Data for: Mo isotope fractionation in collisional Magmatic-Hydrothermal systems

Published: 18 March 2024| Version 1 | DOI: 10.17632/xg9f46g8sv.1
Contributor:
Nan Qi

Description

Data for: Mo isotope fractionation in collisional Magmatic-Hydrothermal systems

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Steps to reproduce

Molybdenite was dissolved in heated to 80°C in 6ml of ultrapure aqua regia for 12 hours. The solutions were dried and a 100 ppb solution was prepared by adding 0.5molar nitric acid to the salts and diluting. A 1 ppm Mo double spike was added to the rock powders as part of a two-step dissolution process. A 100 mg aliquot of rock powder was dissolved in heated 3 ml of HF for 12 hours and dried, 6ml of aqua regia was added to the dried salts, and dissolution of all the material was confirmed visually.

Institutions

Northwest University

Categories

Geochemistry

Funding

National Natural Science Foundation of China

42202073

National Natural Science Foundation of China

42122014

National Natural Science Foundation of China

41630313

China Postdoctoral Science Foundation

2022M722566

Licence