Basin transition

Read J.F. (1980) Carbonate ramp-to-basin transitions and foreland basin evolution, Middle Ordovician, Virginia Appalachians. AAPG Bull. 64, 1575-1612. 

Photochemical and photocatalytic processes are responsible for self-cleaning of the atmosphere, soils, and water basins. Transition metal complexes contribute mainly to cleaning of the hydrosphere, although their cooperation with atmospheric gases is as yet underestimated and the progress needs more detailed investigations. 

Fig. 3.3 Internal energy and number of hopping residues along a reproducible representative FM trajectory for the thermophilic variant of protein G. A hopping residue is defined as tagged for a Ramachandran basin transition in the coarse-grained stochastic process that underlies the FM torsional dynamics. Reprinted from [35], with permission from Elsevier...

Powis, G.D. (1989) Revision of Triassic stratigraphy at the Cooper Basin to Eromanga Basin transition. In The Cooper and Eromanga Basins, Australia (Ed. O Neil, B.J.), pp. 265-277. Proc. Petroleum Exploration Soc. Australia, Soc. Petroleum Engineers, Australian Soc. Exploration Geophysicists (S.A. Branches), Adelaide. 

Bevins R.E., Kokelaar BJP. and Dunklq PN., 1984, Petrology and geochenustry of lower to middle Ordovician igneous rocks in Wales a volcanic arc to marginal basin transition. Proc. Ceol Ass., 95, 337—347. 

Inherent structure analysis provides useM insight into the correlated hydrogen-bond dynamics of water. Many experiments suggest that this tetrahedral HB network has defects, such as an extra (fifth) molecule in the first coordination shell, or 3-coordinated species. Indeed, such 5-coordinated molecules have been directly identified in simulations and the defects were found to be a catalyst for initiating motion in the system, making an obvious possible connection between network defects promoting diffusion and the basin transitions that give rise to diffusive motion of that system [8]. 

Such an analysis shows that among the ISs visited by the system, there are islands (basins) of various sizes, distributed randomly in time, and thus the transitions among the islands (called the basin-basin transitions) occur intermittently. The ISs of water are different from other liquids. As the temperature is lowered, the system spends longer and longer times in a few basins. The basin-basin transitions comprise large IS changes but may often involve relatively small energy barriers [5]. 

Schlager, W., and Chermak, A. 1979. Sediment facies of platform-basin transition Toimge of the ocean, Bahamas. In Geology of Continental Slopes, Doyle, L.J., and Pilkey, O.H., eds.. Society of Economic Paleontologists and Mineralogists, Sp>ecial Publication 27, Tulsa, OK, 374pp. 

Woodhead J, Eggins S, Gamble J (1993) High field strength and transition element systematics in island arc and back-arc basin basalts evidence for multi-phase melt extraction and a depleted mantle wedge. Earth Planet Sci Lett 114 491-504... 

The temperature patterns follow a transition from the more oceanic western area (milder temperatures) to the central depression (high temperatures in summer and intense cold and fog in winter). The northwest-southeast cold and dry wind ( cierzo ) is characteristic of the central depression of the Ebro basin, especially in spring. The cierzo at the middle Ebro valley (around Zaragoza) can lead to soil erosion and salt transport [17]. The wind intensity at this area is highly correlated with evapotranspiration [18]. A mild warm wind is sometimes occurring (especially in summer) following the opposite direction (southeast-northwest). 

Tabara JD, Ilhan A (2008) Culture as trigger for sustainability transition in the water domain the case of the Spanish water policy and the Ebro river basin. Reg Environ Change 8 59-71. doi 10.1007/sl0113-007-0043-3... 

Leaving the details, the equation describing the motion of one particle in two electrostatic waves allows perturbation methods to be applied in its study. There are three main types of behavior in the phase space - a limit cycle, formation of a non-trivial bounded attracting set and escape to infinity of the solutions. One of the goals is to determine the basins of attraction and to present a relevant bifurcation diagram for the transitions between different types of motion. 

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