There are only a few observations published so far that show the initiation
of a coronal mass ejection (CME) and illustrate the magnetic changes in th
e surface origin of a CME. Any attempt to connect a CME with its local sola
r activities is meaningful. In this paper we present a clear instance of a
halo CME initiation. A careful analysis of magnetograms shows that the only
obvious magnetic changes in the surface region of the CME is a magnetic fl
ux cancellation underneath a quiescent filament. The early disturbance was
seen as the slow upward motion in segments of the quiescent filament. Four
hours later, the filament was accelerated to about 50 km s(-1) and erupted.
While a small part of the material in the filament was ejected into the up
per corona, most of the mass was transported to a nearby region. About fort
y minutes later, the transported mass was also ejected partially to the upp
er corona. The eruption of the filament triggered a two-ribbon flare, with
post-flare loops connecting the flare ribbons. A halo CME, which is inferre
d to be associated with the eruptive filament, was observed from LASCO/C2 a
nd C3. The halo CME contained two CME events, each event corresponded to a
partial mass ejection of the filament. We suggest that the magnetic reconne
ction at the lower atmosphere is responsible for the filament eruption and
the halo CME.