Using nanogranitoids and phase equilibria modeling to unravel anatexis in the crustal footwall of the Ronda peridotites (Betic Cordillera, S Spain)
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文摘

Melt inclusions represent the primary anatectic melt produced during anatexis.

Ojén unit represents an inverted metamorphic sequence, not only in terms of temperature but also in pressure.

Previous geodynamic models cannot explain the evolution of this crustal sequence

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