| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8914475 | Journal of Structural Geology | 2018 | 46 Pages |
Abstract
Carbonate facies distribution and early diagenetic imprint constrained the mechanical stratigraphy when fractures occurred. In addition, we observed that fractures related to late tectonic inversion were partly inhibited. Indeed, rock mechanical properties change through time. Characterizing the temporal evolution of carbonate rocks has revealed that diagenesis and sedimentary facies are the prime actors for brittleness and mechanical layering in carbonates.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Arthur P.C. Lavenu, Juliette Lamarche,