1887
PDF

Abstract

In the coastal region of Køge Bugt Maastrichtian chalk and Danian bryozoan limestone form the prequaternary basement. Maastrichtian chalk forms the prequatemary basement along a section of the coastline, while Danian bryozoan limestone inland appears above the chalk. On a regional scale the Maastrichtian/Danian boundary surface dips westwards.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201407366
1997-08-09
2020-11-24
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407366
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error