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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Geophysical prospecting 49 (2001), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Azimuthal anisotropy in rocks can result from the presence of one or more sets of partially aligned fractures with orientations determined by the stress history of the rock. The symmetry of a rock with horizontal bedding that contains two or more non-orthogonal sets of vertical fractures may be approximated as monoclinic with a horizontal plane of mirror symmetry. For offsets that are small compared with the depth of the reflector, the azimuthal variation in P-wave AVO gradient for such a medium varies with azimuth as 〈inlineGraphic alt="inline image" href="urn:x-wiley:00168025:GPR236:GPR_236_mu1" location="equation/GPR_236_mu1.gif"/〉 where φ is the azimuth measured with respect to the fast polarization direction for a vertically polarized shear wave. φ2 depends on both the normal compliance BN and the shear compliance BT of the fractures and may differ from zero if BNBT varies significantly between fracture sets. If BNBT is the same for all fractures, 〈inlineGraphic alt="inline image" href="urn:x-wiley:00168025:GPR236:GPR_236_mu2" location="equation/GPR_236_mu2.gif"/〉 and the principal axes of the azimuthal variation in P-wave AVO for fixed offset are determined by the polarization directions of a vertically propagating shear wave. At larger offsets, terms in 〈inlineGraphic alt="inline image" href="urn:x-wiley:00168025:GPR236:GPR_236_mu3" location="equation/GPR_236_mu3.gif"/〉 and 〈inlineGraphic alt="inline image" href="urn:x-wiley:00168025:GPR236:GPR_236_mu4" location="equation/GPR_236_mu4.gif"/〉 are required to describe the azimuthal variation in AVO accurately. φ4 and φ6 also depend on BNBT. For gas-filled open fractures 〈inlineGraphic alt="inline image" href="urn:x-wiley:00168025:GPR236:GPR_236_mu5" location="equation/GPR_236_mu5.gif"/〉 but a lower value of BNBT may result from the presence of a fluid with non-zero bulk modulus.
    Type of Medium: Electronic Resource
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  • 2
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    Unknown
    National Oceanography Centre
    In:  EPIC3Southampton, National Oceanography Centre
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/pdf
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Dean, Simon M (2004): Analysis of NGR spectra from deep-sea sediments in the Philippine Sea, Site 1201. In: Shinohara, M; Salisbury, MH; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 195, 1-33, https://doi.org/10.2973/odp.proc.sr.195.105.2004
    Publication Date: 2024-01-09
    Description: Natural gamma ray measurements are made routinely during core logging using the physical property multisensor track. The instrument provides a measure of the natural decay of radioactive elements in the core, expressed in counts per second, which is generally used as a proxy for the clay content of nonmarginal marine sediments. At Site 1201 spikes of increased gamma ray emissions, up to six times the average for the entire core over depth intervals on the order of 20-50 cm, are observed from the sediments within 50 m of the basement contact. The spikes show a strong correlation with sediment color variations, coinciding with red/brown layers within otherwise green/gray-colored sediments. In this paper, the gamma ray spectra obtained from 21 measurements using a 4-hr counting period are analyzed to obtain the absolute concentration of the radioactive elements K2O, U, and Th in both the intervals with spikes and the intervals with relatively low count rates. In addition, the concentration of these elements is estimated using the spectra obtained from the routine 20-s counting period measurements and which, although exhibiting a great deal of scatter due to the high statistical uncertainty in the original measurements, are roughly similar to those obtained from the 4-hr counting period. Baseline concentrations for U (1 ppm) and Th (5 ppm) match published averages for the amount present in deep-sea clays; the peak concentrations measured correspond to an additional concentration of 100%-200%. The results are compared to those from downhole logging and shipboard inductively coupled plasma-atomic emission spectrometry measurements. The gamma ray spectra results do not support postdepositional fluid flow through the sediment as the source of the enrichment of radioactive elements. It is more likely that the spikes in the gamma ray emissions are simply the result of interbedding sediments from two different sources, one with relatively high concentrations of K2O, U, and Th.
    Keywords: 195-1201; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg195; Natural gamma-ray spectroscopy tool (NGT); Ocean Drilling Program; ODP; Philippine Sea; Potassium oxide; Thorium; Uranium
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 4
    Publication Date: 2017-06-20
    Description: We present a detailed 3-D P-wave velocity model obtained by first-arrival travel-time tomography with seismic refraction data in the segment boundary of the Sumatra subduction zone across Simeulue Island, and an image of the top of the subducted oceanic crust extracted from depth-migrated multi-channel seismic reflection profiles. We have picked P-wave first arrivals of the air-gun source seismic data recorded by local networks of ocean-bottom seismometers, and inverted the travel-times for a 3-D velocity model of the subduction zone. This velocity model shows an anomalous zone of intermediate velocities between those of oceanic crust and mantle that is associated with raised topography on the top of the oceanic crust. We interpret this feature as a thickened crustal zone in the subducting plate with compositional and topographic variations, providing a primary control on the upper plate structure and on the segmentation of the 2004 and 2005 earthquake ruptures.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2011-04-22
    Description: Environmental Science & Technology DOI: 10.1021/es2001997
    Print ISSN: 0013-936X
    Electronic ISSN: 1520-5851
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
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  • 6
    Publication Date: 2015-07-31
    Description: Background: This paper explores the nature and reasoning for (dis)trust in Australian public and private hospitals. Patient trust increases uptake of, engagement with and optimal outcomes from healthcare services and is therefore central to health practice, policy and planning. Methods: A qualitative study in South Australia, including 36 in-depth interviews (18 from public and 18 from private hospitals). Results: ‘Private patients’ made active choices about both their hospital and doctor, playing the role of the ‘consumer’, where trust and choice went hand in hand. The reputation of the doctor and hospital were key drivers of trust, under the assumption that a better reputation equates with higher quality care. However, making a choice to trust a doctor led to personal responsibility and the additional requirement for self-trust. ‘Public patients’ described having no choice in their hospital or doctor. They recognised ‘problems’ in the public healthcare system but accepted and even excused these as ‘part of the system’. In order to justify their trust, they argued that doctors in public hospitals tried to do their best in difficult circumstances, thereby deserving of trust. This ‘resigned trust’ may stem from a lack of alternatives for free health care and thus a dependence on the system. Conclusion: These two contrasting models of trust within the same locality point to the way different configurations of healthcare systems, hospital experiences, insurance coverage and related forms of ‘choice’ combine to shape different formats of trust, as patients act to manage their vulnerability within these contexts.
    Electronic ISSN: 1472-6963
    Topics: Medicine
    Published by BioMed Central
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