Fig. 3: The Pleistocene Kerinitis Delta System (KDS).
From: Morphodynamic limits to environmental signal propagation across landscapes and into strata
a Oblique aerial image of the topsets of the KDS developed in the hanging wall of the Pirgaki–Mamoussia fault (planar-inclined surface to the left). The height of the outcrop is ~500 m. Image courtesy of Dr Bonita Barrett (Equinor). b ATF diagram for the KDS showing two estimations for the position of the autogenic threshold function. A scenario where Qa* approaches zero at T95 = Tc (solid lines) and a scenario where T95 = 8Tc (dashed lines). Allogenic sediment flux signals have an assumed magnitude of 0.3Qin, and a range between 20 and 50% of Qin based on estimates of Milankovitch-scale sediment supply variations (Blum and Hattier-Womack34; Watkins et al.32).
