Foliated rock has parallel layers.
Foliated.
Foliated rock
That would be sedimentary rock, and (honorable mention) occasionally metamorphic rock.
schist
A sill is a type of pluton that is completely parallel to the rock layers into which it intrudes. Sills are formed when magma is injected between pre-existing rock layers and then solidifies. The resulting igneous rock body is typically flat-lying and can be found sandwiched between the surrounding rock layers.
Those would be non-foliated metamorphic rocks, like quartzite and marble.
A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.
A disconformity exists between parallel layers of sedimentary rock. This is when there is a gap in the rock record represented by a horizontal surface separating younger strata from the older ones.
It is likely a type of metamorphic rock, such as schist or gneiss, which form under high temperature and pressure conditions leading to the alignment of mineral grains into flat layers.
Non-foliated metamorphic rock, such as marble or quartzite, is characterized by the absence of visible layering or banding. The mineral grains in these rocks recrystallize and grow in a uniform manner, without forming distinct layers like in foliated rocks. This type of metamorphism typically occurs under conditions of high pressure and temperature without the presence of directed stress.
A metamorphic rock.
Angular unconformity is not a type of unconformity. The three main types of unconformities are nonconformity, disconformity, and paraconformity. A nonconformity occurs when sedimentary rock is deposited on igneous or metamorphic rock, disconformity is an erosion surface between parallel sedimentary layers, and paraconformity is a buried erosion surface within sedimentary layers.