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Abstract
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Linkage pattern and growth history of fault-related folds have important implications for petroleum exploration.
This study evaluates the lateral growth and fold segmentation in the Dalan Anticline as a NW-SE trending hydrocarbon trap manifested as a fault-related fold within the Zagros Fold-Thrust Belt, SW Iran via tectonic geomorphology analyses. Several qualitative and quantitative geomorphic evidence including wind and water gaps,
drainage network, deflected drainage, drainage density, basin shape, fold front sinuosity, degree of incision in
the drainage basin outlet, stream-length gradient, asymmetry factor and hypsometric integral and related curves
were used to investigate the lateral propagation and linkage pattern in the fold. Systematic variation of these
parameter’s value highlighted the three younger parts of the fold with smaller, elongated and crescent-shaped
basins, concave hypsometric curves. This evidence reveals the presence of two independent fold segments
propagating both in northwest and southeast directions, respectively. The development and evolution of these
segments might led to the spatial and temporal differences in the geometry and activity intensity of the fold. This
study emphasizes the importance of understanding the growth history of fault-related folds in order to understand hydrocarbon migration and accumulation in fold and thrust belts.
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