In this paper, we first reconstructed the burial history using the basin model and synchronously conducted the isothermal adsorption experiment.
These antecedent watershed conditions were evaluated using measured reservoir inflows and climate and watershed conditions analyzed using the Basin Characterization Model (Flint et al. 2013).
We used the Basin Characterization Model (BCM) to model the hydrologic cycle for the California hydrologic region [Figure 1; modified from Hickman (1993)].
First, an initial set of parameters was obtained for each model type by leaving all parameters free and using the basin hopping algorithm provided by SciPy (Blanco-Silva, 2013) to identify a global error basin.
Kubo et al. (2016) showed that the amplitudes and waveforms for the S-waves can be well reproduced using the 1D basin model proposed in this paper and the complex rupture model proposed in their paper, whereas the model in Pandey (2000) strongly underestimates the amplitudes of S-waves.
The study is conducted using the Indus Basin Model Revised – Multi-Year (IBMR MY), a hydro-agro-economic model of the Indus River within Pakistan that simulates river and canal flows, groundwater pumping, water use and economic activities with a distributed, partial equilibrium model of the local scale agro-economic activities in the basin.
Malcolm Forbes, Frank Sinatra and Mario Puzo, whose boat was named Godfather, used the basin.
Coupling the measured T h (°C) with the burial and geothermal histories reconstructed using 1D basin modeling, we relate the homogenization temperature to the relevant geological ages: i.e., 425 412 and 9 4 Ma, corresponding to the Middle to Late Silurian and the Miocene to Pliocene, respectively.
Coupling the homogenization temperatures of fluid inclusions with stratigraphic burial and geothermal histories, reconstructed using 1D basin modeling, the episodes and timing of oil entrapment were determined.
Akbarpour and Sharifi (2005) used GIS (Geographical Information system) to obtain the physiographical characteristics of slope map, soil texture, and runoff curves of Bayeg and Rashtkhar basins, but determined the peak flood discharge of both basins using the WMS model.
