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This takes a broken-down date table, as produced by os.date("*t"), and
converts it into an integer number of seconds since the epoch UTC,
interpreting it as a time in a given time zone. Simply passing a date
table to os.time is not good enough, because os.time always assumes the
date table represents a local time; i.e., you will get different results
from running os.time({year=2012,month=1,day=1,hour=12,min=0,sec=0})
depending on what time zone you run it in.
Here is some documentation for Nmap, but these files are much less comprehensive than what you'll find at the actual Nmap documentation site ( http://nmap.org ).