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It consists of six gravely terraces located below the culminant (Pliocene) basin unit.
To estimate initial losses over sub-basins, transmission losses through channel routing, and downstream runoff, we developed an integrated model combining spatial rainfall distribution, an appropriate basin unit hydrograph, and appropriate infiltration parameters.
Sand-prone architectural elements identified in this work include: a) axial canyons incising a salt-withdrawal basin (Unit 1), b) turbidite lobes intercalated with heterogeneous mass-transport deposits (Unit 2), and c) channel complexes confined by salt-controlled topography (Unit 3).
Using watershed as a basin unit in morphometric analysis is the most logical choice because all hydrological and geomorphic processes occur within the watershed.
When the basin unit hydrograph was derived, the design flood hydrograph was calculated based on excess rainfall duration and design rainfall hyetograph.
Open image in new window Fig. 5 Gas release strength in the uplift period of the Upper Paleozoic, Ordos Basin (unit: ×108 m3/km2) Open image in new window Fig. 6 Gas release strength in the uplift period of the Xujiahe coal measures and carbonaceous mudstones.
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The inland arid region comprises a number of basin units that are surrounded by mountains.
The oldest episode consists of fine-grained muds deposited during a period of relative stability in the basin (units e, f, and g).
Spectrally, these units cannot be distinguished from other rock units in the ROI, which might suggest that they are eroded remnants of older Kufrah basin units.
Within the geothermal reservoir in the Bavarian Molasse Basin, units with a perturbed stress field can either be linked to lithofacial homogeneous bodies (e.g. reef complexes) with a significant size or tectonic structures, as e.g. observed in a set of combined strike-slip/extensional fault system with several en-echelon normal faults building several small relay ramps (Lueschen et al. 2014).
We compare the mass fluxes from large drainage basin units with interior snow accumulation calculated from a regional atmospheric climate model for 1980 to 2004.
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