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  <channel rdf:about="https://www.um.edu.mt/library/oar/handle/123456789/403">
    <title>OAR@UM Community:</title>
    <link>https://www.um.edu.mt/library/oar/handle/123456789/403</link>
    <description />
    <items>
      <rdf:Seq>
        <rdf:li rdf:resource="https://www.um.edu.mt/library/oar/handle/123456789/148652" />
        <rdf:li rdf:resource="https://www.um.edu.mt/library/oar/handle/123456789/148598" />
        <rdf:li rdf:resource="https://www.um.edu.mt/library/oar/handle/123456789/148524" />
        <rdf:li rdf:resource="https://www.um.edu.mt/library/oar/handle/123456789/148517" />
      </rdf:Seq>
    </items>
    <dc:date>2026-08-25T10:56:13Z</dc:date>
  </channel>
  <item rdf:about="https://www.um.edu.mt/library/oar/handle/123456789/148652">
    <title>Seismic anisotropy indicates organized melt beneath the Mid-Atlantic Ridge aids seafloor spreading</title>
    <link>https://www.um.edu.mt/library/oar/handle/123456789/148652</link>
    <description>Title: Seismic anisotropy indicates organized melt beneath the Mid-Atlantic Ridge aids seafloor spreading
Authors: Kendall, J. M.; Schlaphorst, D.; Rychert, C. A.; Harmon, N.; Agius, Matthew; Tharimena, S.
Abstract: Lithospheric plates diverge at mid-ocean ridges and asthenospheric mantle material rises&#xD;
in response. The rising material decompresses, which can result in partial melting, potentially&#xD;
impacting the driving forces of the system. Yet the geometry and spatial distribution of the&#xD;
melt as it migrates to the ridge axis are debated. Organized melt fabrics can cause strong&#xD;
seismic anisotropy, which can be diagnostic of melt, although this is typically not found at&#xD;
ridges. We present anisotropic constraints from an array of 39 ocean-bottom seismometers&#xD;
deployed on 0–80 Ma lithosphere from March 2016 to March 2017 near the equatorial Mid-&#xD;
Atlantic Ridge (MAR). Local and SKS measurements show anisotropic fast directions away&#xD;
from the ridge axis, which are consistent with strain and associated fabric caused by plate&#xD;
motions with short delay times, δt (&lt;1.1 s). Near the ridge axis, we find several ridge-parallel&#xD;
fast splitting directions, φ, with SKS δt that are much longer (1.7–3.8 s). This is best explained&#xD;
by ridge-parallel sub-vertical orientations of sheet-like melt pockets. This observation is much&#xD;
different than anisotropic patterns observed at other ridges, which typically reflect fabric&#xD;
related to plate motions. One possibility is that thicker sub-ridge lithosphere with steep subridge&#xD;
topography beneath slower spreading centers focuses melt into vertical, ridge-parallel&#xD;
melt bands, which effectively weakens the plate. Associated buoyancy forces elevate the subridge&#xD;
plate, providing greater potential energy and enhancing the driving forces of the plates.</description>
    <dc:date>2023-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="https://www.um.edu.mt/library/oar/handle/123456789/148598">
    <title>Deterministic quantum computation with one-clean-qubit model as an open quantum system</title>
    <link>https://www.um.edu.mt/library/oar/handle/123456789/148598</link>
    <description>Title: Deterministic quantum computation with one-clean-qubit model as an open quantum system
Authors: Xuereb, Jake; Campbell, Steve; Goold, John; Xuereb, Andre
Abstract: The deterministic quantum computation with one-clean-qubit model (DQC1) complexity class, or power-ofone&#xD;
qubit model, is examined as an open quantum system.We study the dynamics of a register of qubits carrying&#xD;
out a DQC1 algorithm and show that, for any algorithm in the complexity class, the evolution of the logical qubit&#xD;
can be described as an open quantum system undergoing a dynamics which is unital. Unital quantum channels&#xD;
respect the Tasaki-Crooks fluctuation theorem, and we demonstrate how this is captured by the thermodynamics&#xD;
of the logical qubit. As an application, we investigate the equilibrium and nonequilibrium thermodynamics of&#xD;
the DQC1 trace estimation algorithm. We show that different computational inputs, i.e., different traces being&#xD;
estimated, lead to different energetic exchanges across the register of qubits and that the temperature of the&#xD;
logical qubit impacts the magnitude of fluctuations experienced and quality of the algorithm.</description>
