All
Single isomorphous replacement with anomalous scattering uses two
datasets that are isomorphous while using the anomalous signal in one
(here scattering and dispersion are synonymous?). How does SIRAS use
the anomalous scattering signal that's different than a single
wavelength anomalous dispersion ?
How does an anomalous difference patterson (SAD) differ from an
isomorphous difference patterson with anomalous scattering (presumably
utilizing a native crystal)?
Can a dataset that was not resolved by MAD/SAD be resolved by MIRAS/
SIRAS provided a good native dataset is available (Does MIRAS/SIRAS
offer more phasing power than a typical SAD dataset?)
Any input would be appreciated!
FR
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Francis Reyes M.Sc.
215 UCB
University of Colorado at Boulder
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