Rare earth and other trace element mobility during mylonitization: a comparison of the Brevard and Hope Valley shear zones in the Appalachian Mountains, USA

1996 ◽  
Vol 14 (2) ◽  
pp. 213-226 ◽  
Author(s):  
K. C. CONDIE ◽  
A. K. SINHA
2003 ◽  
Vol 214 (1-2) ◽  
pp. 203-219 ◽  
Author(s):  
Yann Rolland ◽  
Stephen Cox ◽  
Anne-Marie Boullier ◽  
Giorgio Pennacchioni ◽  
Neil Mancktelow

1985 ◽  
Vol 49 (350) ◽  
pp. 107-115 ◽  
Author(s):  
J. H. Baker

AbstractZones of albitization 20 m wide are developed in the peraluminous, undeformed Proterozoic Bastfallshöjden granite, W. Bergslagen, central Sweden. During albitization Na, Si, Mg, Ni, Zn, and Ga are added, while Fe2+, Fe3+, Mn, K, Sc, Rb, Cs, Ba, Pb, U, and F are lost, together with the rare earth elements (REE) in decreasing amounts with increasing atomic number. Ti, Al, P, and Y were immobile. Trace element data for chlorites separated from hydrothermally altered country rocks and from a quartz-chlorite vein in the albitized granite show similar REE patterns indicating a common origin: the most altered granite has a similar REE pattern, probably resulting from interaction with the same hydrothermal fluid which produced the chlorites, in which seawater is thought to have been an important constituent.


2010 ◽  
Vol 74 (2) ◽  
pp. 684-704 ◽  
Author(s):  
Stephan König ◽  
Carsten Münker ◽  
Stephan Schuth ◽  
Ambre Luguet ◽  
J. Elis Hoffmann ◽  
...  

2020 ◽  
Vol 2 (8) ◽  
Author(s):  
Dharmendra Kumar Jigyasu ◽  
Munendra Singh ◽  
Sandeep Singh ◽  
Satyendra Singh ◽  
Indra Bir Singh

2019 ◽  
Vol 104 (4) ◽  
pp. 501-513 ◽  
Author(s):  
Georgia Pe-Piper ◽  
Justin Nagle ◽  
David J.W. Piper ◽  
Chris R.M. McFarlane

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