Step 1: Understanding the formation of Ni-Cu sulphide ores.
Ni-Cu sulphide ores in gabbro-norite rocks are formed through a process called liquid immiscibility. This occurs when magma separates into two immiscible liquids, one rich in sulphide minerals, which eventually solidifies as ore deposits.
Step 2: Analyzing the options.
(A) Hydrothermal replacement: This process involves the replacement of minerals by hydrothermal fluids but is not responsible for the formation of Ni-Cu sulphide ores.
(B) Volcanic exhalation: Volcanic exhalation is a process involving the release of gases, not related to the formation of these ores.
(C) Liquid immiscibility: This is the correct process, where the magma separates into sulphide-rich liquid, leading to the formation of Ni-Cu sulphide ores.
(D) Contact metamorphism: Contact metamorphism involves heat from an intrusion altering surrounding rocks, but it is not responsible for the formation of Ni-Cu sulphide ores.
Step 3: Conclusion.
The correct answer is (C) Liquid immiscibility because this process is responsible for the formation of syngenetic Ni-Cu sulphide ore.
| Column I | Column II | ||
| P. | Malanjkhand | 1. | Uranium ore |
| Q. | Tummalapalle | 2. | Gold ore |
| R. | Bhukia | 3. | Tin ore |
| S. | Tosham | 4. | Copper ore |