Ground Water Problems 1968
DOI: 10.1016/b978-0-08-003468-3.50006-9
|View full text |Cite
|
Sign up to set email alerts
|

Ground Water in Precambrian Rocks in Southern Sweden

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

1973
1973
2007
2007

Publication Types

Select...
2
2

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(1 citation statement)
references
References 4 publications
0
1
0
Order By: Relevance
“…Also, points representing the intersection of two deep seated lineaments are more-favourable sites for groundwater accumulation than points representing the intersection of short (shallow) lineaments. This situation has been proved in the Pre-Cambrian rocks of southern Sweden (Larsson, 1968) where it was shown that open, long fractures tend to drain large volumes to bedrock, with corresponding high yield. On the other hand, close short joints and faults contain small amounts of water.…”
Section: Resultsmentioning
confidence: 90%
“…Also, points representing the intersection of two deep seated lineaments are more-favourable sites for groundwater accumulation than points representing the intersection of short (shallow) lineaments. This situation has been proved in the Pre-Cambrian rocks of southern Sweden (Larsson, 1968) where it was shown that open, long fractures tend to drain large volumes to bedrock, with corresponding high yield. On the other hand, close short joints and faults contain small amounts of water.…”
Section: Resultsmentioning
confidence: 90%