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Creep data of (Dotternhausen) Posidonia shale

Authors
/persons/resource/uddi

Rybacki,  Erik
4.2 Geomechanics and Rheology, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/hermi

Herrmann,  Johannes
4.2 Geomechanics and Rheology, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/wirth

Wirth,  R.
4.4 Interface Geochemistry, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/dre

Dresen,  G.
4.2 Geomechanics and Rheology, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

, 

External Ressource

http://doi.org/10.1007/s00603-017-1295-y
(Supplementary material)

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Citation

Rybacki, E., Herrmann, J., Wirth, R., Dresen, G. (2018): Creep data of (Dotternhausen) Posidonia shale.
https://doi.org/10.5880/GFZ.4.2.2018.001


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_2966895
Abstract
Experimentally determined data to examine the creep behavior of an immature carbonate-rich Posidonia shale (Dottenhausen), subjected to constant stress conditions at temperatures between 50 and 200 °C and confining pressures of 50–200 MPa, simulating elevated in-situ depth conditions. The data are described in and supplementary material to Rybacki et al. (2017; http://doi.org/10.1007/s00603-017-1295-y). The data refer to Figure 1 and Table 1 of Rybacki et al. (2017) and are povided in tab-separated ASCII-Format (.dat). The first column represents time in sec and second column the associated axial strain (decimal separator is a comma). An empty line separates data before and after achieving constant stress conditions (cf., Fig. 1 in Rybacki et al., 2017).