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Another radiometric time scale has been developed from the study of the magnetization of basaltic lavas of the ocean floor.
A magnetic-polarity (or paleomagnetic) time scale has been proposed along the line of the geologic time scale; time divisions are called intervals, or epochs.
Intramolecular rearrangement of secondary structure on a millisecond time scale has been observed for the 5′-leader sequence of Leptomonas collososa 70).
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To avoid the ad hoc choice for Cϕ, more sophisticated models for the scalar time scale have been used in simulations using the EMST model.
After the introduction of the time scale calculus by Hilger [3], oscillation theorems for second order dynamic equations on a time scale have been studied by many authors (see for example [9 11] and the references therein).
Continuing our study of sub-Tg dynamics in these systems by QENS, measurements on polycarbonate (PC) and polysulfone (PSF) with deuterated methyl groups (d6) in the ∼10−13 10−11 s time scale have been performed.
Properties of exponential stability of a time varying dynamic equation on a time scale have been also investigated recently by Bohner and Martynyuk [7], DaCunha [9], Du and Tien [11], Hoffacker and Tisdell [16], Martynyuk [17], and Peterson and Raffoul [19].
By the early 1840s much of the geologic time scale had been developed.
Motions on this time scale have been shown to be important in catalysis and allostery.
MD simulations on the microsecond time scale have been recently employed for studies of protein ligand interactions.
More recently, coarse-grained (CG) simulation approaches (23− 28) that allow membrane protein simulations to be readily extended to a microsecond time scale have been used to predict nonspecific lipid−protein interactions for a wide range of membrane proteins (29).
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