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The growth of these secondary deposits is often slow, and they may not be apparent until many years after the diagnosis of the tumour in the eye.
The explicit identification of paleotsunami deposits is often difficult mainly because the tsunami deposits may be represented by various sediment types and may be similar to other deposits, such as storm deposits (Morton et al., 2007; Switzer and Jones, 2008).
However, the ability to detect secondary deposits is often poor.
This study highlights an important limitation of PET imaging in that the metabolic activity of small tumour deposits is often not sufficient for positive identification, particularly in areas with higher background activity such as in the abdomen and pelvis.
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The common lack of consolidation of volcaniclastic deposits means that, post-deposition, deposits are often thinned or removed by grainsize-dependent erosional processes, with anomalously thick deposits forming in topographic lows.
Deposits are often required, especially for large jobs.
The amount is huge, given that interest rates on deposits are often at least three percentage points lower than they were four years ago — and are now near zero on many bank and money market accounts.
However, unambiguous interpretations of isotope signatures in natural silica deposits are often hampered by a lack of independent quantitative information on isotopic fractionations operating under the environmental conditions of interest.
It has been reported that leaf-like dendrite deposits are often the origin of cell-failure, however, their nature and behavior on discharge (oxidation) - charge (reduction) cycling have been only poorly understood.
In contrast deposits at Bankia, a bailed-out Spanish bank, have fallen by more than a quarter over the past 18 months.A loss of deposits drives up banks' funding costs, since deposits are often cheaper than borrowing on capital markets; it also increases their loan-to-deposit ratio, a marker of vulnerability to droughts in wholesale markets.
The wind-blown depositional process of loess formation yields a relatively loose soil structure that is particularly sensitive to changes in hydro-mechanical loading conditions, and the silt particles that comprise loess deposits are often easily eroded by water or wind.
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