The Upper Cretaceous succession (Cenomanian­ Santonian) of the Staffhorst Shaft, Lower Saxony, northern Germany: integrated biostratigraphic, lithostratigraphic and downhole geophysical log data

Volume: 49, Issue: 3, Pages: 175 - 213
Published: Jan 1, 1999
Abstract
The Cenomanian to Santonian succession of the Staffhorst shaft, ca. 50 km south of Bremen, because of its structural position in the northern German Upper Cretaceous basin, is intermediate in character and fossil content between the pelagic sediments characterizing the Pompeckj Block in the north and the proximal sediments of the Lower Saxony Block in the south. The biostratigraphic subdivision of the shaft is based on inoceramids, echinoids,...
Paper Details
Title
The Upper Cretaceous succession (Cenomanian­ Santonian) of the Staffhorst Shaft, Lower Saxony, northern Germany: integrated biostratigraphic, lithostratigraphic and downhole geophysical log data
Published Date
Jan 1, 1999
Volume
49
Issue
3
Pages
175 - 213
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