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1 hanges in the top and bottom portions of the lowermost ~300 km mantle.
2 his relationship, we focused analyses on the lowermost 500 kilometers of the Mississippi River, where
3         For both species, populations at the lowermost altitude presented older age structure, higher
4  of the uppermost valence band (UVB) and the lowermost conduction band (LCB) in bulk and atomically t
5 ansport of melts in the uppermost mantle and lowermost crust(6,7).
6 ly thinned high-velocity (Vp ~ 7.3-7.4 km/s) lowermost crust, which extends over >350 km distance.
7  amphibole-olivine-pyroxene cumulates in the lowermost crust.
8 (50-70%) transformation of part of the mafic lowermost crustal layer into eclogite facies during Pale
9 t cover the crater peak ring, just below the lowermost Danian pelagic limestone.
10 lated that their ultimate destination is the lowermost few hundred kilometres of the mantle, known as
11 units interbedded with uppermost Triassic to lowermost Jurassic sediments.
12  'interglacial period'(1,3) during which the lowermost latitude LDM ice(4-6) was etched and removed,
13 iple, piecewise continuous interfaces in the lowermost layer (D'') beneath Central and North America.
14                                       In the lowermost layer of the atmosphere-the troposphere-ozone
15  overlain by an isotropic, high-conductivity lowermost lithosphere.
16 ents in a low-shear-velocity province in the lowermost mantle (D'' region) beneath the central Pacifi
17 ogical and electromagnetic properties of the lowermost mantle (D'') is important to understand the fo
18 ser than the surrounding solid phases in the lowermost mantle and that melts will be trapped above th
19 Low Shear Velocity Provinces (LLSVPs) in the lowermost mantle are key to understanding the chemical c
20 erential travel times of phases sensitive to lowermost mantle beneath the central Pacific reveals lat
21                       P waves turning in the lowermost mantle beneath the same region also have anoma
22 ompositional variation should strengthen the lowermost mantle between 1,800 km depth and 2,000 km dep
23 nic lithosphere materials transported to the lowermost mantle by subducting slabs.
24            Stable Mg-rich magnesiowustite in lowermost mantle can destabilize FeO in the core-mantle
25                   The modern view of Earth's lowermost mantle considers a D'' region of enhanced (sei
26 gical observations provide evidence that the lowermost mantle contains superposed thermal and composi
27  modeling suggests a sharp transition in the lowermost mantle from a broad slow region to a broad fas
28 o-called ScS and SKKS waves, which probe the lowermost mantle from above and below, respectively, rev
29                                      Earth's lowermost mantle has thermal, chemical, and mineralogica
30                          Some regions of the lowermost mantle have been observed to have seismic wave
31 tanding deformation of mineral phases in the lowermost mantle is important for interpreting seismic a
32                   Our results imply that the lowermost mantle is more complex than hitherto thought a
33                                  The Earth's lowermost mantle large low velocity provinces are accomp
34  Seismic anomalies in the outer core and the lowermost mantle may be due to magnetic collapse of ferr
35 signature of surface carbon reaching Earth's lowermost mantle may include CaCO(3).
36 mologists have known for many years that the lowermost mantle of the Earth is complex.
37 calized material flows and the region of the lowermost mantle possesses a separate layer circulation.
38 e perovskite (Pv) to postperovskite (pPv) at lowermost mantle pressure-temperature (P - T) conditions
39                     We find that the hottest lowermost mantle regions are commonly located well withi
40                                          The lowermost mantle right above the core-mantle boundary is
41                               The pattern of lowermost mantle structure at the core-mantle boundary i
42 se-boundary crossing directly constrains the lowermost mantle temperature gradients.
43 ase to explain the seismic properties of the lowermost mantle through coupled ab initio and seismic m
44          Compressional waves that sample the lowermost mantle west of Central America show a rapid ch
45 s can be globally distributed throughout the lowermost mantle with variable concentrations.
46 large low-velocity provinces (LLVPs), in the lowermost mantle(1).
