20151215 · Quartz and K-feldspar luminescence dating of a Marine Isotope Stage 5 megalake in the Juyanze Basin, central Gobi Desert, China December 2015 Palaeogeography Palaeoclimatology Palaeoecology 440:96-109
view moreSemantic Scholar extracted view of "Luminescence dating of K-feldspar from sediments: a protocol without anomalous fading correction" by Bo Li et al.
view more201271 · Highlights We dated the K-feldspar from loess samples at the Luochuan section of the Chinese Loess Plateau. The K-feldspar ages are consistent with independent age control for the samples from L1 to L3. The MET-pIRIR protocol can provide reliable ages for the Chinese loess up to ∼300 ka.
view more2023423 · Feldspar Group Minerals. Feldspar is the name of a large organization of rock-forming silicate minerals that make up over 50% of Earth’s crust. They are discovered in igneous, metamorphic, and sedimentary rocks in all components of the sector. Feldspar minerals have very comparable structures, chemical compositions, and bodily properties.
view more2017216 · Request PDF | Late Quaternary lake evolution in the Gaxun Nur basin, central Gobi Desert, China, based on quartz OSL and K-feldspar pIRIR dating of paleoshorelines | Paleoenvironmental changes in ...
view more20231028 · K-feldspar veins are genetically correlated with lamprophyres, whereas sulfide mineral assemblage and trace element compositions of pyrite in K-feldspar veins suggest that K-feldspar veins in lamprophyres are not directly related to …
view more2018111 · Abstract Feldspar is a valuable raw material in the manufacture of glass, ceramic, fillers, enamel frits, and welding electrodes. Feldspar is the single most abundant mineral in the earth crust ...
view more201881 · K-feldspar pIRIR methods have been successfully used to date loess samples from NE Tibetan Plateau, ranging from few hundred years to ~ 200-300 ka (Wang et al., 2018; E et al., 2018;Li et al ...
view more201821 · Discussion The trace elements in K-feldspar are very useful geochemical indicators to assess not only the differentiation degree but also the potential for rare-metal mineralization in pegmatite. The most key trace elements in K-feldspar are Li, Rb, Cs, Sr, Ba, and P (as P 2 O 5 ).
view more201821 · Semantic Scholar extracted view of "K-feldspar composition as an exploration tool for pegmatite-type rare metal deposits in Altay, NW China" by Yong Tang et al.
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