Sorensen, Henning (1986) Clay minerals — a physico-chemical explanation of their occurrence. Geoderma, 37 (3). 261-263 doi:10.1016/0016-7061(86)90057-1
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Clay minerals — a physico-chemical explanation of their occurrence | ||
Journal | Geoderma | ||
Authors | Sorensen, Henning | Author | |
Year | 1986 (July) | Volume | 37 |
Issue | 3 | ||
Publisher | Elsevier BV | ||
DOI | doi:10.1016/0016-7061(86)90057-1Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 12842468 | Long-form Identifier | mindat:1:5:12842468:3 |
GUID | 0 | ||
Full Reference | Sorensen, Henning (1986) Clay minerals — a physico-chemical explanation of their occurrence. Geoderma, 37 (3). 261-263 doi:10.1016/0016-7061(86)90057-1 | ||
Plain Text | Sorensen, Henning (1986) Clay minerals — a physico-chemical explanation of their occurrence. Geoderma, 37 (3). 261-263 doi:10.1016/0016-7061(86)90057-1 | ||
In | (1986, July) Geoderma Vol. 37 (3) Elsevier BV |
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