Stratigraphy and tectonic setting of Laochang massive sulfide deposit in the North Qinling belt, central China
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文摘
The Caotangou Group represents a ca. 490–410 volcanic sequence of the backarc basin. Subduction-related volcanism did not stop at ca. 410 Ma in the North Qinling belt. VHMS deposit in the North Qinling belt developed in a backarc basin during ca. 440–410 Ma.
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