Article Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite
Jillian F. Banfield, Takashi Murakami
1998
Banfield, Jillian F. and Murakami, Takashi. "Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite" American Mineralogist, vol. 83, no. 3-4, 1998, pp. 348-357. https://doi.org/10.2138/am-1998-3-419
Banfield, J. & Murakami, T. (1998). Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite. American Mineralogist, 83(3-4), 348-357. https://doi.org/10.2138/am-1998-3-419
Banfield, J. and Murakami, T. (1998) Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite. American Mineralogist, Vol. 83 (Issue 3-4), pp. 348-357. https://doi.org/10.2138/am-1998-3-419
Banfield, Jillian F. and Murakami, Takashi. "Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite" American Mineralogist 83, no. 3-4 (1998): 348-357. https://doi.org/10.2138/am-1998-3-419
Banfield J, Murakami T. Atomic-resolution transmission electron microscope evidence for the mechanism by which chlorite weathers to 1:1 semi-regular chlorite-vermiculite. American Mineralogist. 1998;83(3-4): 348-357. https://doi.org/10.2138/am-1998-3-419
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