One of the most common depositional features observed in seismic sections are clinoforms manifested in a configuration pattern called ''offlap''. Clinoforms are progradational strata that form through the progressive development of gently sloping surfaces. Paleowater depths can be interpreted from the height of prograding clinoforms. [[:file:exploring-for-stratigraphic-traps_fig21-26.png|Figure 3]] shows prograding reflectors and their possible depositional significance.
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One of the most common depositional features observed in seismic sections are clinoforms manifested in a configuration pattern called ''offlap''. Clinoforms are progradational strata that form through the progressive development of gently sloping surfaces. Paleowater depths can be interpreted from the height of prograding clinoforms. [[:file:exploring-for-stratigraphic-traps_fig21-26.png|Figure 3]] shows [[Depocenter#Sediment_supply_rate_and_facies_patterns|prograding]] reflectors and their possible depositional significance.