Determination of regolith production rates from 238U-234U-230Th disequilibrium in deep weathering profiles (Longnan, SE China)-Reference-Cited by-同舟云学术

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Determination of regolith production rates from 238U-234U-230Th disequilibrium in deep weathering profiles (Longnan, SE China)

Published:2021-07 Issue: Volume:574 Page:120241
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Jia Guo-Dong,Chabaux François,Van der Woerd Jérôme,Pelt Eric,di Chiara Roupert Raphaël,Ackerer Julien,Zhao Zhi-Qi,Yang Ye,Xu Sheng,Liu Cong-Qiang

Funder

CNRS

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference70 articles.

1. Regolith evolution on the millennial timescale from combined U–Th–Ra isotopes and in situ cosmogenic 10Be analysis in a weathering profile (Strengbach catchment, France);Ackerer;Earth Planet. Sci. Lett.,2016

2. Geomorphology: The Mechanics and Chemistry of Landscapes;Anderson,2010

3. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements;Balco;Quat. Geochronol.,2008

4. Global Environment Water, Air, and Geochemical Cycles Prentice-Hall. Englewood Cliffs, NewJersey;Berner,1996

5. Burial of organic carbon and pyrite sulfur in sediments over Phanerozoic time: a new theory;Berner;Geochim. Cosmochim. Acta,1983

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