世界洋底金属成矿作用的地质-地球物理分区

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当前,在世界洋底已发现的主要和分布最广的固体矿产有铁锰结核、钴锰结壳、相当于黄铁矿型矿石的深海多金属硫化物、磷钙土、金属矿与金刚石砂矿。俄罗斯“南方海洋地质”和“北方海洋地质”联合在安哥拉—巴西和马斯克林群岛—澳大利亚完成了宽带状定期横穿海洋的地质—地球物 At present, the major and most widely distributed solid minerals found on the ocean floor are iron-manganese nodules, cobalt-manganese crusts, deep-sea polymetallic sulphides corresponding to pyrite-type ores, calcium carbonate, metalloids and diamond sand mine. Russia’s “Southern Ocean Geology” and “Northern Ocean Geology” have jointly completed a broadband geologic-geo-periodic crossing of the oceans in Angola - Brazil and the Musclore Islands - Australia
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