There is no significant weathering from oxygen. However, the particles in the wind (oxygen) can weather a rock.
No atmosphere-no weather.
Mechanically
Natural acids chemically weather rocks by reacting with minerals in the rock, causing them to break down. Mechanical weathering involves physical processes like freezing and thawing, which cause rocks to break apart without altering their chemical composition.
Water can chemically weather rocks by dissolving minerals, water can also physically weather rocks by fracturing them by hydraulic pressure or frost wedging.
The most likely process that will chemically weather iron-rich rocks is oxidation. When iron is exposed to oxygen and water, it can react to form iron oxide, commonly known as rust. This process weakens the rock structure and can eventually lead to the breakdown of the rock into smaller fragments.
Water can chemically weather rocks by dissolving minerals, water can also physically weather rocks by fracturing them by hydraulic pressure or frost wedging.
Oxygen was trapped in rocks in the very early days of earth. These rocks are known as "banded rocks". It took a long time before the oxygen was let out of the rocks.
water, air, chemicals, ect Acid rain contains sulfuric acid that can chemically weather rocks.
Sedimentary rocks can be both chemically and mechanically weathered.
The acids chemically weather rock by breaking up their chemical composition, which eventually causes the rock to lose mass by decomposition.
Atmospheric oxygen tends to be elemental oxygen (O2). Oxygen in rocks and minerals is chemically combined with other elements to form compounds called oxides.
The process by which oxygen and water weather rocks is called chemical weathering. In this process, chemical reactions occur between minerals in the rocks and the oxygen and water, leading to the breakdown of the rock structure. This can result in the formation of new minerals and the release of soluble ions, contributing to soil formation and the alteration of the landscape.