Rates of Biotite Weathering, and Clay Mineral Transformation and Neoformation, Determined from Watershed Geochemical Mass-Balance Methods for the Coweeta Hydrologic Laboratory, Southern Blue Ridge Mountains, North Carolina, USA-Reference-Cited by-同舟云学术

Rates of Biotite Weathering, and Clay Mineral Transformation and Neoformation, Determined from Watershed Geochemical Mass-Balance Methods for the Coweeta Hydrologic Laboratory, Southern Blue Ridge Mountains, North Carolina, USA

Published:2013-03-16 Issue:2-3 Volume:20 Page:203-224
ISSN:1380-6165
Container-title:Aquatic Geochemistry
language:en
Short-container-title:Aquat Geochem

Author:

Price Jason R.,Velbel Michael A.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s10498-013-9190-y.pdf

Reference84 articles.

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2. Aubert D, Stille P, Probst A (2001) REE fractionation during granite weathering and removal by waters and suspended loads: Sr and Nd isotopic evidence. Geochim Cosmochim Acta 65:387–406

3. Banfield JF, Eggleton RA (1988) A transmission electron microscope study of biotite weathering. Clays Clay Miner 36:47–60

4. Basham IR (1974) Mineralogical changes associated with deep weathering of gabbro in Aberdeenshire. Clay Miner 10:189–202

5. Berner RA, Berner EK (1997) Silicate weathering and climate. In: Ruddiman WF (ed) Tectonic uplift and climate change. Plenum Press, New York, pp 353–365

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