Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geology; December 2005; v. 33; no. 12; p. 953-956; DOI: 10.1130/G21720.1
© 2005 Geological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
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 Connelly, J. N.
Right arrow Articles by Thrane, K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Rapid determination of Pb isotopes to define Precambrian allochthonous domains: An example from West Greenland

James N. Connelly*,1 and Kristine Thrane*,2

1 Jackson School of Geosciences, University of Texas at Austin, 1 University Station, Austin, Texas 78712, USA
2 Geological Institute, University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen, Denmark

Lacking provincial fauna, establishing autochthoneity or allochthoneity of domains in Precambrian orogens typically requires comparison of precollisional attributes across suspect terrane boundaries. We have measured the Pb isotopic compositions of K-feldspar grains in epoxy mounts and rock slabs by a rapid laser ablation–inductively coupled plasma mass spectrometry method with sufficient precision and accuracy to define two large Pb isotopic domains in the Paleoproterozoic Nagssugtoqidian-Rinkian orogen of West Greenland. These domains are interpreted to correlate with and help delineate the Rae and North Atlantic cratons. Their boundary coincides with a recently proposed location of the main collisional suture of this orogen, thus supporting this interpretation. This study validates a rapid analytical Pb isotopic method that will be useful in addressing a range of problems that requires knowledge of crustal affinity in Precambrian terrains.

Key Words: West Greenland • Pb isotopes • Nagssugtoqidian • Rinkian • North Atlantic • laser ablation • ICP-MS




This article has been cited by other articles:


Home page
Geological Society, London, Special PublicationsHome page
M. R. St-Onge, J. A. M. Van Gool, A. A. Garde, and D. J. Scott
Correlation of Archaean and Palaeoproterozoic units between northeastern Canada and western Greenland: constraining the pre-collisional upper plate accretionary history of the Trans-Hudson orogen
Geological Society, London, Special Publications, January 1, 2009; 318(1): 193 - 235.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
F. C. Ramos and F. J. Tepley III
Inter- and Intracrystalline Isotopic Disequilibria: Techniques and Applications
Reviews in Mineralogy and Geochemistry, January 1, 2008; 69(1): 403 - 443.
[Full Text] [PDF]


Home page
GeologyHome page
S. Tyrrell, P.D.W. Haughton, and J.S. Daly
Drainage reorganization during breakup of Pangea revealed by in-situ Pb isotopic analysis of detrital K-feldspar
Geology, November 1, 2007; 35(11): 971 - 974.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of America