2021
DOI: 10.1007/s10933-021-00205-w
|View full text |Cite
|
Sign up to set email alerts
|

Waterborne GPR mapping of stratigraphic boundaries and turbidite sediments beneath the bottom of Lake Polevskoye, Karelia, NW Russia

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2022
2022
2022
2022

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(1 citation statement)
references
References 63 publications
0
1
0
Order By: Relevance
“…In addition, sediment analysis represents a relevant task of lacustrine investigations, where freshwater allows for improved wave penetration and image resolution [259][260][261]. With respect to conventional underwater mapping methods, GPR represents a faster and more reliable solution, particularly in a shallow water context, capable of providing a continuous cross-section of the lake bottom and the underlying sediment column [262][263][264][265][266]. Waterborne GPR mapping of lakes has several objectives, including studies of sedimentation environments and stratigraphic boundaries [267,268], the estimation of a sedimentation rate and volume of lacustrine sediments [269], and the tracing of tectonic faults and displacements beneath the lake [270], improving the understanding of the evolution of water bodies at a local scale.…”
Section: Gpr Applications In Geologymentioning
confidence: 99%
“…In addition, sediment analysis represents a relevant task of lacustrine investigations, where freshwater allows for improved wave penetration and image resolution [259][260][261]. With respect to conventional underwater mapping methods, GPR represents a faster and more reliable solution, particularly in a shallow water context, capable of providing a continuous cross-section of the lake bottom and the underlying sediment column [262][263][264][265][266]. Waterborne GPR mapping of lakes has several objectives, including studies of sedimentation environments and stratigraphic boundaries [267,268], the estimation of a sedimentation rate and volume of lacustrine sediments [269], and the tracing of tectonic faults and displacements beneath the lake [270], improving the understanding of the evolution of water bodies at a local scale.…”
Section: Gpr Applications In Geologymentioning
confidence: 99%