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1 ssal magnetoresistance in manganese oxides ('manganites').
2 which is enhanced by phase separation in the manganite.
3 dr)oxide that was composed of hausmanite and manganite.
4 and orbitally ordered phase in a perovskite manganite.
5 ormation of thermodynamically more favorable manganite.
6 d change of domain-wall pairs in a hexagonal manganite.
7 larities with the colossal magnetoresistance manganites.
8 rs and the colossal magnetoresistance in the manganites.
9 OSV devices using electronic phase separated manganites.
10 nge strains are known to be important in the manganites.
11 and charge ordering, two key features of the manganites.
12 degrees C by using yttrium-based rare earth manganites.
13 notably observed in hole-doped ferromagnetic manganites.
14 eSbTe demonstrates similar properties as the manganites.
15 segregation, reminiscent of optimally doped manganites.
16 to the repeating unit seen in the perovskite manganites.
17 MIT leads to first-order transition in these manganites.
18 agnetic transition and compared with that in manganites.
19 ing, reminiscent of the hexagonal rare earth manganites.
20 lated solids such as pnictides, cuprates and manganites.
21 e antiferromagnetic charge-ordered states in manganites.
22 agnetic, and fully antiferromagnetic bilayer manganites.
23 as well as in colossal magnetoresistance in manganites.
24 romagnetic metal for the CMR effect in doped manganites.
25 e geometrically driven tilt mechanism of the manganites.
27 erties of epitaxial thin films of perovskite manganites (a class of doped Mott insulator) as their co
29 ligned nanocomposites of lanthanum strontium manganite and doped ceria with straight applicability as
30 or the deuterons in the tunnel structures of manganite and groutite, which could be explained by cons
31 reaction intermediate that is converted into manganite and possibly hausmannite during further reacti
32 rol and manipulation of orbital order in the manganites and demonstrate a new way to use THz to under
33 ples including colossal magnetoresistance in manganites and high-T(c) superconductivity in cuprates.
34 Kondo insulators, colossal magnetoresistive manganites and high-transition temperature (high-T(c)) c
35 of colossal magnetoresistance in perovskite manganites and illustrates the role of mixed-phase coexi
37 ewed here by applying several techniques for manganites and other materials are consistent with this
38 lude the 'colossal' magnetoresistance in the manganites and the enhanced magnetoresistance in low-car
39 xide (EMD), the model compounds groutite and manganite, and deuterium intercalated ramsdellite and py
40 to the two-dimensional nature of the layered manganite, and the loss of ferromagnetism is attributed
43 of numerous topological defects in hexagonal manganites are highly relevant to vastly different pheno
45 ll-bounded" topological defects in hexagonal manganites are studied through homotopy group theory and
47 nge, whereas similar magnetic transitions in manganites are tuned by 50-70% chemical substitutions.
