Thermal modelling in shallow subduction: an application to low <i>P/T</i> metamorphism of the Cretaceous Shimanto Accretionary Complex, Japan

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<jats:title>Abstract</jats:title><jats:p>This paper presents the results of numerical modelling to investigate the regional occurrence of prehnite‐bearing metamorphic rocks at shallow levels in subduction zones. The modelling assumes a simple geometrical configuration in which the thermal structure in a prism is controlled by boundary conditions at the top and base of the prism. It is expected that the predominant metamorphic facies in a prism will change with decreasing age of the descending slab. The results of thermal modelling show that the facies boundary between pumpellyite–actinolite and prehnite–actinolite facies (including prehnite–pumpellyite facies) overlaps with an array of <jats:italic>P–T</jats:italic> conditions in the prism when the age of a descending slab is younger than 10 Myr. This implies that the change of the predominant metamorphic facies from pumpellyite–actinolite to prehnite–actinolite facies will switch drastically. The critical age of the switch depends on subduction parameters. In particular, the critical age of the descending slab is <5 Myr in the case of no shear heating, with a subduction rate of <jats:italic>v</jats:italic>=75–200 mm y<jats:sup>−1</jats:sup> and subduction angle of <jats:italic>θ</jats:italic>=5–15°. For shear heating (constant shear stress=30 MPa) with a subduction rate of <jats:italic>v</jats:italic>=75 mm y<jats:sup>−1</jats:sup> and subduction angle of <jats:italic>θ</jats:italic>=10° the critical age is 7 Myr. To test this switching behaviour in the development of prehnite–actinolite facies in the prism, petrologic data from the Cretaceous Shimanto Accretionary Complex (CSAC) in Kyushu, Japan were compiled. The regional occurrence and mineral assemblages of prehnite‐bearing metamorphic rocks suggest that the most of CSAC was metamorphosed under prehnite–actinolite facies. This conclusion is consistent with subduction of a young, hot slab, as has been proposed based on other geological observations. This suggests that the regional extent of the prehnite–actinolite facies metamorphic rocks may be a unique evidence for the subduction of a young, hot slab.</jats:p>

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