Article ID Journal Published Year Pages File Type
4692637 Tectonophysics 2012 13 Pages PDF
Abstract
► Stress history is preserved in the compaction curves of sediments. ► The maximum overburden above the reverse fault is greater than the present vertical stress. ► The thickness of the eroded strata is 2482 m based on compaction curves measured in the laboratory. ► The thickness of the eroded strata is 2773 m based on a conventional regional method. ► The eroded strata were successfully estimated by our laboratory-based local method.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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