English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
Add to Basket
  DetailsSummary

Released
Conference Paper

Investigation of sedimentary deposits in the Atacama desert-Chile using loop source transient electromagnetics

Authors

Blanco,  B.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Yogeshwar,  P.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Tezkan,  B.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Wennrich,  V.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Buske,  S.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Ninnemann,  L.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

Diaz,  D.
28. Kolloquium, 2019, Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung, External Organizations;

External Ressource
Fulltext (public)

EMTF_2019_HalternAmSee_37_Blanco.pdf
(Publisher version), 6MB

Supplementary Material (public)
There is no public supplementary material available
Citation

Blanco, B., Yogeshwar, P., Tezkan, B., Wennrich, V., Buske, S., Ninnemann, L., Diaz, D. (2020): Investigation of sedimentary deposits in the Atacama desert-Chile using loop source transient electromagnetics. - In: Börner, J., Yogeshwar, P., Becken, M. (Eds.), - Protokoll über das 28. Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung: Haltern am See, 23.-27. September 2019, 28. Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung (Haltern am See 2019), 167-167.


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5001615
Abstract
The present study was conducted within the collaborative research center CRC 1211 (EARTH - Evolution at the dry limit) which aims to characterize the mutual relationship of Earth processes and biolog- ical evolution. In this context, claypans in endorheic basins along the Coastal Cordillera of the Atacama desert (Chile) host unique records of the precipitation history of one of the major hyperarid deserts in the world [4,5]. −23 ̊ PAG c) PARANAL Profile NS N Profile B PBT12 PBT12 P4T05 This study aims to provide detailed information about the sedimen- tary architecture and bedrock topography of selected claypans (PAG and PAR, see also Fig. 1, 2). Accordingly, we performed a geophysi- cal survey using the Transient Electromagnetic Method (TEM)[1,2] and Seismics. To derive suitable drilling locations for paleoclimatic research, and to better understand the deposition regime.