Caledonian basement in NW Wedel Jarlsberg Land

ABSTRACT: The area of NW Wedel Jarlsberg Land south of Bellsund (Spitsbergen), be− tween Dunderbukta in the west and the Berzeliustinden mountain group in the east, consists of five fault−bounded blocks: (1) the Renardbreen Block (Middle–Late Proterozoic base− ment rocks), (2) the Chamberlindalen Bl...

Full description

Bibliographic Details
Main Authors: South Of Bellsund, Krzysztof Birkenmajer, Berzeliustinden Block (late Proterozoic, Early Ordovician
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Key words
Arctic
Spitsbergen
Middle/Upper Proterozoic
Cambrian
Ordovician
Cale− donian basement
Bellsund
Berzeliustinden
Chamberlindalen
Dunderbukta
Martinfjella
Renardbreen
Wedel Jarlsberg Land
Wedel-Jarlsberg
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.545.9423
http://www.polish.polar.pan.pl/ppr25/ppr25-003.pdf
Description
Summary:ABSTRACT: The area of NW Wedel Jarlsberg Land south of Bellsund (Spitsbergen), be− tween Dunderbukta in the west and the Berzeliustinden mountain group in the east, consists of five fault−bounded blocks: (1) the Renardbreen Block (Middle–Late Proterozoic base− ment rocks), (2) the Chamberlindalen Block (Late Proterozoic basement rocks), (3) the Martinfjella Block (Late Proterozoic through Early Ordovician basement rocks), (4) the

Similar Items