Present-day stress orientation in the Molasse Basin

The present-day maximum horizontal stress orientation in the Molasse Basin is broadly perpendicular to the strike of the Alpine front, indicating that the stress pattern is probably controlled by gravitational potential energy of Alpine topography rather than by plate boundary forces. The present-da...

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Main Authors: Reinecker, J., Tingay, Mark, Müller, B., Heidbach, O.
Format: Journal Article
Published: Elsevier Science BV 2009
Online Access:http://hdl.handle.net/20.500.11937/21999
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author Reinecker, J.
Tingay, Mark
Müller, B.
Heidbach, O.
author_facet Reinecker, J.
Tingay, Mark
Müller, B.
Heidbach, O.
author_sort Reinecker, J.
building Curtin Institutional Repository
collection Online Access
description The present-day maximum horizontal stress orientation in the Molasse Basin is broadly perpendicular to the strike of the Alpine front, indicating that the stress pattern is probably controlled by gravitational potential energy of Alpine topography rather than by plate boundary forces. The present-day maximum horizontal stress orientations determined herein have important implications for the production of hydrocarbons and geothermal energy in the German Molasse Basin, in particular that hydraulically-induced fractures are likely to propagate N–S and that wells deviated to the north or south may have reduced wellbore instability problems.
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publishDate 2009
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spelling curtin-20.500.11937-219992019-02-19T04:26:12Z Present-day stress orientation in the Molasse Basin Reinecker, J. Tingay, Mark Müller, B. Heidbach, O. The present-day maximum horizontal stress orientation in the Molasse Basin is broadly perpendicular to the strike of the Alpine front, indicating that the stress pattern is probably controlled by gravitational potential energy of Alpine topography rather than by plate boundary forces. The present-day maximum horizontal stress orientations determined herein have important implications for the production of hydrocarbons and geothermal energy in the German Molasse Basin, in particular that hydraulically-induced fractures are likely to propagate N–S and that wells deviated to the north or south may have reduced wellbore instability problems. 2009 Journal Article http://hdl.handle.net/20.500.11937/21999 10.1016/j.tecto.2009.07.021 Elsevier Science BV fulltext
spellingShingle Reinecker, J.
Tingay, Mark
Müller, B.
Heidbach, O.
Present-day stress orientation in the Molasse Basin
title Present-day stress orientation in the Molasse Basin
title_full Present-day stress orientation in the Molasse Basin
title_fullStr Present-day stress orientation in the Molasse Basin
title_full_unstemmed Present-day stress orientation in the Molasse Basin
title_short Present-day stress orientation in the Molasse Basin
title_sort present-day stress orientation in the molasse basin
url http://hdl.handle.net/20.500.11937/21999