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vector<double> storage_for_G; for(unsigned int j = 0; j < EXPERIMENTS; j++) { double A = A0; for(unsigned int i = 0; i < N; i++) { A += AplRandom() * int(b * A / M); if(A <= 0.0) throw ivalid_argument("Account is destroyed!"); } double G = log(A / A0) / N; storage_for_G.push_back(G); }

Table 3.1 Standard k-e model constants (Launder & Spalding 1973). C1 1.44 C2 1.92 C3 1.0 Cm 0.09 sk 1.0 se 1.314 st 0.9

The shape of a foreland basin is controlled by the strength and rheology of the lithosphere A low exural rigidity, which characterizes young, hot and weak lithosphere, results in a narrow, deep basin A high exural rigidity, which characterizes old, cool and strong lithosphere, produces a wide basin with a better-developed forebulge (Flemings & Jordan, 1990; Jordan & Watts, 2005) Variations in the strength and temperature of the lithosphere can thus cause the character of the foreland basin to change along the strike of the orogen Other factors such as inherited stratigraphic and structural inhomogeneities also in uence basin geometry In the Andes, an along-strike segmentation of the foreland partly coincides with variations in these properties and with the segmented geometry of the subducted Nazca plate (Section 1023).

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As a result of lithospheric exure, the sediment thickness in a foreland basin decreases away from the mountain front to a feather edge on the forebulge (Flemings & Jordan, 1990; G mez et al, 2005) Close to the mountain range the sediments are coarse grained and deposited in a shallow water or continental environment; at the feather edge they are ne grained and often turbiditic The sediments thus form a characteristic wedgeshaped sequence in pro le whose stratigraphy re ects the subsidence history of the basin as it grows and migrates outwards during convergence The stratigraphy is thus characterized by units that thin laterally, overstep older members, or may be truncated by erosion Belts of deformed sedimentary rock in which the layers are folded and duplicated by thrust faults are common in foreland basins Like their counterparts in accretionary prisms (Section 97, Fig 9.

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20) and in zones of transpression (Section 82, Fig 88b), foreland fold and.

When a portion of your Web page has been designated as a Library item, yellow highlighting is displayed over the entire item within the Document window. The highlighting helps you to quickly recognize a Library item. If you find the effect distracting, you can disable it. Go to Edit Preferences (Dreamweaver Preferences) and, from the Highlighting panel of the Preferences dialog box, deselect the checkbox to the right of the Library Items color selection. Alternatively, deselecting View Visual Aids Invisible Elements hides Library Item highlighting, along with any other invisible items on your page.

The fourth and nal question is the need for a control strategy to process the rules. Earlier, we observed that the stock selection expert system would reach two con icting recommendations when two facts are asserted:

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know that my tending isn t what she wants She wants her Mama Sometimes when I visit, she will say so: I miss Mama, or I feel as though Mama is here with me sometimes She yearns for her mother, but with great determination she continues to mother me as I cope with my Parkinson s And so the cycle continues Putting my mother, myself, and my children into perspective is important as I try to understand what is happening between me and my children since Parkinson s entered our lives When I think about my mother s role in my life, I can begin to understand my children as they adjust to the invasion of an incurable disease into my life This chapter centers around my children, Susan and Randy, and their spouses, and how they have adjusted to their mother having Parkinson s disease.

Moho Fast-spreading ridge Volcanics/basalt Dikes Gabbro Ultramafic/peridotite Lower crust Melt lens Crystal mush zone (partially molten) Transition zone (largely solid)

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