[HTML][HTML] LA_MC_ICP_MS 锆石微区原位U_Pb 定年技术_ 侯可军
侯可军， 李延河， 田有荣 - 矿床地质, 2009 - wenku.baidu.com
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[HTML][HTML] Calibration and correction of LA-ICP-MS and LA-MC-ICP-MS analyses for element contents and isotopic ratios
Abstract LA-ICP-MS and LA-MC-ICP-MS have been the techniques of choice for achieving
accurate and precise element content and isotopic ratio, the state-of-the-art technique …
accurate and precise element content and isotopic ratio, the state-of-the-art technique …
Temporal and spatial variations of Mesozoic magmatism and deformation in the North China Craton: Implications for lithospheric thinning and decratonization
Abstract Mesozoic (Triassic–Cretaceous) magmatic rocks and structural deformation are
widely distributed in the North China Craton (NCC) and are crucial to understanding the …
widely distributed in the North China Craton (NCC) and are crucial to understanding the …
[HTML][HTML] Two-billion-year-old volcanism on the Moon from Chang'e-5 basalts
The Moon has a magmatic and thermal history that is distinct from that of the terrestrial
planets. Radioisotope dating of lunar samples suggests that most lunar basaltic magmatism …
planets. Radioisotope dating of lunar samples suggests that most lunar basaltic magmatism …
Qinghu zircon: A working reference for microbeam analysis of U-Pb age and Hf and O isotopes
Zircon is the most useful mineral for studies in U-Pb geochronology and Hf and O isotope
geochemistry. Matrix effect is a major problem of the microbeam techniques such as SIMS …
geochemistry. Matrix effect is a major problem of the microbeam techniques such as SIMS …
Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and jet sample cone in combination with the addition of nitrogen by laser …
The effect of three different cone combinations on the performance of laser ablation MC-ICP-
MS (Neptune plus) for the in situ Hf isotope analysis of zircon were investigated. The signal …
MS (Neptune plus) for the in situ Hf isotope analysis of zircon were investigated. The signal …
Oxygen isotopes trace the origins of Earth's earliest continental crust
Much of the current volume of Earth's continental crust had formed by the end of the
Archaean eon (2.5 billion years ago), through melting of hydrated basaltic rocks at depths of …
Archaean eon (2.5 billion years ago), through melting of hydrated basaltic rocks at depths of …
Giant impacts and the origin and evolution of continents
Earth is the only planet known to have continents, although how they formed and evolved is
unclear. Here using the oxygen isotope compositions of dated magmatic zircon, we show …
unclear. Here using the oxygen isotope compositions of dated magmatic zircon, we show …
Mid-Eocene high Sr/Y granites in the Northern Himalayan Gneiss Domes: Melting thickened lower continental crust
L Zeng, LE Gao, K Xie, J Liu-Zeng - Earth and Planetary Science Letters, 2011 - Elsevier
Within the Himalayan collisional belt, granotoids occur along two sub-parallel belts, the
Northern Himalayan Gneiss Domes (NHGD) and the High Himalayan Crystalline Series …
Northern Himalayan Gneiss Domes (NHGD) and the High Himalayan Crystalline Series …