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Audiological assessment in the newborn is carried out mainly by using objective measures, although objective tests of hearing can be used on a child of any age. These include tympanometry to help diagnose middle ear effusions (OME), transient evoked or distortion product otoacoustic emissions (TEOAE or DPOAE) to record the outer hair cell activity when the middle ear is clear of OME, and Auditory Brainstem Evoked Response Audiometry to determine the threshold of hearing under natural sleep. TYMPANOMETRY (ACOUSTIC IMPEDANCE TEST) Tympanometry (acoustic impedance test) is a simple test that involves placing a probe in the ear canal and gives a measure of middle ear compliance and pressure. A high frequency probe tone is used in babies up to about 4 months of age, compared to a 256 Hz probe tone used in older children. A at graph (Figure 17.1) indicates presence of an effusion in the middle ear or OME. OTOACOUSTIC EMISSIONS (OAES) Otoacoustic emissions (OAEs) are tiny sounds generated by the outer hair cells, when external sounds reach the inner ear. A proportion of these generated sounds leak back through the middle ear and are recorded by a probe placed in the ear canal and displayed on a screen. The cochlea is fully developed by about 32 weeks of gestation and the presence of transient evoked otoacoustic emissions (TEOAEs) suggests intact outer hair cells. Over 99% of these babies with TEOAEs have normal hearing although a small number, especially those who have had perinatal problems such as hypoxia and jaundice (less than 1%), may still have a sensori-neural hearing loss, e.g. auditory neuropathy. In these babies, a full audiological assessment is essential to detect the degree and nature of hearing loss.

In modeling the golf club program, we need only be concerned with the player threads and the allocator monitor that embody the concurrent behavior of the go club. We can abstract away from the details of how the program s display inter-

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formed in less than 3 Ma and the Kerguelen Plateau in 45 Ma Most of the volcanic activity occurred in short, violent episodes separated by long periods of relative quiescence Estimates of the average rates of formation, which include the periods of quiescence, are 12 18 km3 a 1 for the Ontong Java Plateau and 2 8 km3 a 1 for the Deccan Traps Ontong Java s rate of emplacement may have exceeded the contemporaneous global production rate of the entire mid-ocean ridge system (Cof n & Eldholm, 1994) The outpouring of large volumes of ma c magma in such short periods of time requires a mantle source This characteristic has encouraged interpretations involving deep mantle plumes (Sections 55, 1210), although the existence and importance of these features are debated widely (Anderson & Natland, 2005).

9/21/05

With XML, each section of the page is given its own set of tags, according to its meaning, as follows:

Solving for y, we finally have (1 cx)y 2x(1 cx) cx, y 2x 1 1/(1 cx).

Mantle plumes may form large oceanic plateaux and some continental ood basalts also may be attributed to them Beneath the Ethiopian Plateau and the Kenya Dome (in the East African Plateau), extensive volcanism and topographic uplift appear to be the consequences of anomalously hot asthenosphere (Venkataraman et al, 2004) The isotopic characteristics of the volcanic rock and the large volume of ma c lava erupted over a short period of time (Hofmann et al, 1997; Ebinger & Sleep, 1998) suggest that a plume or plumes below the uplifts tap deep undegassed mantle sources (Marty et al, 1996; Furman et al, 2004) As the deep plumes ascend they undergo decompression melting with the amount of melt depending on the ambient pressure (Section 742) Consequently, less melting is expected under thick continental lithosphere than under thick oceanic lithosphere.

Frequency ( % )

Border Setting Top Right Bottom Left Style Description Sets the color and settings for a border along the top of an element. Sets the color and settings for a border along the right side of an element. Sets the color and settings for a border along the bottom of an element. Sets the color and settings for a border along the left side of an element. Sets the style of the border. You can use any of the following as a border: Dotted, Dashed, Solid, Double, Groove, Ridge, Inset, and Outset.

You ll also need about 12 6 of 1/4 -thick foam spacer material. This can be anything somewhat stiff; for my portable, I used X-Acto Foam Board from the stationery section of WalMart (look near the pens and tag board). It s cheap, easy to cut, and comes in 20 30 sheets for a couple of bucks.

where the factor .Zt-8 sets the sign of the likelihood ratio and the sum of the errors represents the accumulation of evidence. By (A.4) and (14.58), this sum is over only those indices I where .Zt-s # 2 - . Using :8 (14.58) we can write (14.59) as