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.
Main Authors: | , , , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
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 |
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. |
---|