Article ID Journal Published Year Pages File Type
9526130 Sedimentary Geology 2005 27 Pages PDF
Abstract
The Miocene coral reef growth and development in the Antalya Basin are characterized by large- to small-scale, transgressive-regressive reefal cycles which are closely related to the complex interaction of sporadic influxes of coarse terrigeneous clastics derived from the tectonically active basin margins and the related sea-level fluctuations.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Facies and environmental setting of the Miocene coral reefs in the late-orogenic fill of the Antalya Basin, western Taurides, Turkey: implications for tectonic control and sea-level changes
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