Results 171 to 180 of about 11,921 (228)
Recurrence rates of explosive volcanism in paleo-equatorial Pangaea, and implications for climate near the peak late Paleozoic ice age. [PDF]
Pfeifer LS +6 more
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Palaeomagnetic and geochronologic results from lower cretaceous volcanics of the western Qiangtang terrane and implications for the Lhasa-Qiangtang collision. [PDF]
Zhang Y +13 more
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Himalayan "S-type" granite generated from I-type sources. [PDF]
Ding H, Zhang Z, Kohn MJ.
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Magmatic evolution of the Kikai caldera revealed by zircon triple dating and its chemistry. [PDF]
Ito H.
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Redox chemistry of early Earth and the origin of life. [PDF]
Moldogazieva NT +3 more
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Tectonism rather than "snowball Earth" glaciation is responsible for the Great Unconformity. [PDF]
Zhan RR +11 more
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2021
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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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
openaire +1 more source
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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