Hydrothermal fluid flow modelling in homogeneous and stratified sedimentary basin

The movies show the evolution in time of 2-D numerical model calculations investigating hydrothermal fluid flow around a cooling sills in a sedimentary basin. Each movie shows the evolution of a single variable for a specific model setup. The reported variables are: water fraction in the host rock (fH2O), mass of methane (mCH4), permeability (Perm), porosity (Phi), temperature (T), and TOC content of the host rock (TOC).

S0: five reference simulations in simplified setups

S1-S3 : The basin has been dissected in three regions with different basin depths. Each of these regions was investigated in a specific 2D modelling section which is refered to as setup S1, S2 and S3, respectively.

Data and Resources

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Cite this as

Galerne, Christophe, Hasenclever, Jörg (2019). Dataset: Hydrothermal fluid flow modelling in homogeneous and stratified sedimentary basin. https://doi.org/10.1594/PANGAEA.900982

DOI retrieved: 2019

Additional Info

Field Value
Imported on November 29, 2024
Last update November 29, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.900982
Author Galerne, Christophe
Given Name Christophe
Family Name Galerne
More Authors
Hasenclever, Jörg
Source Creation 2019
Publication Year 2019
Resource Type text/tab-separated-values - filename: Galerne-Hasenclever_2019
Subject Areas
Name: Chemistry

Name: Geophysics

Name: Lithosphere

Related Identifiers
Title: Distinct degassing pulses during magma invasion in the stratified Karoo Basin – New insights from hydrothermal fluid flow modelling
Identifier: https://doi.org/10.1029/2018GC008120
Type: DOI
Relation: IsSupplementTo
Year: 2019
Source: Geochemistry, Geophysics, Geosystems
Authors: Galerne Christophe , Hasenclever Jörg .