48 prates and colossal magnetoresistance in the manganites arise out of a doping-driven competition betw
49 de an atomic-scale basis for descriptions of manganites as mixtures of electronically and structurall
52 he interfacial carrier doping in cuprate and manganite atomic layers, leading to the transition from
53 al study of topological defects in hexagonal manganites based on Landau theory with parameters determ
55 lumns in the room temperature charge-ordered manganite Bi0.35Sr0.18Ca0.47MnO3 using aberration-correc
58 we demonstrate that the orbital domains in a manganite can be oriented by the polarization of a pulse
60 train-induced defects in grain boundaries of manganites deeply impact their functional properties by
61 , but very little change in the shift of the manganite deuterons was observed, consistent with the st
63 of Fe(3)O(4), colossal magnetoresistances in manganites (e.g., La(0.5)Ca(0.5)MnO(3)), and superconduc
64 at the ferromagnetic domain structure of the manganite electrodes is imprinted into the antiferromagn
65 well time; the high spin polarization in the manganite electrodes, which remains high right up to the
68 ous Mn(II), about 18% of the oxygen atoms in manganite exchange with the aqueous phase, which is clos
69 r example, multiferroic hexagonal rare earth manganites exhibit a dense network of boundaries between
70 l involving the Ce(IV) f orbitals.Perovskite manganites exhibit intriguing but poorly understood prop
71 phases of correlated materials: for example, manganites exhibiting colossal magneto-resistance suitab
74 The total charge observed for the insulating manganite films quantitatively agrees with that needed t
78 ght centered at 230 nm produced H(2) gas and manganite (gamma-MnOOH) with an apparent quantum yield o
79 reductive transformation of birnessite into manganite (gamma-MnOOH), whereas at pH 8.0 and 8.5, conv
81 L(-1), respectively) led to the formation of manganite, hausmannite (Mn(II)Mn(III)(2)O(4)), and grout
83 or catalytic action, and numerous studies of manganites have linked electroresistance to electrochemi
84 s that this effect is general to all cuprate/manganite heterostructures and the presence of direct bo
85 e we demonstrate that one type of perovskite manganites, i.e., a (La(2/3)Pr(1/3))(5/8)Ca(3/8)MnO(3) t
87 The ground-state electronic order in doped manganites is frequently associated with a lattice modul
88 phenomenon of colossal magnetoresistance in manganites is generally agreed to be a result of competi
89 to generate interesting functionality in the manganites, is important for the emerging field of DW na
91 ects in epitaxial films of the ferromagnetic manganite La(0.7)Ca(0.3)MnO(3) using strain-mediated fee
93 ges at the interface between a ferromagnetic manganite (La(0.7)Sr(0.3)MnO(3)) and a semimetallic irid
96 re can be stabilized in five-unit-cell-thick manganite layers in superlattices, placing the upper lim
97 ults in a ferromagnetic coupling between the manganite layers that can be controlled by a voltage.
100 rature dependences could be used to identify manganite-like domains within the sample of groutite, wh
101 g-range motion is intrinsic to the hexagonal manganites, linking it to their improper ferroelectricit
103 with water, suggesting that some of the bulk manganite mineral (i.e., beyond surface) is exchanging w
104 e structure showed high Mn in the veins, and manganite [Mn(III)] accumulated in necrotic lesions appa
105 ectrodes, which remains high right up to the manganite-nanotube interface; and the resistance of the
108 cs of antiferromagnetic spin ordering in the manganite Pr(0).(7)Ca(0).(3)MnO(3) following ultrafast p
111 d manipulated at room temperature, hexagonal manganites provide a unique opportunity to explore how t
113 over, the high levels of disorder typical of manganites result in behaviour similar to that of well-k
114 closer inspection of phase diagrams in many manganites reveals complex phases where the two order pa
115 electricity (trimerization) in the hexagonal manganites RMnO3 leads to a network of coupled structura
116 spin-reorientation transitions of hexagonal manganite single crystal and thin films and compare dire
118 hases within the same sample of a perovskite manganite, such as La(1-x-y)Pr(y)Ca(x)MnO3, presents res
119 domain microstructure as those found in the manganites, such as the characteristic six-domain "clove
120 he hysteretic behavior in strained thin film manganites, suggesting close connection between the glas
124 direct observation of structural domains on manganite surfaces, and trace their origin to surface-ch
127 e show for the quasi-two-dimensional bilayer manganites that only the outermost Mn-O bilayer is affec
130 n observed in many colossal magnetoresistive manganites, there is no consensus that they are spin gla
131 ol of the exchange bias (EB) in single-phase manganite thin films with nominallyuniform chemical comp
134 tomic-resolution the charge distribution for manganite-titanate interfaces traversing the metal-insul
137 f the electronic phase of a magnetoresistive manganite via direct excitation of a phonon mode at 71 m
138 and G-AFM states, which is in contrasted to manganites where a similar magnetic phase transition tak
139 ic strain, contrasting with other half-doped manganites, where AF order has no observable effect on t
141 triangular lattice of multiferroic hexagonal manganite YMnO(3) produces a highly unusual thermal Hall