Marine electrical resistivity profile 4 - east, Bykovsky Peninsula, Siberia

The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset betw...

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Bibliographic Details
Main Authors: Angelopoulos, Michael, Overduin, Pier Paul, Jenrich, Maren, Nitze, Ingmar, Günther, Frank, Strauss, Jens, Westermann, Sebastian, Schirrmeister, Lutz, Kholodov, Alexander L, Krautblatter, Michael, Grigoriev, Mikhail N, Grosse, Guido
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Alas
AWI Arctic Land Expedition
BYK_profile4e_parallel_to_shore
Bykovsky
DEPTH
water
electrical resistivity
Electrical resistivity tomography
ERT
LATITUDE
Lena2017
Lena Delta
LONGITUDE
Near surface geophysics
PETA-CARB
POINT DISTANCE from start
Position
Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool
Resistivity
apparent
Resistivity profiler
IRIS Syscal Pro Deep Marine
RU-Land_2017_Lena
Submarine Permafrost
subsea permafrost
talik
Thermokarst Lagoon
Arctic
Talik
Peta
lena delta
permafrost
Thermokarst
Siberia
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.934184
https://doi.org/10.1594/PANGAEA.934184
Description
Summary:The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset between the first electrode and the boat was approximately 10 m.

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