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- W2380648169 abstract "The tectonic evolution of the intracontinental rift period about the Jiangda tectonic belt is discussed based on the terrane and plate tectonics theories.As a main portion of the Changdu-Simao tectonic zone,the Jiangda tectonic belt has experienced a similar intracontinental rifting history to its main tectonic zone.The intracontinental rifting of the Jiangda tectonic belt developed on the base of the continental margin arc.The intracontinental rift period of the Jiangda tectonic belt experienced volcanic graben(T3-J1),intracontinental sag(J2-K2)and strike-slip graben-horst structure stages.In this period,the characteristic rift-type palaeogeomorphology,sedimentary formation and bimodal magmatism formed.Sedex type ore deposits formed in the volcanic graben stage and a lot of skarn polymetallic ore deposits formed in the intracontinental sag stage." @default.
- W2380648169 created "2016-06-24" @default.
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- W2380648169 date "2010-01-01" @default.
- W2380648169 modified "2023-09-28" @default.
- W2380648169 title "Intracontinental rift evolution and mineralization of the Jiangda tectonic belt on the eastern margin of the Tibetan plateau,SW China" @default.
- W2380648169 hasPublicationYear "2010" @default.
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