47  decouple the mantle above 2,000 km from the lowermost mantle, and provide a rheological basis for th
48 ation for laterally varying viscosity in the lowermost mantle, as required by long-period geoid model
49 he basaltic materials are accumulated at the lowermost mantle, high electrical conductivity of these
50 estabilize high-temperature anomalies in the lowermost mantle, in disagreement with the seismic obser
51                                       In the lowermost mantle, near the core-mantle boundary, denser
52 compositions) at the P - T conditions of the lowermost mantle, searching for candidate rocks with a s
53            A unique structure in the Earth's lowermost mantle, the Perm Anomaly, was recently identif
54 MgCO(3) under reducing conditions of Earth's lowermost mantle, these observations allow us to predict
55 uated to reveal the thermal structure of the lowermost mantle, where no phase transitions were previo
56  and seismologically distinct regions of the lowermost mantle, which may organize global mantle flow
57  to monitor dynamic processes in the Earth's lowermost mantle, yet no related seismic observations we
58         The thermal structure of the Earth's lowermost mantle--the D'' layer spanning depths of appro
59  be present in the D'' region of the Earth's lowermost mantle.
60 ilizing compositional heterogeneities in the lowermost mantle.
61 rly immune from the influence exerted by the lowermost mantle.
62 ditions and evidences of its presence in the lowermost mantle.
63 tes and the seismological counterpart in the lowermost mantle.
64 py and X-ray diffraction to pressures of the lowermost mantle.
65 on for the seismic wave heterogeneity in the lowermost mantle.
66 m an anomalously hot overlying region of the lowermost mantle.
67 plumes, including Hawaii, may also reach the lowermost mantle.
68 und to be stable under the conditions of the lowermost mantle.
69 e, and in solution in magnesiowustite in the lowermost mantle.
70 for Fe(1-x)O wustite to pressures of Earth's lowermost mantle.
71 ing that dense metallic melt may form in the lowermost mantle.
72 welling of buoyant material sourced from the lowermost mantle.
73 s of decadal-scale structural changes in the lowermost mantle: (1) a 10s km-scale shrinkage or moveme
74 ix well-resolved plumes that extend into the lowermost mantle: Ascension, Azores, Canary, Easter, Sam
75  the uppermost mantle or lithosphere and the lowermost-mantle analogue of the lithosphere, the D" reg
76 )/V(S) ratio than MgSiO(3) bridgmanite under lowermost-mantle conditions.
77 g that BMO fractional crystallization yields lowermost-mantle densities much higher than those of LLV
78 erovskite polymorphs of MgSiO3, performed at lowermost-mantle temperatures and pressures.
79 s a direct expression of the dynamics of the lowermost martian atmosphere.
80                                          The lowermost metal layer is a high melting point solder and
81 and provides a Carnian age constraint on the lowermost part of the Baijiantan Formation.
82            Only a single individual from the lowermost part of the Cerithium Limestone is considered
83                                          The lowermost part of the Earth's mantle-known as D''-shows
84  of seismic heterogeneities in the middle to lowermost parts of the lower mantle.
85         Our results imply that the middle to lowermost parts of the lower-mantle would exhibit enhanc
86                                          The lowermost portion of Earth's mantle (D") above the core-
87 ing associated with volcanic aerosols in the lowermost stratosphere (LMS) had not been considered.
88  approximately 50 kilometers, descend to the lowermost stratosphere and are followed by anomalous tro
89 from persistent circulation anomalies in the lowermost stratosphere and is greatest during boreal win
90 ., upper troposphere, tropopause region, and lowermost stratosphere).
91  models show a substantial moist bias in the lowermost stratosphere.
92 phere to the abundance of water vapor in the lowermost stratosphere.
93  experiment and inter-model variability that lowermost stratospheric water vapor decreases local temp
94                                       Hence, lowermost stratospheric water vapor exerts a first order
95                                          Its lowermost third receives the axons of the clawed class I
96 ps previously known only from the Middle and lowermost Upper Triassic outside North America.