[1654] - Quaternary sediment architecture in the Orkhon Valley (central Mongolia) inferred from capacitive coupled resistivity and Georadar measurements

All available metadata of the dataset are listed below. Some features are available, e.g. download of dataset or additional description file.

Features
Citation
Mackens, S., Klitzsch, N., Gruetzner, C., Klinger, R., 2017. Quaternary sediment architecture in the Orkhon Valley (central Mongolia) inferred from capacitive coupled resistivity and Georadar measurements. Geomorphology, 292, 72 - 84. DOI: 10.1016/j.geomorph.2017.05.002.
Identification
Title(s):Main Title: Quaternary sediment architecture in the Orkhon Valley (central Mongolia) inferred from capacitive coupled resistivity and Georadar measurements
Description(s):Abstract: Detailed information on shallow sediment distribution in basins is required to achieve solutions for problems in Quaternary geology, geomorphology, neotectonics, (geo)archaeology, and climatology. Usually, detailed information is obtained by studying outcrops and shallow drillings. Unfortunately, such data are often sparsely distributed and thus cannot characterise entire basins in detail. Therefore, they are frequently combined with remote sensing methods to overcome this limitation. Remote sensing can cover entire basins but provides information of the land surface only. Geophysical methods can close the gap between detailed sequences of the shallow sediment inventory from drillings at a few spots and continuous surface information from remote sensing. However, their interpretation in terms of sediment types is often challenging, especially if permafrost conditions complicate their interpretation. Here we present an approach for the joint interpretation of the geophysical methods ground penetrating radar (GPR) and capacitive coupled resistivity (CCR), drill core, and remote sensing data. The methods GPR and CCR were chosen because they allow relatively fast surveying and provide complementary information. We apply the approach to the middle Orkhon Valley in central Mongolia where fluvial, alluvial, and aeolian processes led to complex sediment architecture. The GPR and CCR data, measured on profiles with a total length of about 60 km, indicate the presence of two distinct layers over the complete surveying area: (i) a thawed layer at the surface, and (ii) a frozen layer below. In a first interpretation step, we establish a geophysical classification by considering the geophysical signatures of both layers. We use sedimentological information from core logs to relate the geophysical classes to sediment types. This analysis reveals internal structures of Orkhon River sediments, such as channels and floodplain sediments. We also distinguish alluvial fan deposits and aeolian sediments by their distinct geophysical signature. With this procedure we map aeolian sediments, debris flow sediments, floodplains, and channel sediments along the measured profiles in the entire basin. We show that the joint interpretation of drillings and geophysical profile measurements matches the information from remote sensing data, i.e., the sediment architecture of vast areas can be characterised by combining these techniques. The method presented here proves powerful for characterising large areas with minimal effort and can be applied to similar settings.
Identifier(s):DOI: 10.1016/j.geomorph.2017.05.002
Responsible Party
Creator(s):Author: Sonja Mackens
Author: Norbert Klitzsch
Author: Christoph Gruetzner
Author: Riccardo Klinger
Publisher:Elsevier
Topic
TR32 Topic:Soil
Related Sub-project(s):B8
Subject(s):CRC/TR32 Keywords: Geophysics, GPR
File Details
File Name:Mackens_et_al_2017.pdf
Data Type:Text
File Size:3340 kB (3.262 MB)
Date(s):Date Accepted: 2017-05-03
Available: 2017-05-05
Mime Type:application/pdf
Data Format:PDF
Language:English
Status:Completed
Constraints
Download Permission:OnlyTR32
General Access and Use Conditions:According to the TR32DB data policy agreement.
Access Limitations:According to the TR32DB data policy agreement.
Licence:TR32DB Data policy agreement
Geographic
North:-no map data
East:-
South:-
West:-
Measurement Region:Other
Measurement Location:--Other--
Specific Informations - Publication
Status:Published
Review:PeerReview
Year:2017
Type:Article
Article Type:Journal
Source:Geomorphology
Volume:292
Number Of Pages:13
Page Range:72 - 84
Metadata Details
Metadata Creator:Tanja Kramm
Metadata Created:2019-01-31
Metadata Last Updated:2019-01-31
Subproject:B8
Funding Phase:3
Metadata Language:English
Metadata Version:V43
Metadata Export
Metadata Export:
Export XML
Dataset Metrics
Page Visits:18
Metadata Downloads:0
Dataset Downloads:0
Dataset Activity
Features