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I agree with Peter Donis' more careful answer, if you try to ask "what happens if a mass suddenly disappears" in GR, and work through the mathematics, you find that it can't happen because of local conservation laws.
I would suggest that doing some research on tidal locking would be helpful to the OP. You don't need GR for this, either. For instance, Wikki http://en.wikipedia.org/wiki/Tidal_locking has some of the basics:
and
Wikki has some basic info on the well known behavior of angular momentum, including the breakdown of total angular momentum into spin and orbital components
http://en.wikipedia.org/wiki/Angular_momentum
The section below would be of particular interest:
I would suggest that doing some research on tidal locking would be helpful to the OP. You don't need GR for this, either. For instance, Wikki http://en.wikipedia.org/wiki/Tidal_locking has some of the basics:
Tidal locking results in the Moon rotating about its axis in about the same time it takes to orbit Earth. Except for libration effects, this results in the Moon keeping the same face turned towards Earth, as seen in the figure on the left. (The Moon is shown in polar view, and is not drawn to scale.) If the Moon were not spinning at all, it would alternately show its near and far sides to Earth, while moving around Earth in orbit, as shown in the figure on the right.
and
The angular momentum of the whole A–B system is conserved in this process, so that when B slows down and loses rotational angular momentum, its orbital angular momentum is boosted by a similar amount (there are also some smaller effects on A's rotation). This results in a raising of B's orbit about A in tandem with its rotational slowdown. For the other case where B starts off rotating too slowly, tidal locking both speeds up its rotation, and lowers its orbit.
Wikki has some basic info on the well known behavior of angular momentum, including the breakdown of total angular momentum into spin and orbital components
http://en.wikipedia.org/wiki/Angular_momentum
The section below would be of particular interest:
In orbits, the angular momentum is distributed between the spin of the planet itself and the angular momentum of its orbit:
## \mathbf{L}_{\mathrm{total}} = \mathbf{L}_{\mathrm{spin}} + \mathbf{L}_{\mathrm{orbit}} ##