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Oracle has another enhanced mandatory access control security solution called Oracle Label Security (OLS). The OLS feature is implemented by using VPDs to support a complex row-level model of access control. Oracle s current version of label security differs from conventional mandatory access control in some details. Labels have structure, with each label containing three fields. These components are the label s level, compartment, and group. Level. Levels are organized in hierarchies and typically have the semantics of military sensitivity of information levels, such as Public, Proprietary, Restricted, Secret, Top Secret, and so on. Compartment. The compartments within a level correspond to categories of information. Categories are peer containers and are not organized into hierarchies within levels or across levels. They enable data restriction based on context or business logic. Users with access to a certain level can only access their own categories within that level. Compartments support the need to know policy features described in 3. Users are assigned Read and Write compartments. When the user accesses a row on a read or write, the user s compartment definition is compared to the row s compartment definitions. A data element can belong to multiple compartments. Group. The third component of the label defines ownership. Ownership definitions can be hierarchical. This third component is unusual in that it allows the definition of additional discretionary access control mechanisms over and above those already passed at the SYSTEM and OBJECT levels. Labels can be composed of a standalone level component, a level and associated compartment, or all three components. Groups represent an additional degree of freedom in security policy definition. We recommend that they should be used with care, because incorrect configuration could contradict prior policy decisions.

Cascading Style Sheets offer another method for indenting the first line of a paragraph. You can set an existing HTML tag, such as <p>, to any indent amount using the Text Indent option found on the Block panel of the Style Sheet dialog box. You can find a full discussion of text indent and other style sheet controls in 7.

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(1996) Paleomagnetic evidence of an early Paleozoic rotated terrane in Northwest Argentina; a clue for Gondwana Laurentia interaction Geology 24, 953 6 Cook, FA (2002) Fine structure of the continental re ection Moho Bull geol Soc Am, 114, 64 79 Cook, FA et al (1992) Lithoprobe crustal re ection cross-section of the southern Canadian Cordillera I: foreland thrust and fold belt to Fraser River fault Tectonics 11, 12 35 Cook, FA et al (1999) Frozen subduction in Canada s Northwest Territories: Lithoprobe deep lithospheric re ection pro ling of the western Canadian Shield Tectonics 18, 1 24 Cook, FA et al (2004) Precambrian crust beneath the Mesozoic northern Canadian Cordillera discovered by Lithoprobe seismic re ection pro ling Tectonics 23, doi:101029/ 2002TC001412 Cooper, AK et al (1992) Evidence for Cenozoic crustal extension in the Bering Sea region Tectonics 11, 719 31 Corliss, J.

sinking of these regions preserves the organic layers by progressive burial. The process of coali cation refers to the physical and chemical changes experienced by the organic matter after burial in response to rising temperature and pressure. On compression, water and volatiles are expelled and the deposit becomes enriched in carbon. The degree of coali cation is re ected in coal of different ranks, varying from the low rank lignite to high rank anthracite. Plate tectonics affects coal formation in that it controls the latitude of a region (Section 3.4) and creates the environments necessary for the preservation of organic matter, of which the most important are passive continental margins (Section 7.7). Deltas formed on such margins produce the most favorable conditions for coal formation, and swamps can develop on a regional scale. Present day examples include the Niger, Amazon, and Mississippi deltas, and ancient examples the Carboniferous coals of North America and northwest Europe. Intracratonic deltas, such as the Rhine, are similarly productive and are likely to be preserved due to their stable surroundings. Coal deposits are also found in aulacogens and ensialic backarc basins. The tectonism associated with collisional orogens provides an environment whereby coals increase in grade by high-pressure metamorphism.

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