  Using observations from Solar Dynamics Observatory, we studied an interesting
example of a sigmoid formation and eruption from small-scale flux canceling
regions of active region (AR) 11942. Analysis of HMI and AIA observations infer
that initially the AR is compact and bipolar in nature, evolved to sheared
configuration consisting of inverse J-shaped loops hosting a filament channel
over a couple of days. By tracking the photospheric magnetic features, shearing
and converging motions are observed to play a prime role in the development of
S-shaped loops and further flux cancellation leads to tether-cutting
reconnection of J-loops. This phase is co-temporal with the filament rise
motion followed by sigmoid eruption at 21:32 UT on January 6. The flux rope
rises in phases of slow (v$_{avg}$ = 26 km~s$^{-1}$) and fast (a$_{avg}$= 55
ms$^{-2}$) rise motion categorizing the CME as slow with an associated weak
C1.0 class X-ray flare. The flare ribbon separation velocity peaks at around
peak time of the flare at which maximum reconnection rate (2.14 Vcm$^{-1}$)
occurs. Further, the EUV light-curves of 131, 171\AA~have delayed peaks of 130
minutes compared to 94\AA~and is explained by differential emission measure.
Our analysis suggests that the energy release is proceeded in a much long time
duration, manifesting the onset of filament rise and eventual eruption driven
by converging and canceling flux in the photosphere. Unlike strong eruption
events, the observed slow CME and weak flare are indications of slow runway
tether-cutting reconnection where most of the sheared arcade is relaxed during
the extended post phase of the eruption.
