18 results on '"Tian, Heng-Ci"'
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2. First classification of iron meteorite fragment preserved in Chang’e-5 lunar soils
3. Reassessing the classification of Chang'e-5 basalts using pyroxene composition
4. Potassium isotopic fractionation during multistage alteration of oceanic crust in the southern Mariana Trench
5. Geochemistry of impact glasses in the Chang’e-5 regolith: Constraints on impact melting and the petrogenesis of local basalt
6. Multi-mode chemical exchange in seafloor alteration revealed by lithium and potassium isotopes
7. Lithium isotope fractionation during magmatic differentiation and hydrothermal processes in post-collisional adakitic rocks
8. Quantitative verification of 1:35 diluted fused glass disks with 10 mg sample sizes for the wavelength-dispersive X-ray fluorescence analysis of the whole-rock major elements of precious geological specimens
9. Tracing carbonate dissolution in subducting sediments by zinc and magnesium isotopes
10. Barium isotope evidence for recycled crustal materials in the mantle source of continental basalts
11. Iron, magnesium, and titanium isotopic fractionations between garnet, ilmenite, fayalite, biotite, and tourmaline: Results from NRIXS, ab initio, and study of mineral separates from the Moosilauke metapelite
12. Large Mg Fe isotope fractionation in volcanic rocks from northeast China: The role of chemical weathering and magma compositional effect
13. Diffusion-driven extreme Mg and Fe isotope fractionation in Panzhihua ilmenite: Implications for the origin of mafic intrusion
14. Approach to trace hidden paleo-weathering of basaltic crust through decoupled Mg Sr and Nd isotopes recorded in volcanic rocks
15. Melt inclusions in phenocrysts track enriched upper mantle source for Cenozoic Tengchong volcanic field, Yunnan Province, SW China
16. Low δ26Mg volcanic rocks of Tengchong in Southwestern China: A deep carbon cycle induced by supercritical liquids
17. Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts
18. Origin of low δ26Mg basalts with EM-I component: Evidence for interaction between enriched lithosphere and carbonated asthenosphere
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