The origin of gypsum in Vertisols in New Caledonia determined by isotopic characteristics of sulphur-Reference-Cited by-同舟云学术

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The origin of gypsum in Vertisols in New Caledonia determined by isotopic characteristics of sulphur

Published:1994-11 Issue:3-4 Volume:63 Page:179-195
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Podwojewski P.,Arnold M.

Publisher

Elsevier BV

Subject

Soil Science

Reference56 articles.

1. Evaporation from soil shrinkage cracks;Adams,1964

2. Evaporation from a simulated soil shrinkage crack;Adams,1969

3. The influence of rock weathering on the genesis of gypsum and carbonate in some australian and zone soils;Akpokodje;Aust. J. Soil Res.,1984

4. East Pacific rise at 21oN;Arnold,1981

5. Isotope geochemistry of sulphur;Ault;Geochim. Cosmochim. Acta,1959

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1. Hydrochemical characteristics and paleoclimate changes recorded from Sugan Lake on the northern boundary of Tibetan Plateau since mid-Holocene;CATENA;2022-10

2. Chapter 9 Mineral resources and prospectivity of non-ultramafic rocks of New Caledonia;Geological Society, London, Memoirs;2020

3. Chapter 7 Post-obduction evolution of New Caledonia;Geological Society, London, Memoirs;2020

4. Morphological, physical, and clay mineralogy of calcareous and gypsiferous soils in North of Lorestan, Iran;Canadian Journal of Soil Science;2019-12-01

5. Vertic Features;Interpretation of Micromorphological Features of Soils and Regoliths;2018

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