Nickel Ore Deposits and Their Geological Associations
Common Geological Settings for Nickel Ores
Nickel ores are commonly found in specific geological environments, including:
- Ultramafic Igneous Rocks: These rocks, rich in magnesium and iron, often host nickel sulfide deposits.
- Laterites: Formed by intense weathering of ultramafic rocks, leading to nickel-enriched lateritic deposits.
- Sea-Floor Polymetallic Nodules: Contain significant amounts of nickel along with manganese, copper, and cobalt.
Step 1: Identifying the Incorrect Association
- Skarns: A group of metamorphic rocks formed by contact metamorphism of calcareous rocks.
- **Skarns are not a primary source of nickel**, as they are more commonly associated with tungsten, iron, and copper mineralization.
Step 2: Determining the Correct Answer
Since skarns do not typically host nickel ores, the correct answer is:
\[ \mathbf{(D):\ Skarns} \]
Final Answer:
Thus, nickel ores are not typically associated with skarns, making the correct option: (D).