2026-05-25T12:37:55Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:80052025-08-26T12:30:47ZDOIDBDOIDB.GIPPfalse4DOIDB.GIPP
10.5880/GIPP.201812.1
Buske, Stefan
Stefan
Buske
0000-0003-3111-6922
TU Bergakademie Freiberg, Germany
Wennrich, Volker
Volker
Wennrich
0000-0003-3617-1963
University of Cologne, Cologne, Germany
Melles, Martin
Martin
Melles
0000-0003-0977-9463
University of Cologne, Cologne, Germany
Ninnemann, Lukas
Lukas
Ninnemann
0000-0001-5105-6483
TU Bergakademie Freiberg, Germany
Seismic investigations of clay pans in the Atacama Desert (N-Chile) (SEISCLAYPAN)
GFZ Data Services
2024
controlled source seismics
seismic weight drop
near surface geophysics
CONTROLLED_SOURCE_SEISMOLOGY > CORRELATED_DATA
CONTROLLED_SOURCE_SEISMOLOGY > LOCAL_SCALE
CONTROLLED_SOURCE_SEISMOLOGY > NEAR_SURFACE
CONTROLLED_SOURCE_SEISMOLOGY > RAW_DATA
CONTROLLED_SOURCE_SEISMOLOGY > REFLECTION
CONTROLLED_SOURCE_SEISMOLOGY > REFRACTION
CONTROLLED_SOURCE_SEISMOLOGY > RESERVOIR_SCALE
CONTROLLED_SOURCE_SEISMOLOGY > VERTICALLY_STACKED_DATA
CONTROLLED_SOURCE_SEISMOLOGY > VIBRO_SOURCE
CONTROLLED_SOURCE_SEISMOLOGY > WIDE-ANGLE_REFLECTION_REFRACTION
LAND
SEG-Y_DATA_FORMAT
SEISMIC_WAVEFORM_DATA
SENSOR > GEOPHONE
SENSOR > VERTICAL_COMPONENT
EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES > SEISMIC PROFILE
Geophysical Instrument Pool Potsdam (GIPP)
GFZ German Research Centre for Geosciences, Potsdam, Germany
GIPP Support Team
GFZ German Research Centre for Geosciences, Potsdam, Germany
2018-10/2018-11
2018-10/2018-11
2018-10/2018-11
Dataset
10.1190/1.1440530
10.1016/j.jsames.2022.103746
Ninnemann, L., Seismische Abbildung der Struktur dreier Tonpfannen in der Atacama-Wüste mit Hilfe von Ersteinsatz-Laufzeittomographie. BSc thesis, TU Bergakademie Freiberg, 2020.
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5028222
CC BY 4.0
The data set was acquired in the framework of the CRC 1211 “Earth – Evolution at the dry limit” which aims to study continuous longterm (Quaternary-Miocene) paleoclimatic/environmental records from the hyperarid core of the Atacama desert / N Chile covering the last up to 10 Ma. As part of this project, three clay pans were investigated in the Coastal Cordillera (Huara 20° 4'32.75"S; 69°55'1.46"W; PAG: 21°32'27.39"S; 69°54'47.21"W; Paranal 24°29'20.53"S; 70° 8'54.63"W). The clay pans are located along a latitudinal transect across the hyperarid core of the Atacama from 20° S to 24.5° S. The seismic survey comprised a couple of crossing 2D high-resolution seismic lines per each of the clay pans, acquired with vertical component geophones, Geode recorders and a PEG-40 accelerated weight drop as source.
Central coordinate of the Huara Site
Central coordinate of the PAG Site
Central coordinate of the Paranal Site
Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ
http://dx.doi.org/10.13039/501100010956
201812
GIPP: SEISCLAYPAN
Deutsche Forschungsgemeinschaft
http://dx.doi.org/10.13039/501100001659
CRC 1211
Earth – Evolution at the dry limit