Allanite and epidote weathering at the Coweeta Hydrologic Laboratory , western North Carolina

@inproceedings{US2006AllaniteAE,
  title={Allanite and epidote weathering at the Coweeta Hydrologic Laboratory , western North Carolina},
  author={A. U.S. and Jason and Price and Michael Anthony Velbel and Lina C. Patino},
  year={2006}
}
Allanite and epidote occur in the parent rocks of weathered regolith at the Coweeta Hydrologic Laborato~y in North Carolina and exhibit different responses to weathering. Petrographically, epidote and allanite are identical at Coweeta, and only with additional analytical techniques (e.g., EDS or LAICP-MS) can the two be distinguished. Allanite is more abundant in unweathered bedrock but weathers readily below the weathering front. In contrast, the much less abundant epidote persists into the… CONTINUE READING

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