Geology of and climatic indicators in the Westphalian A New Glasgow formation, Nova Scotia, Canada: implications for the genesis of coal and of sandstone-hosted lead deposits

By the Late Carboniferous, Late Paleozoic northward drift of the continent Laurentia had carried Nova Scotia from the southern dry climate belt into the equatorial rainy belt. Carboniferous amalgamation of Laurentia with the southern continent Gondwana enclosed the area within the new supercontinent...

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Bibliographic Details
Published in:Atlantic Geology
Main Author: Chandler, F. W.
Format: Article in Journal/Newspaper
Language:English
Published: Atlantic Geoscience Society 1998
Subjects:
Online Access:https://journals.lib.unb.ca/index.php/ag/article/view/2039