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We suggest that a lower crossover temperature may be required to adequately model regional C4 distribution in the Malagasy Hauts-Plateaux, where average monthly temperatures remain below 21°C year-round yet C4 grasslands spatially comprise a significant portion of basin vegetation cover.
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Many of the floodplains of higher order basins in southern portion of the Basin and Range Province of the American Southwest have been farmed intermittently for hundreds of years, and continuously for the past century.
In the present study, the Rh value of the basin 0.005 shows the major portion of the basin having gentle slope (Table 4).
Although fluids do circulate, flow in the deeper portions of basins tends to be very slow (Toth 1962, 1963), leading to basin-scale travel times that may be millions of years or longer (Kreitler 1989; Hogan et al. 2007).
In the supper-critical condition, a large "flat" subsidence basin bottom appears in the central portion of the basin.
Most of the storms formed either in the Mozambique Channel or in the far eastern portion of the basin, with five storms crossing from the adjacent Australian basin east of 90º E.
In contrast, the results for the eastern sub-basin suggest that vertical leakage rates around the South Australian portion of the Basin margin are low and that more of the vertical leakage component in the eastern sub-basin is occurring distal to the Basin margins.
The Sichuan Basin is a prime petroliferous basin in China, and multiple overpressure systems exist vertically in the central portion of the basin.
As the lake drained, it formed two smaller lakes: Titicaca, in the northern portion of its basin, and Minchin, predecessor to modern Lake Poopó, in the southern basin.
For this study, the portion of the basin which falls within Tanzania, will be referred to as the "basin".
The collision also resulted in southward migration of the basin centre and steepened the bottom topography in the southern portion of the basin.
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