Rare earth elements as indicators of groundwater environment changes in a fractured rock system: evidence from fracture-filling calcite

Author:

Lee Seung-Gu,Lee Dae-Ha,Kim Yongje,Chae Byong-Gon,Kim Won-Young,Woo Nam-Chil

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference27 articles.

1. The nature of groundwater flow in fractured rock: evidence from the isotopic and chemcal evolution of recryastallized fracture calcites from the Canadian Precambrian Shield;Bottomley;Geochim. Cosmochim. Acta,1992

2. Brookins, D. J., 1989. Aqueous geochemistry of rare earth elements. In Lipin, B. R. and Mckay, G. A. (Eds), Geochemistry and Mineralogy of Rare Earth Elements. Mineral. Soc. Am., pp. 201–225 (Chapter 8).

3. Rare earth element complexation by carbonate and oxalateions;Cantrell;Geochim. Cosmochim. Acta,1987

4. Carlos, B. A., Chipera, S. J., Bish D. L., 1995. Calcite and zeolite fracture coatings in Topopah Spring Tuff along Drill Hole wash, Yucca Mountain, Nevada. In: Proc. 6th Internat. Conf. High Level Radioactive Waste Management, pp. 100–102.

5. Identification of conductive Fractures in Cryatalline Rocks;Chae;J. Korean Soc. Groundwater Env.,1998

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