التفاصيل البيبلوغرافية
العنوان: |
Input and resulting structural and parameterized subsurface data for a geological model of the geothermal research platform Groß Schönebeck (North German Basin) |
المؤلفون: |
Norden, Ben, Bauer, Klaus, Krawczyk, Charlotte M. |
المساهمون: |
Norden, Ben |
بيانات النشر: |
GFZ Data Services |
سنة النشر: |
2022 |
المجموعة: |
GFZ Data Services (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
مصطلحات موضوعية: |
Groß Schönebeck, reservoir model, petrophysical parameterization, Rotliegend, Permo-Carboniferous volcanic rocks, EPOS, geo-energy test beds, compound material > rock > igneous rock, compound material > rock > sedimentary rock, EARTH SCIENCE > SOLID EARTH > GEOTHERMAL DYNAMICS > GEOTHERMAL ENERGY, EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > SEDIMENTARY ROCKS > SEDIMENTARY ROCK PHYSICAL/OPTICAL PROPERTIES, EARTH SCIENCE SERVICES > MODELS > GEOLOGIC/TECTONIC/PALEOCLIMATE MODELS, In Situ/Laboratory Instruments > Corers, Models/Analyses > Merged Analysis, Phanerozoic > Paleozoic > Permian |
جغرافية الموضوع: |
Geothermal Research Platform Groß Schönebeck, 13.6011 13.6025 52.9031 52.9043 |
الوصف: |
The dataset presented in this compilation provides the input data used for the geological interpretation and for the model parameterization (Norden et al., 2022) of a 3D seismic survey in the area of the geothermal research platform Groß Schönebeck (carried out in 2017; Krawczyk et al., 2019), focussing on the deep Permo-Carboniferous geothermal targets. The geothermal research platform Groß Schönebeck is located about 50 km north of Berlin, on the southern edge of the Northeast German Basin, and is equipped with two deep wells, the E GrSk 3/90 and Gt GrSk 4/05 boreholes. In this data compilation we provide general data on the location of the boreholes and data on the applied methods and the interpretation of petrophysical properties (density, porosity, permeability, thermal properties) obtained by core analysis and well-log interpretation. Because cores were available for the E GrSk 3/90 borehole only, most of the data is referring to the borehole that was drilled more or less vertically. The other borehole (Gt GrSk 4/05) is a deviated well, drilled as a geothermal production well. Further on, we provide the main interpreted structural reflector horizons of the geological model from surface to the assumed top of sedimentary Carboniferous (for discussion of the uncertainty of this boundary please consider the comments in Norden et al., 2022) and the horizons and 3D grid properties of a parameterized simulation grid for the deep geothermal target (sedimentary Rotliegend and Permo-Carboniferous volcanic rocks). |
نوع الوثيقة: |
dataset |
اللغة: |
unknown |
Relation: |
url:https://faculty.ksu.edu.sa/sites/default/files/klinkenbergspaper-1941.pdf; url:http://d-nb.info/971558531/34; url:https://www.sciencedirect.com/bookseries/developments-in-petroleum-science/vol/37/suppl/C; url:https://docplayer.org/4941525-Geothermie-forschungsbohrung-in-gross-schoenebeck-von-der-planung-bis-zur-stimulation.html; http://dx.doi.org/10.5880/GFZ.4.8.2022.013 |
DOI: |
10.5880/GFZ.4.8.2022.013 |
الاتاحة: |
https://doi.org/10.5880/GFZ.4.8.2022.013 |
Rights: |
CC BY 4.0 ; http://creativecommons.org/licenses/by/4.0/ |
رقم الانضمام: |
edsbas.7F83C485 |
قاعدة البيانات: |
BASE |