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Here are some of the key findings of the expedition:

The fragments of IM1 were found in a small area of the ocean floor, which suggests that the meteor impacted in a relatively small area.

The fragments were made of a material that is not found in our solar system, which provides further evidence that IM1 originated from another star system.

The fragments were very small, ranging in size from a few millimeters to a few centimeters.

The fragments were subject to degradation by the Earth's atmosphere, which makes it difficult to study them.