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1 esonant metasurface and a metallic thin-film reflector.
2 plasmonic structures and a distributed Bragg reflector.
3 ary of resonator and the "close" boundary of reflector.
4 lements, such as the all-angle acoustic back reflector.
5 r SOI structures without the use of any back-reflector.
6 in its ability to act as a structural light reflector.
7 tetrafluoroethylene (PTFE) cell as a diffuse reflector.
8 tandard solution and deposited onto a quartz reflector.
9 t spread function (PSF) was assessed off the reflector.
10 oscopy, radar, and frequency scanned antenna reflectors.
11 etic waves (directional emitter) without any reflectors.
12 d in layers, together acting as interference reflectors.
13 ng of ballistic energy carriers by pyramidal reflectors.
14 multimode cavity between two acoustic Bragg reflectors.
15 terference of light with intracellular Bragg reflectors.
16 d photoreceptors are positioned behind these reflectors.
17 vskite transition is too wide to cause sharp reflectors.
18 nside diameter: 5.5 m), reflected by a retro-reflector and recorded using a fast thermoelectrically c
19 ber of seismic observations, such as the D'' reflector and the high degree of seismic anisotropy with
20 h, we introduce an integrated photonic solar reflector and thermal emitter consisting of seven layers
23 ectronic barriers to realize tunable plasmon reflectors and phase retarders in future graphene-based
26 ent densities of 25 mA/cm(2) with a backside reflector, and simulations further show that such stacki
27 eased at the 330-kilometer and 450-kilometer reflectors, and S-wave impedance decreased near 200 kilo
28 this unique synthesis platform include Bragg reflectors, antireflective coatings, and chiral metamate
30 we interpret a negative-polarity sedimentary reflector approximately 500 meters above the subducting
32 ove and below, respectively, reveal multiple reflectors beneath Central America and East Asia, two ar
33 The three-dimensional shape of this micro-reflector can be tuned as a function of time, vapor temp
34 ering nanopost on top of a distributed Bragg reflector, capable of providing a nearly 2pi nonlinear p
37 into the iridocyte to form a potential Bragg reflector consisting of an array of narrow, parallel cha
39 Instead we argue that the seismic layer 2A reflector corresponds to an alteration boundary that can
41 antum dots (QDs) in planar distributed Bragg reflector (DBR) cavity with an average position uncertai
43 Planar microcavities with distributed Bragg reflectors (DBRs) host, besides confined optical modes,
45 ed increased distance between the target and reflector distance of greater than 1.0 cm (range, 1.1-2.
50 bsorbers/emitters for visible light and good reflectors for IR light, which are desirable for efficie
54 i Scout (Cianna Medical, Aliso Viejo, Calif) reflector-guided localization and excision of breast les
55 uch as waveguides, lenses, beamsplitters and reflectors have been implemented by structuring metal su
59 uctive interference from intracellular Bragg reflectors in specialized skin cells called iridocytes.
61 s 45-kilometer depth contour occur below the reflector, in the subducted oceanic mantle, consistent w
65 Here we show that, although the layer 2A reflector is imaged near the top of the sheeted dyke com
66 the formation rate and shapes of these micro-reflectors is presented, along with a ray tracing model
67 ed over young oceanic crust commonly image a reflector known as 'layer 2A', which is typically interp
69 the frequency bandwidth corresponding to the reflector loss at -10 dB was up to 5.8 GHz within the fr
72 ed films, the transition from transmitter to reflector occurs when the sheet resistance is approximat
73 er can serve as a strong frequency-selective reflector of magnetic fields when operating in the near-
74 rating a hybrid conductive distributed Bragg reflector on the back side of the transparent conducting
78 and excision of breast lesions by analyzing reflector placement, localization, and removal, along wi
81 lly consist of four packets of finely spaced reflectors separated by homogeneous interpacket regions
82 peptides are identified in the (+) ion MALDI reflector spectrum by the presence of [MH-H3PO4]+ and [M
84 indicates that this condition obtains for a reflector that is a solid over fluid interface; it is no
87 how strong P-to-S converted reflections from reflectors that are aligned at a depth of approximately
88 wavelength dielectric layer closed by a gold reflector the highest absorptance is attainable at perpe
90 ction respectively as a compact director and reflector, the second harmonic radiation is deflected 90
91 atmospheric pressure ion mobility orthogonal reflector time-of-flight mass spectrometer (IM(tof)MS) t
92 atmospheric pressure ion mobility orthogonal reflector time-of-flight mass spectrometer (IM(tof)MS) t
93 ion mobility spectrometry with an orthogonal reflector time-of-flight mass spectrometer to analyze ch
94 wise internally trapped light and multilayer reflectors to control the direction of light emission.
101 ve, infrared-activated, electromagnetic wave reflectors were percutaneously inserted adjacent to or w
103 e can reconcile seismic observation of a D'' reflector with recent experiments showing that the width
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