Paleogeography of the southwestern Ordos Basin and exhumation history of the Liupan Shan area. [PDF]
Liu F, Wang M.
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Spatio-temporal constraints on thrusting across fold-and-thrust belts worldwide. [PDF]
Curzi M, Billi A, Carminati E, Tavani S.
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Extremely rapid, yet noncatastrophic, preservation of the flattened-feathered and 3D dinosaurs of the Early Cretaceous of China. [PDF]
MacLennan SA +9 more
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Constraints of middle-late Permian granites in Eastern Inner Mongolia on the final subduction of the Paleo Asian Ocean. [PDF]
Zhao C, Yu Y, Liu Y, Cai H, He J, Gao X.
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Provenance Analysis in the Nima Basin during Paleogene and Its Implications for the Decline of the Tibetan Central Valley. [PDF]
Luo Y, Mi W, Gao Y, Qin L.
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We present U-Pb, Lu-Hf, and O isotopic data, as well as size-shape data for approximately 3700 detrital zircons from 15 European rivers. In combination with geomorphological information for each river basin (area, drainage length, and hypsometric curves), we evaluate the representativeness and biases affecting such datasets.
Castillo , Paula +4 more
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Mineral inclusion assemblage and detrital zircon provenance
Chemical Geology, 2018Abstract Mineral inclusions are common in magmatic zircon and a potentially rich source of petrologic information. Controls on the relative proportions of inclusion phases, specifically early-crystallizing minerals such as apatite and late-crystallizing phases such as quartz, K-feldspar, and muscovite, have not been systematically studied.
Elizabeth A. Bell +3 more
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Bias in detrital zircon geochronology and thermochronometry
Chemical Geology, 2013Abstract Detrital studies that utilize zircon U–Pb geochronology and fission-track (FT) thermochronometry are subject to a range of potential sources of bias that should be properly evaluated and minimized. Some of them are common to any single-grain mineral analysis (e.g., variable bedrock mineral fertility, hydraulic sorting during transport ...
MALUSA', MARCO GIOVANNI +4 more
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Detrital zircon evidence for the antiquity of Taiwan
Geosciences Journal, 2009In-situ U-Pb geochronology and Hf isotopic studies of zircons from the Pre-Tertiary basement complex and Eocene rocks of the Central Range of Taiwan were carried out to elucidate the history of detrital zircons older than 2.3 Ga. Zircons from the eastern Backbone Range and Eastern Central Range show Paleoproterozoic to late Neoarchean ages (2.3−≥2.5 Ga)
Ching-Ying Lan +10 more
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