Provenance and Tectonic Evolution of the Kongtongshan Formation Conglomerate in Southwest Ordos Basin, China. [PDF]
Cui L, Nan Q, Zhou W, Song L, Zhang H.
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Fossil wood cells recorded 300 million years of Europe's tectonic history. [PDF]
Trümper S +10 more
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Formation Mechanism and Variability of Tight Sandstone Reservoirs under Multi-Provenance Convergence: A Case Study of the Second Member of the Upper Triassic Xujiahe Formation in the Northeastern Sichuan Basin. [PDF]
Pu Q +8 more
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Collision Timing and Provenance Shifts from the Late Oligocene to Middle Miocene in the Southeasternmost Zagros Orogen. [PDF]
GholamiZadeh P +5 more
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Protracted late Paleozoic volcanic arc activity along the Northeast Asian continental margin. [PDF]
Kim HS +6 more
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Late Cretaceous-Paleogene Exhumation History and Evolution of Paleotopography in the Gaize Basin, Central Tibet. [PDF]
Gao Y +5 more
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Chang'e-6 farside anorthosites indicate hemispherically comparable magma ocean solidification. [PDF]
Wang Z +17 more
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Bias in detrital zircon geochronology and thermochronometry [PDF]
Abstract 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 geochronology and processes in accretionary wedges
Earth-Science Reviews, 2020Abstract The detrital zircon U–Pb geochronology has been widely employed to analyze accretionary wedges over the past decade. The goal of this paper is, first, to briefly review this rapidly growing field of research and then to explore the exciting potential of the detrital zircon geochronology for interpreting processes in accretionary wedges.
Jiří Žák +2 more
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Detrital zircon reference for the North China block
Journal of Asian Earth Sciences, 2006Abstract U–Pb analyses of 250 single detrital zircons from Upper Proterozoic to Ordovician strata collected from the Zhuozi Shan in north-central China provide a detrital zircon reference for the North China block, a major crustal entity in the Asian tectonic collage.
George E. Gehrels, Brian J Darby
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