Granite, when weathered and eroded, doesn't directly turn into a single specific sedimentary rock. Instead, the process of weathering and erosion breaks down the granite into various components:

* Quartz: This durable mineral survives the weathering process and becomes sand grains.

* Feldspar: This mineral breaks down into clay minerals.

* Micas: These minerals also break down into clay minerals.

These components then get transported and deposited in a new location. Depending on the depositional environment, the resulting sedimentary rocks can be:

* Sandstone: If quartz grains are abundant, the sedimentary rock will be sandstone.

* Claystone or Shale: If clay minerals are dominant, the sedimentary rock will be claystone or shale.

* Arkose: If feldspar is present in significant amounts, the resulting sandstone will be arkose.

Therefore, granite can ultimately form a variety of sedimentary rocks depending on the weathering, erosion, and depositional processes involved.