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Evidence for a regional-scale fluid loss event during mid-crustal metamorphism (1991)

Yardley, Bruce ; Bottrell, Simon H. ; Cliff, R. A.

[s.l.] : Nature Publishing Group

Nature 349 (1991), S. 151-154

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ISSN: 1476-4687

Quelle: Nature Archives 1869 - 2009

Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik

Notizen: [Auszug] The area investigated is in Connemara, western Ireland, where a late Precambrian (Dalradian) succession of sediments has undergone a complex history of folding and metamorphism8, culminating in a low-pressure, high-temperature metamorphism with accompanying folding (D3) that was related to the ...

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1038/349151a0

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Digitale Medien

Metamorphic fluid flow (1991)

YARDLEY, BRUCE ; BOTTRELL, SIMON H. ; CLIFF, R. A.

[s.l.] : Nature Publishing Group

Nature 352 (1991), S. 484-484

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ISSN: 1476-4687

Quelle: Nature Archives 1869 - 2009

Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik

Notizen: [Auszug] YARDLEY ET AL. REPLY - The differences between our interpretation of regional fluid flow through the Connemara marble and Tanner's arise through differences in our maps; oversimplifications that inevitably accompany a short article; and because of differences in interpretation of the relative ...

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1038/352484a0

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Digitale Medien

Redistribution of uranium by physical processes during weathering and implications for radon production (1993)

Bottrell, Simon H.

Springer

Environmental geochemistry and health 15 (1993), S. 21-25

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ISSN: 1573-2983

Quelle: Springer Online Journal Archives 1860-2000

Thema: Geologie und Paläontologie , Medizin

Notizen: Abstract Erosion of the Edale shales of Derbyshire during the Tertiary and Quaternary has resulted in sediment deposits in and on the underlying karstified limestones. Sorting during sedimentation has generated clay-rich sediments which are uranium enriched due to a clay association of uranium in the shales. Radon production in these sediments is at or close to equilibrium with their uranium content, and their fine grain-size ensures efficient radon release. Such sediments are therefore potent local sources of environmental radon.

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1007/BF00146289

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