Answers are grounded in this paper and cite their sources.
Assessment of granite fertility indicators and geochemical properties in Nonggeori Granite, suggesting exploration for rare elements.
This paper provides a whole-rock geochemical dataset (major oxides and trace elements, 57 analytes) and derived granite fertility indicators for the Precambrian Nonggeori Granite exposed in the Taebaek-Sangdong metallogenic belt (Northeastern Yeongnam Massif, South Korea).Two representative samples (NG1 and NG2) were collected from the pluton, powdered (<105 μm), and analyzed at Activation Laboratories Ltd., using lithium borate fusion or four-acid digestion followed by inductively coupled plasma optical emission spectrometry, inductively coupled plasma mass spectrometry, and fluoride ion selective electrode measurements.The samples are high-silica leucogranites (SiO 2 , 73.30-74.08wt.%) with low MgO (0.17-0.38 wt.%), CaO (0.44-0.62 wt.%), and Fe 2 O 3 (T) (1.47-1.69wt.%).Both samples are peraluminous with Al 2 O 3 /(Na 2 O+K 2 O+CaO)≈1.30.Trace-element signatures include elevated Rb (313-341 ppm), Cs (19.8-23.1 ppm), and Sn (12-19 ppm) and low Nb/Ta (3.87-4.44),collectively suggesting an evolved granite with a rare-metal affinity.When compared with 15 published criteria for Li-Sn-bearing fertile granites, NG1 satisfies 11 indicators whereas NG2 satisfies five indicators, implying significant intra-pluton heterogeneity in fractionation and fertility signals.The dataset can serve as baseline information for screening fertile zones within the Nonggeori Granite and for vectoring exploration toward rare-element (lithium-cesium-tantalum type) pegmatites, as well as for designing follow-up mineral-chemical and geochronological studies.
No takes yet. Share an insight, caveat, or question.
Lee et al. (2026) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: