1887

Abstract

The current subway network of Vienna should be expanded to the south. For the planning it was necessary to drill several exploratory wells along possible corridors. In one of these exploratory wells gas was encountered in a 20 cm thick sand layer at a depth of 38 m below ground elevation. The gas bearing layer consists mainly of sand and gravel and might be part of braided stream deposits of Pannon D. In the course of this research project the lateral extension of this gas bearing layer should be mapped. Considering the resolution potential of seismic reflection at these depths and the strong velocity/density contrast the gas bearing sand would provide we decided to use this geophysical method for delineating the lateral extension of the gas bearing horizon.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20130708
2013-06-10
2020-08-05
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20130708
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