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This requires the establishment of distal limits for the integral that represent the proximal and distal limit of the deposit (Table 1).
Standard methods of estimating tephra volume are based on assumptions about the decay of deposit thickness with distance away from a source and knowledge of the isopach areas produced by the deposit (Table 1).
The samples from sand deposit (Table 1) do not have as much shell debris as the beach samples; however, within the sampled deposits from the tsunami layers several Globigerina sp., sea-urchin radiols, Elphidium crispum, Nonion boueanum; Bulimina; Orbulina universa sp., as well as a some individual Sphaeroidinellopsis sp. were found.
A concordant pair of dates was also obtained using enamel and bone from a cattle mandible (Bos taurus, GF10), which was found deflated on the surface of the paleolake deposit (Table 6, dates 9, 10).
Five radiocarbon dates from bone and charcoal within Graves I and VIII as well as an overlying midden deposit (Table 1) bracket use of the site between 17,250 16,350 cal BP and 15,000 14,200 cal BP (95% confidence intervals, using BCal software [20]).
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The following factors were significant predictors of non-SN metastases by univariate analysis: primary tumor size, number of involved SNs, ECE, AJCC classification, diameter, and penetrative depth of the SN metastatic deposit (Tables 3 and 4).
Class 6 lesions showed advanced glomerular amyloid deposition (>76% of tuft involved by amyloid deposits) (Table 1).> -wrap-foot> Class dependent on % of tuft and glomerular compartment involved.
The features of the E3 deposits (Table 3) suggest a large, very energetic tsunami.
Furthermore, we analyzed the major element compositions of the volcanic glass shards above the E4 deposits (Table 5).
The solid deposits studied were dark brown semi-solid materials, characterized by high melting point, and for this reason, they were classified as wax deposits (Table 1).
All the elements found correspond to the chemical composition of the identified minerals, including trace elements that may be useful for identification of mineral deposits (Table 1).
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