About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)

Abstract


Journal of Sedimentary Petrology
Vol. 54 (1984)No. 3. (September), Pages 746-758

Messinian Fanglomerates: The Colombacci Formation in the Pietrarubbia Basin, Italy

A. J. de Feyter, N. Molenaar

ABSTRACT

During the late Miocene, in the central Italian Apennines, sedimentation occurred in a few distinct basins resulting from synsedimentary tectonics. Alluvial fan sediments of the Messinian Colombacci Formation accumulated in the most western of these basins, the Pietrarubbia basin. The Colombacci Formation consists of coarse-grained, predominantly clast-supported conglomerates, pebbly sandstones, sandstones, and marls, which were deposited by high-viscosity debris flows and braided streams. The alluvial-fan deposits owe their development to an area of high relief that was caused by synsedimentary folding. The mode of deposition and the occurrence of caliche nodules point to a semiarid climate.


Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24