Global Patterns in Cratonic Mid?Lithospheric Discontinuities From Sp Receiver Functions

نویسندگان

چکیده

The goal of this study is to constrain the origins layering in seismic velocity structure within cratonic mantle lithosphere (i.e. mid-lithospheric discontinuities [MLDs]). For long-lived stations cratons worldwide, we calculated S-to-P converted phase receiver function stacks using time domain deconvolution and a k-means algorithm select robust, consistent functions. Negative MLDs appear only 50% stacks, indicating that negative are common but intermittent. correspond shear drops 1%–4%, which could be caused by layers minerals created metasomatism, although vertical anisotropy cannot ruled out. In craton interiors, have lower amplitude (<3% drops) can explained metasomatism original Archean mantle. MLD amplitudes increase with decreasing upper (toward outer margins cratons), do not depend on age craton. Thus, dominated age-related variations composition, and, instead, more strongly correlated proximity tectonic metasomatic activity occurred long after formation. less numerous among Paleoproterozoic thermotectonic ages, view shallow release slab-derived fluids during early “warm” subduction was favorable for We also observe gradients below 150 km at boundaries presence changes lithosphere-asthenosphere boundary and/or Lehmann discontinuity.

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ژورنال

عنوان ژورنال: Geochemistry Geophysics Geosystems

سال: 2021

ISSN: ['1525-2027']

DOI: https://doi.org/10.1029/2021gc009819