ライフサイエンスコーパス: lowermost

1 For both species, populations at the lowermost altitude presented older age structure, higher

2 of the uppermost valence band (UVB) and the lowermost conduction band (LCB) in bulk and atomically t

3 lated that their ultimate destination is the lowermost few hundred kilometres of the mantle, known as

4 units interbedded with uppermost Triassic to lowermost Jurassic sediments.

5 iple, piecewise continuous interfaces in the lowermost layer (D'') beneath Central and North America.

6 In the lowermost layer of the atmosphere-the troposphere-ozone

7 overlain by an isotropic, high-conductivity lowermost lithosphere.

8 ents in a low-shear-velocity province in the lowermost mantle (D'' region) beneath the central Pacifi

9 ogical and electromagnetic properties of the lowermost mantle (D'') is important to understand the fo

10 ser than the surrounding solid phases in the lowermost mantle and that melts will be trapped above th

11 erential travel times of phases sensitive to lowermost mantle beneath the central Pacific reveals lat

12 P waves turning in the lowermost mantle beneath the same region also have anoma

13 ompositional variation should strengthen the lowermost mantle between 1,800 km depth and 2,000 km dep

14 nic lithosphere materials transported to the lowermost mantle by subducting slabs.

15 Stable Mg-rich magnesiowustite in lowermost mantle can destabilize FeO in the core-mantle

16 The modern view of Earth's lowermost mantle considers a D'' region of enhanced (sei

17 gical observations provide evidence that the lowermost mantle contains superposed thermal and composi

18 modeling suggests a sharp transition in the lowermost mantle from a broad slow region to a broad fas

19 o-called ScS and SKKS waves, which probe the lowermost mantle from above and below, respectively, rev

20 Earth's lowermost mantle has thermal, chemical, and mineralogica

21 Some regions of the lowermost mantle have been observed to have seismic wave

22 tanding deformation of mineral phases in the lowermost mantle is important for interpreting seismic a

23 Our results imply that the lowermost mantle is more complex than hitherto thought a

24 The Earth's lowermost mantle large low velocity provinces are accomp

25 Seismic anomalies in the outer core and the lowermost mantle may be due to magnetic collapse of ferr

26 mologists have known for many years that the lowermost mantle of the Earth is complex.

27 e perovskite (Pv) to postperovskite (pPv) at lowermost mantle pressure-temperature (P - T) conditions

28 We find that the hottest lowermost mantle regions are commonly located well withi

29 The pattern of lowermost mantle structure at the core-mantle boundary i

30 se-boundary crossing directly constrains the lowermost mantle temperature gradients.

31 ase to explain the seismic properties of the lowermost mantle through coupled ab initio and seismic m

32 Compressional waves that sample the lowermost mantle west of Central America show a rapid ch

33 decouple the mantle above 2,000 km from the lowermost mantle, and provide a rheological basis for th

34 ation for laterally varying viscosity in the lowermost mantle, as required by long-period geoid model

35 he basaltic materials are accumulated at the lowermost mantle, high electrical conductivity of these

36 estabilize high-temperature anomalies in the lowermost mantle, in disagreement with the seismic obser

37 In the lowermost mantle, near the core-mantle boundary, denser

38 compositions) at the P - T conditions of the lowermost mantle, searching for candidate rocks with a s

39 A unique structure in the Earth's lowermost mantle, the Perm Anomaly, was recently identif

40 uated to reveal the thermal structure of the lowermost mantle, where no phase transitions were previo

41 and seismologically distinct regions of the lowermost mantle, which may organize global mantle flow

42 The thermal structure of the Earth's lowermost mantle--the D'' layer spanning depths of appro

43 be present in the D'' region of the Earth's lowermost mantle.

44 ilizing compositional heterogeneities in the lowermost mantle.

45 rly immune from the influence exerted by the lowermost mantle.

46 ditions and evidences of its presence in the lowermost mantle.

47 und to be stable under the conditions of the lowermost mantle.

48 tes and the seismological counterpart in the lowermost mantle.

49 py and X-ray diffraction to pressures of the lowermost mantle.

50 on for the seismic wave heterogeneity in the lowermost mantle.

51 m an anomalously hot overlying region of the lowermost mantle.

52 plumes, including Hawaii, may also reach the lowermost mantle.

53 e, and in solution in magnesiowustite in the lowermost mantle.

54 ing that dense metallic melt may form in the lowermost mantle.

55 ix well-resolved plumes that extend into the lowermost mantle: Ascension, Azores, Canary, Easter, Sam

56 the uppermost mantle or lithosphere and the lowermost-mantle analogue of the lithosphere, the D" reg

57 erovskite polymorphs of MgSiO3, performed at lowermost-mantle temperatures and pressures.

58 and provides a Carnian age constraint on the lowermost part of the Baijiantan Formation.

59 The lowermost part of the Earth's mantle-known as D''-shows

60 of seismic heterogeneities in the middle to lowermost parts of the lower mantle.

61 Our results imply that the middle to lowermost parts of the lower-mantle would exhibit enhanc

62 ing associated with volcanic aerosols in the lowermost stratosphere (LMS) had not been considered.

63 approximately 50 kilometers, descend to the lowermost stratosphere and are followed by anomalous tro

64 from persistent circulation anomalies in the lowermost stratosphere and is greatest during boreal win

65 Its lowermost third receives the axons of the clawed class I

66 ps previously known only from the Middle and lowermost Upper Triassic outside North America.