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In the creation of petroleum, source rocks are buried by natural geologic processes and, over geologic time, converts the organic materials to liquids and gases that can migrate through cracks and pores in the rocks until it reaches the surface or is trapped by a tight overhead formation. The result is an oil and/or gas reservoir. Oil shale was deposited in a wide variety of environments including freshwater to saline ponds and lakes, epicontinental marine basins, and related subtidal shelves. They were also deposited in shallow ponds or lakes associated with coal-forming peat in limnic and coastal swamp depositional environments. It is not surprising, therefore, that oil shale exhibit a wide range in organic and mineral composition. Most oil shale contain organic matter derived from varied types of marine and lacustrine algae, with some debris of land plants, depending upon the depositional environment and sediment sources. Oil shale does not undergo that natural maturation process but produces the material that has come to be known as kerogen (Scouten, 1990). In fact, there are indications that kerogen, being different to petroleum, may be a by-product of the maturation process. The kerogen residue that remains in oil shale is formed during maturation and is then rejected from the organic matrix because of its insolubility and relative unreactivity under the maturation conditions (Speight, 2007; Chap. 4). Furthermore, the fact that kerogen, under the conditions imposed upon it in the laboratory by high-temperature pyrolysis, forms hydrocarbon products does not guarantee that the kerogen of oil shale is a precursor to petroleum. Oil shale ranging from Cambrian to Tertiary in age occurs in many parts of the world (Table 6.2). Deposits range from small occurrences of little or no economic value to those

Figure 5-2.

-- read din value read(l, tmpdin, good_val); assert good_val REPORT bad din value ; read(l, space); --- skip a space

SP2 makes significant changes in Windows XP to improve the overall security of the operating system. The changes are in four basic areas:

Predict the possible products by combining the cation of one reactant with the anion of the other and vice versa: PbI2 + NaNO3 Apply the solubility rules to the two possible products: PbI2(s) NaNO3(aq) Insoluble, therefore a precipitate will form. Soluble, no precipitate will form.

System.exit(0);

System.out.println("Cannot create URL for: " + filename);

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Description At least one item from this group must start before this service is loaded. The subkey SYSTEM\CurrentControlSet\Control\ServiceGroupOrder contains the service group load order. Lists the specific services that must load before this service loads. Describes the component. Specifies the display name of the component. Controls whether a driver error requires the system to use the LastKnownGood control set or to display a Stop message.

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Windows Support Tools help you deploy Windows XP Professional, manage your network, and troubleshoot problems. You can find Windows Support Tools in the \Support\Tools folder on your operating system CD. The folder also includes two cabinet files, Deploy.cab and Support.cab, which contain numerous tools in compressed form. For information about

When you move a dynamic disk to a computer that has no dynamic disks, the dynamic disk retains its disk group name and ID from the original computer and uses them on the local computer. For more information about disk groups, see article 222189, Description of Disk Groups in Windows 2000 Disk Management, in the Microsoft Knowledge Base. To find this article, see the Microsoft Knowledge Base link on the Web Resources page at http://www.microsoft.com /windows/reskits/webresources. For more information about converting basic disks to dynamic, including the limitations of dynamic disks, see Converting Basic Disks to Dynamic Disks later in this chapter.

public boolean mouseEnter(Event e, int x, int y){

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