ORBi: Horrent Catherine - Seismic refraction surveys in Bernburg, Germany: an application of the generalized reciprocal and phantoming method

Reference : Seismic refraction surveys in Bernburg, Germany: an application of the generalized recip...


	Document type :	Scientific congresses and symposiums : Paper published in a book
	Discipline(s) :	Engineering, computing & technology : Geological, petroleum & mining engineering
	To cite this reference:	http://hdl.handle.net/2268/14454

Title :	Seismic refraction surveys in Bernburg, Germany: an application of the generalized reciprocal and phantoming method
Language :	English
Author, co-author :	Horrent, Catherine [ > > ]
	Brouyère, Serge [Université de Liège - ULg > Département Argenco : Secteur GEO3 > Hydrogéologie & Géologie de l'environnement >]
	Demanet, Donat [ > > ]
	Michiels, Thierry [ > > ]
	Jongmans, Denis [ > > ]
Publication date :	1997
Main document title :	Modern Geophysics in Engineering Geology
Editor :	McCann, D. M.
	Eddleston, M.
	Fenning, P. J.
	Reeves, G. M.
Publisher :	Geological Society
Collection and collection volume :	Geological Society Engineering Geology Special Publication n°12
Pages :	407-411
On invitation :	No
Audience :	International
ISBN :	1-897799-92-6
City :	London
Country :	United Kingdom
Event name :	Modern Geophysics in Engineering Geology
Event date :	du 12 au 15 septembre 1994
Event organizer :	Université de Liège
Event place (city) :	Liège
Event country :	Belgium
Keywords :	[en] seismis refraction ; generalized reciprocal and phantoming method
Abstract :	[en] The paper presents a case study of a seismic refraction survey in Bernburg, Germany. The interpretation was made using the GRM method and phantoming concept. The aim of the survey was to map the depth of the bed-rock over a distance of 2 km. The survey was divided into five linear profiles ranging from 150 to 640 metres in length. The resulting interpreted sections show substantial variations in velocity (1300 to 4500 m/s) and depth (5 to 18 m) of bed-rock. Correlation with existing boreholes shows that the top of the bed-rock is located with an accuracy of the order of 1 metre.
Target :	Researchers ; Professionals ; Students
Permalink :	http://hdl.handle.net/2268/14454

File(s) associated to this reference

Fulltext file(s):

	File	Commentary	Version	Size	Access
Open access	brouyere2.pdf		Publisher postprint	79.72 kB	View/Open

All documents in ORBi are protected by a user license.

Dspace v1.5