Slab breakoff: a causal mechanism or pure convenience?
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摘要:
The idea of lithosphere delamination has long been conceived as a mechanism to cause tectonic uplift,metamorphism and magmatism in active orogenic belts [1-3].Since the publication of the two seminal papers by Davies and yon Blanckenburg [4,5],the idea of slab breakoff has been more widely accepted over the last ~20 years as the favored mechanism to cause collision zone magmatism and exhumation of subduction-zone metamorphosed rocks.These two papers showed the physical probability of slab-breakoff during continental collision and illustrated possible geological consequences using the Alpine geology as an example.