    <dc:date>2023-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="https://www.um.edu.mt/library/oar/handle/123456789/148524">
    <title>Time-dependent horizontal-to-vertical spectral ratio (HVSR) analysis of ambient seismic noise</title>
    <link>https://www.um.edu.mt/library/oar/handle/123456789/148524</link>
    <description>Title: Time-dependent horizontal-to-vertical spectral ratio (HVSR) analysis of ambient seismic noise
Abstract: Existing local research has employed the horizontal-to-vertical spectral ratio (HVSR) for &#xD;
static microzonation and long-term groundwater monitoring. Building on this work, this &#xD;
thesis provides the first high-resolution quantification of how sub-daily meteorological &#xD;
fluctuations, specifically wind-driven noise and atmospheric variables, directly modulate &#xD;
seismic site response parameters across the stations of the Malta Seismic Network in the &#xD;
Maltese archipelago. By establishing these correlations, this study enhances &#xD;
the methodological accuracy of HVSR in the Maltese context, providing a framework to &#xD;
isolate meteorological noise from geological signals and enabling more reliable site&#xD;
response assessments for local engineering and microzonation projects. &#xD;
This study analyses four years (2017-2020) of continuous seismic data recorded by the &#xD;
Malta Seismic Network to investigate temporal variability in HVSR parameters. The &#xD;
research evaluates how HVSR peak frequency and amplitude evolve and examines the &#xD;
potential influence of meteorological variables, including wind speed, precipitation, &#xD;
temperature, and relative humidity. Statistical analysis is used to identify stations that &#xD;
exhibit sensitivity to environmental forcing and to assess the extent to which such factors &#xD;
may influence the stability and interpretation of HVSR measurements in the Maltese &#xD;
Islands. Forward modelling was also used to confirm whether the observed &#xD;
meteorological effects can potentially create subsurface parameter changes, such as &#xD;
variations in soil moisture or density, which could affect the HVSR measurements. &#xD;
This thesis further confirms that HVSR parameters are sensitive to wind strength and &#xD;
reveals that two stations (MELT and CBH9) have a heightened sensitivity to wind speed &#xD;
compared to other stations within the Malta Seismic Network. Hence, caution should be &#xD;
exercised when analysing data from these stations during windy days. Association &#xD;
between HVSR and other meteorological parameters, including precipitation, revealed &#xD;
weak effect sizes, indicating that other short-term meteorological forcing is not registered &#xD;
by HVSR.
Description: B.Sc. (Hons)(Melit.)</description>
    <dc:date>2026-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="https://www.um.edu.mt/library/oar/handle/123456789/148517">
    <title>The variability of Heteracris adspersa (Redtenbacher, 1889) re-examined (Orthoptera : Acrididae, Eyprepocnemidinae)</title>
    <link>https://www.um.edu.mt/library/oar/handle/123456789/148517</link>
    <description>Title: The variability of Heteracris adspersa (Redtenbacher, 1889) re-examined (Orthoptera : Acrididae, Eyprepocnemidinae)
Authors: Cassar, Louis F.; Lanfranco, Sandro; Massa, Bruno
Abstract: A new subspecies of Heteracris adspersa was described in 1978 on the basis of morphometrics and structure configuration of the male&#xD;
subgenital plate from specimens collected in Sardinia. The present study examines specimens (n=175) from a broad suite of localities, &#xD;
ranging from the Middle East across to the western Mediterranean. Statistical analyses are subsequently carried out on a revised dataset &#xD;
comprising 94♂♂ and 55♀♀. Microscopic examination of the subgenital plate is also conducted on specimens from Sardinia, Sicily, &#xD;
Malta and Yemen and compared with those published in the original description. Findings demonstrate that the subspecies massai is practically an artefact of unintended consequence, essentially a case of taxonomic inflation, in view of evident intra and interpopulation&#xD;
variability across a wide geographic area; consequently, H. a. massai is synonymised.</description>
    <dc:date>2026-01-01T00:00:00Z</dc:date>
  </item>
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