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Detrital Mineral U/Pb Age Dating and Geochemistry of Magmatic Products in Basin Sequences

Dating and geochemical analyses of detrital minerals (mainly zircons) combined with traditional methods, such as heavy minerals and sandstone modes, are a powerful tool in paleogeographic and paleotectonic research and industrial applications.

Salvato in:
Natura: Online
Lingua:inglese
Pubblicazione: MDPI - Multidisciplinary Digital Publishing Institute 2023
Soggetti:
detrital zircon U-Pb geochronology
bulk geochemistry
provenance
tectonic setting
West Bogeda Shan
U-Pb geochronology
detrital zircon
source-to-sink
provenance analysis
mixing model
sediment budgeting
east China seas
Pennsylvanian
Sino-Korean Block
detrital zircons
U–Pb ages
subduction zones
U–Pb dating
sandstone petrography
peripheral bulge
tectonics
zircon U-Pb ages
muscovite 40Ar/39Ar ages
sediment provenance
Yangtze River
detrital-zircon age spectrum
Ereendavaa terrane
Mongol-Okhotsk orogenic belt
opening of the Mongol-Okhotsk ocean
northeastern Mongolia
Lu-Hf isotopes
early Miocene
Yinggehai-Song Hong Basin
South China Sea
stratigraphic thicknesses
net sand to gross thickness ratio
conglomerate percentage
heavy mineral analysis
detrital zircon U‒Pb geochronology
Intermontane basin
Mongolia
laser ablation U-Pb dating
Hafnium isotope-ratio
terrane definition
paleotectonic reconstruction
Western Andes
Miocene
Silante Formation
Ecuador
compositional heterogeneity
major element
nonmarine basin
gejiu basalts
zircon U–Pb dating
geochemistry
Sr–Nd–Pb isotope
petrogenesis
Cameroon
Meiganga
gold placer
trace element
geochronology
Archean-Proterozoic origins
zircon crystal morphology
zircon textures
zircon trace elements
alteration of zircon
REE in zircon
rare metal granites
Li-F granites
Western Hercynian Meseta
Permian basin
Tiddas Souk Es-Sebt des ait ikko volcanic basin
U–Pb geochronology
mineralogy
petrology
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
Accesso online:ONIX_20230220_9783036549545_50
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