The highly radiogenic Os and Pb isotopic compositions of the Jiangzi diabases were produced by crustal contamination, but the Cuona basalts experienced the least crustal contamination given their relatively low γOs(t), 206Pb/204Pbi, 207Pb/204Pbi, and 208Pb/204Pbi values. The Cuona basalts were generated by low degrees of melting (3–5%) of garnet lherzolites (3–5 vol.% garnet), and elsewhere the Jiangzi diabases were formed by relatively lower degrees of melting (1–3%) of garnet lherzolite (1–5 vol.% garnet). The analyzed mafic rocks are enriched in high field strength elements and have positive Nb–Ta anomalies relative to Th and La, which have ocean island basalt-like characteristics. Zircon grains from these two localities yielded concordant weighted mean 206Pb/238U ages of 137.25 ± 0.98 and 131.28 ± 0.78 Ma (2σ), respectively. Here we present petrological, geochronological, geochemical, and Sr–Nd–Hf–Pb–Os isotopic data for high-Ti mafic rocks from two localities (Cuona and Jiangzi) in the eastern Tethyan Himalaya igneous province (147–130 Ma). There are some older (147–130 Ma) magmatic provinces on circum-eastern Gondwana, but the relationship between these provinces and the Kerguelen mantle plume remains controversial. The Kerguelen large igneous province (LIP) has been related to mantle plume activity since at least 120 Ma. The low γOs(t) values relative to many other plume-related picrites (from ocean islands or flood basalt provinces) indicate that there was no clear Os isotope evidence of involvement of the Earth's core or recycled crustal components in the formation of Emeishan flood basalt province.

There is no clear evidence for recycled crustal material in the mantle source of the Emeishan picrites, or for a significant degree of interaction of the picrites with ancient subcontinental lithospheric mantle of the Yangtze craton. The low γOs(t) values of the picrites are unusual in terms of plume-related magmatism. The high γOs(t) values of the basalts could be the result of crustal contamination, which is enabled by the low Os concentrations in the parental basalts. The picrites have distinctly unradiogenic Os isotopes with γOs(t) values (t = 259 Ma) of − 0.9 to − 2.4, but the associated basalts have suprachondritic Os isotope compositions with γOs(t) of 1.8 to 73.3, which overlap with published data for basalts from other localities in the province. They have higher Os concentrations (1.5–3 parts per billion), and slightly lower Re concentrations (< 0.07 ppb) than those from many other flood basalt provinces (FBPs) and ocean island picrites. The picrites from the two sections have overlapping Re and Os concentrations and initial Os isotopic compositions. Eighteen geochemically well characterised samples, including 12 picrites and 6 basalts from two sections near Lijiang, have been analyzed for Os isotopes. This paper presents the first Re–Os isotope data for picrites from the province. You can quickly set and manage the parameters for conversion with basic and alternative presets.Picrites from the Lijiang area, in the western part of the Emeishan flood basalt province, are considered to be one of the most important indicators of the Emeishan mantle plume, and may represent initial mantle plume activity. It incorporates the Lame MP3 Encoder 3.97 encoding algorithms which generate crisp tantalizing quality audio. This Sound Normalizer is simple to use with fast and excellent quality results. The Sound Normalizer also allows editing ID3 tags (build-in Mp3 ID3 Tag Editor) with support for ID3v1 and ID3v2 tags, converting Wav to Mp3 files and Mp3 to Wav files (build-in Wav/Mp3 Converter) using Lame MP3 Encoder 3.97, listening Mp3 and Wav files using the build-in audio player. The Mp3 Normalizer allows to modify a volume of a scanned file directly without usage tags. The mp3 normalization is fulfilled under standard Replay Gain.

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