深海矿床有各种不同的特征和成因,它是沿着大陆和大陆边缘发生的各种地质作用的产物,并扩散到深海底。铜、铅、锌矿床可能在板块离散的早期阶段形成在沿着大陆边缘的大陆地壳上。由来自新生离散边缘的热所驱动的海水热循环接触大陆地壳的岩石而淋滤着各种金属,并把所产生的溶液挟带到同海底,当溶液同底层水接触后,经过一系列过程便发生了 Deep sea deposits have a variety of different characteristics and causes, which are products of various geological processes along continental and continental margins and spread to deep seabed. Copper, lead and zinc deposits may form on the continental crust along the continental margin in the early stages of plate tectonics. The heat of the seawater, driven by the heat from the nascent discrete edge, contacts the crustal rocks of the continent to leach the various metals and bring the resulting solution to the seafloor. After the solution comes in contact with the subterranean water, it undergoes a series of processes It happened