Paleozoic carbonatites controlled rare-earth-elements mineralization at Bayan Obo. [PDF]
Li Y +5 more
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Pervasive impact modification of pristine lunar clasts. [PDF]
Barboni M +4 more
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Abiotic synthesis during the interaction of ferrous chloride-rich silicic fluids with marble under high-grade metamorphic conditions. [PDF]
Fei C, Guo S, Li Y, Liu J.
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Magnetostratigraphic constraints on the late Ediacaran paleomagnetic enigma. [PDF]
Pierce JS +13 more
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A two-stage mantle plume-sagduction origin of Archean continental crust revealed by water and oxygen isotopes of TTGs. [PDF]
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Petrological diversity of continental arc magmatism evidenced by Triassic magmatic complexes in East Kunlun Orogen. [PDF]
Gan J +6 more
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Orogeny and topography influenced Jurassic-Cretaceous terrestrial ecosystem evolution in northeastern Asia. [PDF]
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Evidence of slab tearing on an inherited Mesozoic rift transfer fault in the Betic Cordillera. [PDF]
Pedrera A +13 more
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The south margin of the central Altyn is an early paleozoic tectonic unit confirmed by Zircon dating evidence. [PDF]
Ma T, Liu L, Zhang S, Gai Y, Zhai M.
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Interpretation of discordant U‐Pb zircon ages: An evaluation
Journal of Metamorphic Geology, 1997The most widely used technique for the determination of high precision mineral growth ages in igneous and metamorphic rocks is dating of zircons with the U‐Pb method. The interpretation of these ages, particularly in metamorphic settings, is hampered by an incomplete understanding of the common phenomenon of partial Pb‐loss in zircon.
Mezger, Klaus, KROGSTAD, E. J.
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