On the metallogenic role of craton terrains in the marginal sea lithosphere
Tóm tắt
The metallogenic efficiency of the marginal sea lithosphere of Northeastern Asia is associated mainly with the ore formation variety of the remaining cratons and microcratons that defined the structural peculiarity of the region; these are setoffs of the Precambrian basement, brachyform, anticline highs, and genesis of rifts within TMA periods. These formations allowed us to explain the reasons for the unique metal-bearing feature of the marginal sea lithosphere of the Pacific Ocean ore belt in addition to phenomena of an inherited nature of mineralization and conditions of formation of polychronous ore deposits.
Tài liệu tham khảo
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