Overview
- Authors:
-
-
Hillert Ibbeken
-
Institut für Geologie, Freie Universität Berlin, Berlin 33, Germany
-
Ruprecht Schleyer
-
Institut für Geologie, Freie Universität Berlin, Berlin 33, Germany
Access this book
Other ways to access
Table of contents (19 chapters)
-
-
Introduction
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 1-3
-
The Source
-
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 6-14
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 15-29
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 30-45
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 46-50
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 51-64
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 65-80
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 81-88
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 89-109
-
From the Source to the River-Mouth Sediment
-
Front Matter
Pages 111-111
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 112-123
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 124-142
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 143-146
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 147-155
-
River-Mouth Sediment and Provenance
-
Front Matter
Pages 157-157
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 158-170
-
- Hillert Ibbeken, Ruprecht Schleyer
Pages 171-191
-
Processes, Budget and Statistical Comparison
-
Front Matter
Pages 193-193
About this book
Deciphering provenance - this is the study of how far geology, geomorphology and climate of a source, a mountainous area, may be reconstructable from its erosional products released to the sea; from gravel and sand, from silt, sand, clay which recombine to form a new cycle of rocks. The purpose of this book is to give a quantitative picture of both source and sediment and the masses involved in the flux of material; based on a modern case study in Calabria, southern Italy, a mountain range which is part of an active plate margin. High erosion rates in the past (200mm/ka), and dramatic ones at present (1500mm/ka), make the area a powerful source of sediment comparable to orogenic conditions of the geological past. The book presents the first systematic, quantitative and data-bank supported study - here a larger source with small rivers and their sedimentary products - of the complex topic of provenance of terrigenous sediments and related mass balances at an active plate margin. It may serve as an orientation for corresponding research in other plate tectonic realms.