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  • 1
    Publication Date: 2015-05-05
    Description: Silicon nanocrystals formed in the annealed SiN x /Si 3 N 4 superlattices are attractive for research due to the smaller band offsets of Si 3 N 4 matrix to Si in comparison with commonly used SiO x /SiO 2 superlattices. However, the annealed SiN x /Si 3 N 4 structures contain an increased number of nanocrystal interface defects, which completely suppress nanocrystal emission spectrum. In this work, we study a novel SiO x N y /Si 3 N 4 hetero multilayer combination, which compromises the major issues of SiO x /SiO 2 and SiN x /Si 3 N 4 superlattices. The annealed SiO x N y /Si 3 N 4 superlattices are investigated by TEM, demonstrating a precise sublayer thicknesses control. The PL spectra of the annealed SiO x N y /Si 3 N 4 superlattices are centered at 845–950 nm with an expected PL peak shift for silicon nanocrystals of different sizes albeit the PL intensity is drastically reduced as compared to SiO 2 separation barriers. The comparison of PL spectra of annealed SiO x N y /Si 3 N 4 superlattice with those of SiO x N y /SiO 2 superlattice enables the analysis of the interface quality of silicon nanocrystals. Using the literature data, the number of the interface defects and their distribution on the nanocrystal facets are estimated. Finally, it is shown that the increase of the Si 3 N 4 barrier thickness leads to the increased energy transfer from the Si nanocrystals into the Si 3 N 4 matrix, which explains an additional drop of the nanocrystal PL intensity.
    Print ISSN: 0021-8979
    Electronic ISSN: 1089-7550
    Topics: Physics
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  • 2
    Publication Date: 2019-07-16
    Description: The continental margin of Mozambique formed during the initial dispersal of Gondwana about 180 Ma. Due to the lack of deep seismic and dense potential field data, many details of the timing and geometry of the early breakup in this region remained unknown to date. To close this gap, a research project (MoBaMaSis (“Mozambique Basin Marine Seismic Survey”) with the French research vessel R/V Marion Dufresne II was conducted in 2007. This paper presents the results of P-wave, magnetic and 2D-gravity modelling along two parallel seismic refraction profiles between 37° and 41° E, crossing the Mozambique rifted margin. The crust shows the characteristics of normal to slightly thickened oceanic crust. A lower crustal highvelocity- body with P-wave-velocities of 7.0–7.5 km/s is observed along both profiles. Its origin is discussed in the context of upper mantle convection and thermal properties. The existing magnetic anomaly identifications have been extended to older ages. We postulate that the oldest oceanic crust near the Central Mozambique continental margin has been formed around M41n (166 Ma). Closer to the coast a pronounced negative magnetic anomaly exists that we interpret to coincide with the continent–ocean-transition. This implies that the position of the continent–ocean-transition is located significantly closer to the shoreline than proposed before.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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