Read e-book online 3-regularity in generalized quadrangles of order (s, s2) PDF

By Thas J. A.

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M. Ripley Department of Geological Sciences, Indiana University, Bloomington, IN 47401, USA Abstract. Key factors for the formation of world-class magmatic NiCu deposits include sulfide saturation in magma, large magma/sulfide ratio and accumulation of sufficient quantity of immiscible sulfide liquid in limited localities. Results from two well-known Ni-Cu deposits in the world, the Talnakh deposits in Siberia, Russia and the Voisey’s Bay Deposit in Labrador, Canada, indicate that a dynamic magma conduit in the upper crust is an ideal environment in which these factors can prevail.

6 What controls the endowment of VHMS deposits in Archean terrains? Lead and Nd isotope data suggest fundamental differences in the tectonic character of the Eastern Goldfields Province and the Abitibi-Wawa Subprovince. The Eastern Goldfields Province is characterized by evolved crust with relatively narrow rift-like zones that contain the only known significant VHMS deposits. ) extensional zone that was active over a period of 50 million years. Hence, we infer that the high endowment of VHMS deposits in the Abitibi-Wawa Subprovince is a consequence of its unique tectonic character, which would have resulted in both a high heat flow and extensional structures to channel fluid flow.

In the same area, actinolite-epidote-chlorite ortho-greenschists, interlayered in metasediments are rhythmically interlayered by beds, 15-30 cm thick. 15 % MnO, accompanied by siderite, quartz, albite, Cr-magnetite, hyalophane, phengite, Cr-chlorite and chalcopyrite. In the Krecevo-Kiseljak-Fojnica- Busovaca area occur numerous predominantly small and subordinate middle sized quartz veins. 5% SiO2, accessories are chlorite, sericite and pyrite. The quartz veins are predominantly synkinematic, some are post-kinematic.

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3-regularity in generalized quadrangles of order (s, s2) by Thas J. A.


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