The correct response is:
Minerals from the crust dissolve in water that is superheated by magma, and the minerals are deposited on the ocean floor as the water cools.
At divergent boundaries, when tectonic plates move apart, magma rises from the mantle and can heat the surrounding water. This superheated water can dissolve minerals from the crust, and as it rises and cools, those minerals can precipitate and form deposits on the ocean floor. This process is common at mid-ocean ridges where hydrothermal vents are found.