Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
  Journal of the Geological Society   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Journal of the Geological Society; October 1992; v. 149; no. 5; p. 689-692; DOI: 10.1144/gsjgs.149.5.0689
© 1992 Geological Society of London
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by HOLE, M. J.
Right arrow Articles by STILL, J.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Mobility of the high field strength, rare earth elements and yttrium during late diagenesis

M. J. HOLE, N. H. TREWIN and J. STILL

Department of Geology and Petroleum Geology, University of Aberdeen, Meston Building, Aberdeen AB9 2UE, UK

Authigenic titanite occurs as a secondary, pore-filling cement in the Permian sandstones of the Cock of Arran, Scotland. The titanite is apparently not associated with in situ alteration of a specific mineral phase or phases, suggesting it crystallized from fluids migrating through these porous and permeable sandstones. The titanite contains significant concentrations of Zr, Nb, P, Ce, Nd, Gd and Y, implying that these elements were also carried in solution, probably in the form of halogen or carbonate complexes associated with hydrothermal circulation related to the intrusion of the adjacent Northern Granite.




This article has been cited by other articles:


Home page
 Geological Society of America BulletinHome page
C. P. North, M. J. Hole, and D. G. Jones
Geochemical correlation in deltaic successions: A reality check
Geological Society of America Bulletin, May 1, 2005; 117(5-6): 620 - 632.
[Abstract] [Full Text] [PDF]

Home page
 American MineralogistHome page
A. R. Chakhmouradian
Crystal chemistry and paragenesis of compositionally unique (Al-, Fe-, Nb-, and Zr-rich) titanite from Afrikanda, Russia
American Mineralogist, November 1, 2004; 89(11-12): 1752 - 1762.
[Abstract] [Full Text] [PDF]

Home page
 Economic GeologyHome page
A. J. McCready, E. F. Stumpfl, J. H. Lally, M. Ahmad, and R. D. Gee
Polymetallic Mineralization at the Browns Deposit, Rum Jungle Mineral Field, Northern Territory, Australia
Economic Geology, March 1, 2004; 99(2): 257 - 277.
[Abstract] [Full Text] [PDF]

Home page
 Proceedings of the Yorkshire Geological SocietyHome page
D. S. Wray and C. J. Wood
Distinction between detrital and volcanogenic clay-rich beds in Turonian-Coniacian chalks of eastern England
Proceedings of the Yorkshire Geological Society, May 1, 1998; 52(1): 95 - 105.
[Abstract] [PDF]

Home page
 Journal of the Geological SocietyHome page
J. E. Bouch, M. J. Hole, N. H. Trewin, and A. C. Morton
Low-temperature aqueous mobility of the rare-earth elements during sandstone diagenesis
Journal of the Geological Society, November 1, 1995; 152(6): 895 - 898.
[Abstract] [PDF]

Home page
 Journal of the Geological SocietyHome page
R. A. BATCHELOR and L. JEPPSSON
Late Llandovery bentonites from Gotland, Sweden, as chemostratigraphic markers
Journal of the Geological Society, October 1, 1994; 151(5): 741 - 746.
[Abstract] [PDF]


JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2010 by Geological Society of London