plagioclase-spinel peridotite facies boundary to the surface.

61 lities of the brain and skeleton, dysmorphic facies, brachydactyly, seizures, and hypoplastic externa

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

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

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

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

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

67 om channel-dominated to floodplain-dominated facies commonly observed in foreland basin stratigraphy.

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

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

70 ring exhumation at granulite and amphibolite facies conditions.

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

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

73 weakness, scoliosis, rigid spine, dysmorphic facies, cutaneous involvement, respiratory failure, and

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

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

76 congruent clinical features including coarse facies, developmental delay, intellectual disability, an

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

78 mafic lowermost crustal layer into eclogite facies during Paleoproterozoic orogeny without later del

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

80 as criterion for differentiating associated facies (e.g., turbidites, debrites), though not without

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

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

83 ding periods of simultaneous debris and wash facies forming processes, erosion, and reworking.

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

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

86 omagnetism, plate-circuit analyses, sediment facies, geodynamic modeling, and geochemistry suggest mo

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

88 Nine sedimentary facies have been defined.

89 Seven main facies and several secondary facies have been deposited in multiple environments.

90 Those facies have noncore depths that can be monitored by matc

91 h psychomotor retardation and characteristic facies (IHPRF).

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

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

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

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

96 eous potential, water saturation, depth, and facies) in addition to direct core permeability and poro

97 oderate intellectual disability, and similar facies, including horizontal or slightly bowed eyebrows,

98 Sedimentary facies indicate a paleodepth range from below storm wave

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

100 rmation of lower crustal rocks into eclogite facies is usually expected to result in lower crustal de

101 an index hydrous mineral for the blueschist facies, its stability at mantle depths in diverse subduc

102 ic occurrences of 'anachronistic' carbonates-facies largely absent from marine environments after the

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

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

105 rmobarometric methods applicable to eclogite-facies mafic rocks to a set of eclogites cropping out th

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

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

108 Heterogeneous hornblende-granulite facies melts from ocean crust gabbros +/- basalts fluxed

109 conditions to produce eclogites and eclogite facies metamorphic rocks.

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

111 d in part on an interpretation that eclogite-facies metamorphism and, therefore, collisional orogenes

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

113 re/pressure (thermobaric ratio) of granulite facies metamorphism peaked at over 1500 degrees C/GPa du

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

115 ated between gas sand, water sand, and shale facies, minimizing uncertainties in fluid and lithology

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

117 e identified as the following main limestone facies (mudstone, mudstone-wackestone, wackestone, wacke

118 ype of mild intellectual disability, similar facies, myopathy, and cerebral white matter hyperintensi

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

120 he Cambrian and are preserved where suitable facies occur.

121 ome (hypotonia, developmental delay, typical facies, oculomotor apraxia, polydactyly, and subtle post

122 limb spasticity, muscle wasting, dysmorphic facies, optic atrophy, leuko-axonopathy with hypomyelina

123 e unrelated to post-impact fluvio-lacustrine facies or pre-impact target bedrock.

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

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

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

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

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

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

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

131 In the geological record, eclogite-facies rocks are irrefutable indicators of subduction an

132 A granulite facies shear zone network dissects an anorthosite intrus

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

134 ative sandstone facies, and cumulative shale facies shows around 10.8%, 15.2%, 20.6%, 13.4% probabili

135 g loss, Retinitis pigmentosa and distinctive Facies (SHRF, #OMIM 617763).

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

137 retreat from the southwestern Ross Sea using facies succession and paired ramped pyrolysis oxidation

138 ntary characteristics of these allochthonous facies suggest.

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

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

141 ed or on the appearance of the configuration facies through microscopy.

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

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

144 ed bed ([Formula: see text] according to the facies transition probability matrix.

145 -section in an effort to illustrate vertical facies variations in the Upper Surma group.

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

147 marine clay devoid of sedimentary carbonate facies with thermal maturity in the early stage of the o

148 nal is present in both reefal and non-reefal facies within reef-supporting regions, suggesting that r