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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
Chapter from:
Petroleum
Exploration and Development
Petroleum
Geologists. All rights reserved.
Fluid
Migration in Sedimentary Basins
Chapter 9
GIS-Based Analysis of
Fluid
Migration in Sedimentary Basins
Gernot Paulus
Department of Geology and Paleontology, University of Salzburg
Salzburg, Austria
ABSTRACT
Subsurface fluid
migration is a multi-parameter process depending on many different components (e.g., tectonics, facies, lithology, hydrochemistry, and hydraulics). Knowledge of subsurface
fluid
migration is critical to the success of
petroleum
and geothermal exploration, and to
petroleum
production in sedimentary basins. A geographical information system (GIS) has been used for the present study to integrate different data sets related to subsurface
fluid
migration and to perform spatial analysis on the resulting comprehensive database. The discussion illustrates the reliance on geographic location as the common frame of reference during the integration phase. The area of investigation is the Molasse Basin in Upper Austria, which is a typical asymmetric, compressional foreland basin at the northern margin of the Alps. Due to
petroleum
exploration and production, an excellent data set exists with more than 500 wells ranging in depth from 1000 to 4000 m. Three different fault systems have been active at different times from pre-Tertiary until the present and have a large impact on hydrocarbon migration and
fluid
flow. There are two components to the
fluid
migration modeled in this study: (1) a north-directed migration of hydrocarbons and (2) an east-directed
fluid
flow of deep groundwater at basin scale in a Jurassic carbonate aquifer. The aquifer is the main target for geothermal exploration in this area. The datasets used in the spatial analysis contain well data, subsurface fault data, and hydrocarbon
reservoir
data. Applications and examples of various spatial GIS analysis techniques are presented here, including (1) investigation of the spatial relationship between subsurface faults and well locations using buffer zones and topological overlay, (2) calculation of fault density and assessing its implication on subsurface
fluid
flow, (3) modeling of fault-related
fluid
flow using cost surfaces, and (4) spatial overlay of hydrocarbon
reservoir
information and fault-related permeability distributions. These examples provide a comprehensive overview of how to use the unique capabilities of a GIS in subsurface geologic analysis.
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