High-Precision Zircon SIMS Zr Isotope Analysis

Author(s):  
Sheng He ◽  
Yang Li ◽  
Li-Guang Wu ◽  
Dong-Fa Guo ◽  
Zi-Ying Li ◽  
...  

Zirconium isotope is a very promising tracer to investigate magmatic processes such as magma crystallization and differentiation, and to tackle the secular evolution of continental crust. With zircon being its...

2020 ◽  
Vol 545 ◽  
pp. 119648 ◽  
Author(s):  
Jing-Jing Fan ◽  
Jie Li ◽  
Qiang Wang ◽  
Le Zhang ◽  
Jing Zhang ◽  
...  

2021 ◽  
Author(s):  
Jean Milot ◽  
Janne Blichert-Toft ◽  
Chloé Malod-Dognin ◽  
Philippe Telouk ◽  
Mariano Ayarzagüena Sanz ◽  
...  

2021 ◽  
Author(s):  
Mitsuru Suzuki ◽  
Tsuyoshi Iizuka ◽  
Kota Yamamoto ◽  
Takafumi Hirata

Author(s):  
Hai-Ou Gu ◽  
Sun He

This study presents a method for high-precision stable potassium (K) isotope analysis using Multi-Collector Inductively Coupled Plasma Mass Spectrometry (MC-ICPMS) without collision cell in low resolution mode. Cold plasma technique...


1999 ◽  
Vol 63 (5) ◽  
pp. 687-702 ◽  
Author(s):  
Jens Fiebig ◽  
Uwe Wiechert ◽  
Douglas Rumble ◽  
Jochen Hoefs

2008 ◽  
Vol 418 (1) ◽  
pp. 178-183 ◽  
Author(s):  
I. V. Chernyshev ◽  
I. V. Vikent’ev ◽  
A. V. Chugaev ◽  
K. N. Shatagin ◽  
V. P. Moloshag

Mineralogia ◽  
2011 ◽  
Vol 42 (1) ◽  
pp. 53-61 ◽  
Author(s):  
Andrzej Pelc ◽  
Stanisław Hałas ◽  
Robert Niedźwiedzki

Oxygen isotope analysis of shark teeth phosphates from Bartonian (Eocene) deposits in Mangyshlak peninsula, Kazakhstan We report the results of high-precision (±0.05‰) oxygen isotope analysis of phosphates in 6 teeth of fossil sharks from the Mangyshlak peninsula. This precision was achieved by the offline preparation of CO2 which was then analyzed on a dual-inlet and triple-collector IRMS. The teeth samples were separated from Middle- and Late Bartonian sediments cropping out in two locations, Usak and Kuilus. Seawater temperatures calculated from the δ18O data vary from 23-41°C. However, these temperatures are probably overestimated due to freshwater inflow. The data point at higher temperature in the Late Bartonian than in the Middle Bartonian and suggest differences in the depth habitats of the shark species studied.


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