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The ribbon cable attached between the LCD glass and the screen s motherboard may not be reinstalled into its jack correctly, or may have come loose during assembly. Dismantle the screen assembly and check. Check that you ve connected the audio and video wires between the PSOne and the screen correctly. Again, on some models these switch around, so you can try swapping them as well. Check the seventeen connections between both halves of the TV. Did one break loose, or is one touching another If the brightness dial is turned all the way up, the screen will go completely white regardless of the picture. Spin the dial down and check if that s the problem here. An incorrectly rewired brightness dial cable can also cause the picture to disappear, so check it as well. Check the volume dial s ribbon cable. If even a few of the wires come loose, it can cause the sound to not work. Be sure the headphone jack has been properly rewired as explained in 4. If it isn t, the sound won t work, since it passes through this jack before going to the speaker. Check the audio connection between the PSOne and the TV.

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Eastern branch of the East African Rift system to depths of 500 km They found a steep-sided, west-dipping low velocity anomaly that is similar to the one modeled by Davis & Slack (2002) above 160 km depth Below this depth, the anomaly broadens to the west indicating a westerly dip Similar structures have been imaged below Tanzania (Ritsema et al, 1998; Weeraratne et al, 2003) and parts of Ethiopia (Benoit et al, 2006) Bastow et al (2005) found that a tabular (75 km wide) low velocity zone below southern Ethiopia broadens at depths of >100 km beneath the more highly extended northern section of the rift (Fig 77c,d) The anomalies are most pronounced at 150 km depth These broad, dipping structures are dif cult to reconcile with models of a simple plume with a well-de ned head and tail.

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I m going to bend the rules and go a bit beyond 10 tags by also introducing you to two related tags: To make text bold, wrap it in <b> tags; to make it italicized, wrap it in <i> tags. With the addition of <font>, <b>, and <i> tags, our example page now looks as follows:

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Instead they appear to be more consistent with either multiple plumes or tomographic models (Plate 73 between pp 244 and 245) where the hot asthenosphere connects to a broad zone of anomalously hot mantle beneath southern Africa In the deep mantle below South Africa, Ritsema et al (1999) imaged a broad (4000 by 2000 km2 area) low velocity zone extending upward from the core mantle boundary and showed that it may have physical links to the low velocity zones in the upper mantle beneath East Africa (Plate 73 between pp 244 and 245) The tilt of the deep velocity anomaly shows that the upwelling is not vertical Between 670 and 1000 km depth the anomaly weakens, suggesting that it may be obstructed.

Excel lets you combine two or more objects into a single object. This feature is known as grouping. For example, if you create a design that uses four separate AutoShapes, you can combine them into a group. Then you can manipulate this group as a single object (move it, resize it, and so on). To group two or more objects, select all the objects and then right-click. Choose Grouping Group from the shortcut menu. Later, if you need to modify one of the objects in the group, you can ungroup them by right-clicking and selecting Grouping Ungroup from the shortcut menu. This command breaks the object into its original components.

These observations support the idea that anomalously hot asthenosphere beneath Africa is related in some way to this broad deep zone of upwelling known as the African superswell (Section 1283) Nevertheless, a consensus on the location, depth extent and continuity of hot mantle material below the East African Rift system has yet to be reached (cf Montelli et al, 2004a) A comparison of the mantle structure beneath rifts in different settings indicates that the size and strength of mantle upwellings are highly variable Achauer & Masson (2002) showed that in relatively cool rifts, such as the Baikal Rift and the southern Rhine Graben, low velocity zones are only weakly negative ( 25% relative to normal mantle P-wave velocities) and occur mostly above depths of 160 km.

When saturated hydrocarbons are treated with metal catalysts in the presence of hydrogen, carbon-carbon 0' bonds are cleaved, with the concomitant formation of new carbon-hydrogen bonds called hydrogenolysis, Hydrogenolysis is not identical with hydrocracking, The latter is the very complex refinery operation that is used to convert high-molecular-weight hydrocarbons to lower-boiling products (see Section 2.1), In the hydrocracking process bifunctional catalysts consisting of a hydrogenation-dehydrogenation component (a metal) and an acidic component are employed and most cracking takes place on the acidic sites, In the present

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