Abstract

The uneven Earth’s spinning has been reported to affect geological processes, i.e. tectonism, seismicity and volcanism, on a planetary scale. Here, we show that changes of the length of day (LOD) influence eruptive activity at subduction margins. Statistical analysis indicates that eruptions with volcanic explosivity index (VEI) ≥3 alternate along oppositely directed subduction zones as a function of whether the LOD increases or decreases. In particular, eruptions in volcanic arcs along contractional subduction zones, which are mostly E- or NE-directed, occur when LOD increases, whereas they are more frequent when LOD decreases along the opposite W- or SW-directed subduction zones that are rather characterized by upper plate extension and back-arc spreading. We find that the LOD variability determines a modulation of the horizontal shear stresses acting on the crust up to 0.4 MPa. An increase of the horizontal maximum stress in compressive regimes during LOD increment may favour the rupture of the magma feeder system wall rocks. Similarly, a decrease of the minimum horizontal stress in extensional settings during LOD lowering generates a larger differential stress, which may enhance failure of the magma-confining rocks. This asymmetric behaviour of magmatism sheds new light on the role of astronomical forces in the dynamics of the solid Earth.

Highlights

  • The angular velocity of Earth’s rotation varies in response to astronomical forcing and terrestrial dynamics

  • We propose that the rupture of magma chamber wall rocks occurs when the differential stress generated by length of day (LOD) oscillation reaches a critical threshold

  • We evaluate whether the ΔLODeff-related stress can be comparable with the other computed stress values, associated with other physical process, capable to promote the triggering of volcanic eruptions

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Summary

Introduction

The angular velocity of Earth’s rotation varies in response to astronomical forcing and terrestrial dynamics. Results Our results show that Earth’s spin changes induce an asymmetric response of VEI ≥3 explosive eruptions along “W”- vs “E”-directed subduction zones (Fig. 1).

Results
Conclusion
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