About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
Pub. Id:
First Page:
Last Page:
Book Title:
Article/Chapter:
Subject Group:
Spec. Pub. Type:
Pub. Year:
Author(s):
Abstract:
In Greenland and Arctic Scandinavia, Devonian sedimentary rocks crop out in only two areas: (1) East Greenland between lat. 71 1/2 °N and 74 1/2 °N, and (2) Svalbard (Spitsbergen and possibly Bjornoya).
The strata are nonmarine clastic units, and they are dated largely by their vertebrate fossils.
The Greenland succession has an aggregate thickness of 7,000 m and ranges in age from late Middle Devonian to late Late Devonian. The Spitsbergen succession has an aggregate thickness of 6,500 m and ranges in age from Silurian through early Early Devonian to late Middle Devonian. Both successions overlie deformed Ordovician or older rocks and unconformably underlie Carboniferous or younger rocks.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |