The correct option is 1 and 3 only.
Explanation
The distribution of minerals in India is intrinsically linked to the country's geological structure. Generally, ancient crystalline rocks (igneous and metamorphic) host metallic minerals, while sedimentary formations are the primary source of non-metallic minerals and mineral fuels.
Statement 1 is Correct: The Peninsular Plateau, composed of old crystalline and metamorphic rocks (such as the Dharwar and Cuddapah systems), contains the vast majority of India's metallic mineral reserves. This region is rich in ferrous minerals like iron ore and manganese, as well as non-ferrous minerals like copper and bauxite.
Statement 2 is Incorrect: The Himalayan region is geologically complex and is known to contain deposits of metallic minerals such as copper, lead, zinc, cobalt, and tungsten. While it contains some Tertiary coal (e.g., in Jammu & Kashmir and the North East), it is not broadly classified as being "rich in mineral fuels" compared to the major sedimentary basins. The primary reserves of mineral fuels (coal and petroleum) are located in the Gondwana basins and the sedimentary basins of Assam, Gujarat, and offshore regions.
Statement 3 is Correct: Sedimentary basins and young fold mountains are the typical geological settings for non-metallic minerals. Minerals such as limestone, dolomite, gypsum, phosphate, and salt are commonly found in sedimentary rock systems (e.g., the Vindhyan system).
Key Takeaway: In India, metallic minerals are concentrated in the Peninsular Shield, whereas mineral fuels (coal, petroleum) and non-metallic minerals (limestone, gypsum) are predominantly associated with sedimentary basins.