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Predicting the hydrodynamics, morphology and evolution of ancient deltaic successions requires the evaluation of the three-dimensional depositional process regime based on sedimentary facies analysis.
The Morne L'Enfer Formation (Late Pliocene) along Cedros Bay and Erin Bay in SW Trinidad, provides a window into the facies and process regime of the ca. 850 m-thick deltaic succession at an inner-shelf location some 100 km landward of the coeval shelf edge.
Exceptionally high shelf-subsidence rates (0.8 6.0+ mm/yr), a marked basinward stepping (to east and northeast) of the paleo-Orinoco shelf prism and post-Pliocene uplift of Trinidad all allow the sedimentary facies, process regime and the evolution of the Late Miocene Orinoco Delta to be evaluated from extensive outcrops along the southwest, and south coasts of Trinidad.
Moreover, air mass flow is a key factor to define and identify the combustion process regime.
In these models, parameters of the VAR model depend on the regime variable (left( {S_{t} } right)), which makes the process regime dependent.
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Subsequent experimental validation of the new injector design, and its flexibility to changing process regimes for GaN and InGaN will be demonstrated for the 42×2″ Planetary Reactor®.
Thereby, the unique advantages of microreaction systems are to carry out chemical reactions in unusual process regimes or under isothermal conditions.
The process was shown to have a universal invariant parameter, which defines conditions of similarity of channels and process regimes with respect to obtaining coatings of equal step coverage quality.
Characteristics of sectors include variety in channel patterns, process regimes and biotope types.
Our results have important implications for understanding deforestation, edge-driven processes, regime shifts, and the management of complex pattern-process relationships.
In the branching-process regime, we simulated the absolute frequency of the two types of interest (A1 B1 and A1 B2) over time.
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