Facies analysis and tectonic significance of lacustrine fan-deltaic successions in the Pliocene–Pleistocene Mugello Basin, Central Italy

M Benvenuti - Sedimentary Geology, 2003 - Elsevier
The Mugello Basin is an intermontane asymmetric basin, trending WNW–ESE and filled with
Pliocene–Pleistocene alluvial and lacustrine deposits. The study focuses on the
sedimentary succession deposited at the basin's northern margin and uses facies analysis
to reconstruct the margin's depositional and deformation history. The controversial concepts
of “fan delta” and “hyperconcentrated flow,” adopted in this study, are firstly discussed. The
early Pleistocene succession consists of two higher order, coarsening-upward successions …
以上显示的是最相近的搜索结果。 查看全部搜索结果