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U-Pb isotope ratios and trace element concentrations of carbonate-fluorapatit...
These data are trace element concentrations and U-Pb isotope ratios from phosphate nodules in Carboniferous-age carbonates, shales and phosphorites in Co. Clare, western... -
U-Pb isotopy data of deformed samples from the Yushu mélange, western Jinsha ...
Deformed samples from the Yushu mélange, in the western Jinsha Suture, have been dated by U-Pb isotopy on zircons. This dataset presents U-Pb isotopy data obtained for these... -
Secondary ion mass spectrometry (SIMS) Uranium-Lead analyses of shock-recryst...
U-Pb data for shock-recrystallised zircon from the Lappajärvi impact crater, Finland. Discordance here refers to the calculated difference between the ²⁰⁶Pb/²³⁸U age and the... -
Detrital zircon geochronology data, petrographic point count data and paleocu...
Triassic turbidites of the Nanpanjiang basin of south China represent the most expansive and voluminous siliciclastic turbidite accumulation in south China. The Nanpanjiang... -
(Table 1) Lead, thorium and uranium isotopic concentration and ages of zircon...
Reconstruction of the geologic history of the Yenisey Ridge, which developed as an accretionary collision orogen on the western margin of the Siberian craton is essential to... -
(Table 1) Lead isotope ratios of zircons from sample 122 of ODP Hole 153-922A
According to the theory of plate tectonics, rocks found in the vicinity of mid-ocean ridges - where oceanic plates are created - should be relatively young (at most several Myr... -
Appendix A: LA-ICP-MS results (Laser-ablation inductively coupled plasma mass...
Three samples of garnet-kyanite paragneiss from the Variscan Ulten Zone (Northern Italy) were studied in detail for U-Th-Pb monazite dating. Monazite in these gneisses is... -
U-Pb, trace element, and Hf isotope analysis for Macquarie Island detrital zi...
Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the... -
Table A1 LA-ICP-MS zircon U-Pb data of Laoniushan granitoids
The NWW-striking Qinling Orogen formed in the Triassic by collision between the North China and Yangtze Cratons. Triassic granitoid intrusions, mostly middle- to high-K,... -
Table 1: U-Pb analyses of zircons and monazites of paragneisses which belong ...
Samples of high grade metamorphic basement rocks of Wilson Terrane cropping out in the Deep Freeze Range and on Kay Island were collected during GANOVEX VI to study their... -
Tab. 1: Zircon isotopic data and rock ages from the Antarctic Peninsula
Morphological and U-Pb isotope studies on sedimentary zircons reflect the orogenic evolution of their former host rocks. The orogenic history of detrital zircons from the... -
Tab. 1: U-Pb analyses of zircons from rock samples in MT. Newton and Cumpston...
We present new U-Pb zircon (SHRIMP) data on rocks from Mt Newton and Cumpston Massif in the southern Prince Charles Mountains. Our data demonstrate that Mt Newton was affected... -
(Table 1) U-Pb isotopic results of single-grain zircon and monazite analyses,...
At Elan Bank of the Kerguelen Plateau in the southeast Indian Ocean, Leg 183 of the Ocean Drilling Program recovered clasts of garnet-biotite gneiss in a fluvial conglomerate... -
U-Pb (zircon) geochronologic analyses for rocks of the Transantarctic Mountai...
The Byrd Glacier discontinuity us a major boundary crossing the Ross Orogen, with crystalline rocks to the north and primarily sedimentary rocks to the south. Most models for... -
Thorium, Uranium and Lead isotopic and geochronologic data for zircon crystal...
Individial CA-TIMS ages of analyses in red were excluded from the final age calculation.(a) z1, z2 etc. are labels for single zircon grains or fragments annealed and chemically... -
U-Th-Pb isotope and age determinations on sample Strieg5
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U-Th-Pb isotope and age determinations on sample Strieg4
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U-Th-Pb isotope and age determinations on sample S2
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U-Th-Pb isotope and age determinations on sample P1
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U-Th-Pb isotope and age determinations on sample Leit8
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