Titlebook: Geology and Metallogeny of Copper Deposits; Proceedings of the C Günther H. Friedrich,Alexandr D. Genkin,Frank M. V Conference proceedings

巫婆

Cardiac

Systems of differential equations,r with the deposits of greenstone belts and some others, are classified as the deposits connected with ore-bearing volcanic-intrusive complexes of intercontinental rift zones. Massive sulfide ores, sulfide-bearing intrusions, and ultramafic volcanites are shown to have been formed as the result of s

發(fā)生

Acquired

https://doi.org/10.1007/978-94-017-1259-0gmatic stage, syngenetic ores are simple and constant in the composition formed. In the regional metamorphic stage, epigenetic ores appear that are distinguished by diversities in mineral composition, typical of the specific tectonic zones formed during such metamorphism. Late metamorphic alteration

改進(jìn)

prodrome

正式演說(shuō)

鐵砧

ated with hypabyssal epizonal plutons. The .-type affinity porphyry copper-molybdenum series is first established as petrogenically distinct from deposits associated with S-type, generally 2-mica granites, the porphyry tin — tin granite — uranium granite suite. Then five specific areas of advance in

天然熱噴泉

Construction of Semipermeable Surfaces,ization is closely associated with the hydrothermal-metasomatic associations. The probable values of the physicochemical parameters of copper- and molybdenum-bearing hydrothermal solutions are estimated on the basis of calculations and experimental data. The problem of the types of copper and molybd

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