The magma activity on the earth's surface not only shapes the magnificent natural landscape, but also buries undiscovered mineral deposits. Among them, the magma copper deposits produced by the rock melting process, namely "granite copper mines", have become the most important copper resources in the world today. The formation of these deposits is a testament to the dynamic workings of the Earth's interior and is crucial to meeting humanity's copper needs.
Granite copper deposits are formed by hydrothermal fluids released from magma chambers thousands of meters deep. Due to high temperature and pressure, these fluids form the vein structure of the rock and mineral deposits along the veins. Over time, these fluids began to interact with moisture from the atmosphere, further promoting multiple levels of hydrothermal alteration, forming deposits rich in copper, molybdenum, silver and gold.
The economic value of these large copper deposits is comparable to the balance of the Earth for thousands of years, and their ore concentration can be as low as 0.15% and still be worth mining.
Based on a comprehensive analysis of geological data, there are more than 120,000 granite copper deposits in the world, of which an estimated 38% are still in existence. The resources of these copper deposits are not only copper, but also important by-products such as gold and molybdenum. This makes granite copper mines the main source to meet global demand today, and most of their geological ages belong to the Phanerozoic, showing the activeness of their formation.
The vast majority of large granite copper deposits are associated with calcic-alkaline intrusions, although some gold-rich deposits are associated with high-sodic-calcic magmatic compositions. These magmas associated with the formation of granite copper deposits usually come from partial melting of rocks in subduction zones where seawater is altered.
The melting of the mantle and the structural conditions required for the ascent of magma are both key to the formation of granite copper deposits.
Although granite copper deposits are associated with arc volcanism, they are not typical of this environment. Studies have shown that structural changes and pressure transformation methods are the key factors triggering the formation of granite copper deposits. These include compression of the troposphere, enlargement of the volcanic chamber, and enhanced differentiation of hydrothermal fluids.
Granitic copper deposits are often associated with multiple intrusions and dikes and are characterized by multi-colored ores and diverse mineral displays. Sulfide deposits often occur between rock fragments to create rich mineral deposits.
As open-cut mining methods become more common, these copper mines are being mined in increasingly sophisticated ways, making for more efficient use of resources.
Currently, most of the world's granite copper mines are concentrated in western America, Southeast Asia, Oceania and other regions, all of which are distributed on the Pacific Ring of Fire. As the demand for copper continues to increase with global economic development, the development potential of these deposits has become increasingly important.
As global demand for resources continues to rise, developing and optimizing the technology for these copper mines will be a major challenge for the industry in the future. In addition to traditional prospecting methods, the introduction of new technologies will become an important trend in the industry. For future granite copper mines, exploring potential resources and sustainable management will be important considerations.
Faced with the ever-evolving global economic environment and resource pressures, have you ever thought about how these granite copper mines hidden deep underground will shape the future of human life and industrial development?