RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD

A Rb-Sr whole rock isochron has yielded an age of 3000 m.y. for the infracrustal rocks occurring in Flyverfjord, East Greenland. This age is further evidence for the presence of Precambrian basement rocks occurring in the East Greenland Caledonian fold belt.

Bibliographic Details
Main Authors: Scoresby Sund, East Greenland, David C. Rex, Andrew Gledhill, Department Of Earth Sciences
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Flyverfjord
Greenland
East Greenland
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560
http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf
Description
Summary:A Rb-Sr whole rock isochron has yielded an age of 3000 m.y. for the infracrustal rocks occurring in Flyverfjord, East Greenland. This age is further evidence for the presence of Precambrian basement rocks occurring in the East Greenland Caledonian fold belt.

Similar Items