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In response to westward subduction of the Paleo-Pacific, the North China Craton experienced the uplift of an eastern coastal plateau followed by subsidence in the Early Cretaceous, which potentially drove a shift in climatic patterns. Here we use the oxygen isotope ratios of garnets from magmatic...
Hybridization of asthenospheric and lithospheric melts is required to explain kimberlite compositions16. At pressures conducive to diamond formation (≳5 GPa), the LAB—a thermal boundary with a temperature range of 1,300–1,400 °C—closely coincides with the solidus of carbonated mantle2,...
In response to westward subduction of the Paleo-Pacific, the North China Craton experienced the uplift of an eastern coastal plateau followed by subsidence in the Early Cretaceous, which potentially drove a shift in climatic patterns. Here we use the oxygen isotope ratios of garnets from magmatic...
a, Frequency distribution of carbonatites (n = 387; data from ref. 42) and kimberlites (n = 1,133; data from ref. 65) through geological time, showing peaks coinciding with the break-up phase of supercontinent cycles.b, Cross-correlations between ΔFand global carbonatites spa...
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The CN bond is a powerful probe of protein structure and dynamics because it absorbs in a region of the infrared spectrum apart from the other vibrations that occur naturally in proteins, and because its infrared absorption line shape is sensitive to specific characteristics of the local environment...
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