Fig. 6: Proposed scenarios for lower crustal sulfide crystallization and mobilization. | Nature Communications

Fig. 6: Proposed scenarios for lower crustal sulfide crystallization and mobilization.

From: Mobilisation of deep crustal sulfide melts as a first order control on upper lithospheric metallogeny

Fig. 6

A Modeling results of progressive sill emplacement at the base of the crust in the Ivrea Zone show the rise in overall temperature on the emplacement of successive sills29. Approximate relative timings of the Isola Sill and Sella Bassa are shown. Note that each magma pulse is emplaced at 1100 °C, though cools quickly; and a significant melt fraction only becomes present when the overall temperature of the complex reaches the silicate solidus. At 1 GPa, Cu-sulfide melt is present and mss crystalline between 1090 and 1160 °C. B Schematic representation of the evolution, fractionation, and mobility of sulfide liquid in lower crustal cumulates. See text for description of Steps 1–8. px pyroxene, amp amphibole, mss monosulfide solid solution, iss intermediate solid solution, cpy chalcopyrite, pn pentlandite, po pyrrhotite. Approximate positions of steps 1–8 from B are indicated in bold on A.

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