Article https://doi.org/10.1038/s41467-024-53435-7 Crustal melting and continent uplift by mafic underplating at convergent boundaries Received: 5 December 2023 Accepted: 11 October 2024 Check for updates Zhipen
The numerical results show that two distinct breakup modes, namely continental interior and edge breakup ("edge" refer to continent above the plate boundary interface), may develop depending on the "maturity" of the convergent margin and the age of the oceanic lithosphere. For a slab age of ~...
magnesite, oxides and carbonatite melt were performed using a JEOL JXA-8530F Plus field emission electron microprobe (EPMA) at the Centre for Advanced Microscopy, the Australian National University and the Oxford INCA 250 X-MAX 20 energy-dispersive X-ray spectrometer at Macquarie University. The an...
magnesite, oxides and carbonatite melt were performed using a JEOL JXA-8530F Plus field emission electron microprobe (EPMA) at the Centre for Advanced Microscopy, the Australian National University and the Oxford INCA 250 X-MAX 20 energy-dispersive X-ray spectrometer at Macquarie University. The an...
We document a complete cycle of deep burial and exhumation in metamorphosed volcano-sedimentary rocks of the Waroonga Greenstone Belt (WGB) along the Ida Fault, a major tectonic boundary (≥500 km long) within the Yilgarn Craton. The Yilgarn Craton mostly exposes Meso- to Neoarchean granite–...
Their upper reaches are westward and eastward flowing, respectively, with a very low divide, clearly closer to the eastern boundary of the topographic domain. The latter evidence suggests that the westward flowing river exerted the most effective headward erosion. The headward erosion of the ...
250), constitute an important boundary condition in the thriving literature. Specifically, we propose that as a conduit for meeting AEs social and relational needs in the new host country's cultural environment (Claggett and Karahanna, 2018; Ehrhardt and Ragins, 2019; Farh et al., 2010), ...
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Metamorphic fluids, faults, and shear zones are carriers of carbon from the deep Earth to shallower reservoirs. Some of these fluids are reduced and transport energy sources, like H2 and light hydrocarbons. Mechanisms and pathways capable of transporting
We document a complete cycle of deep burial and exhumation in metamorphosed volcano-sedimentary rocks of the Waroonga Green- stone Belt (WGB) along the Ida Fault, a major tectonic boundary (≥500 km long) within the Yilgarn Craton. The Yilgarn Craton mostly exposes Meso- to Neoarchean granite...