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Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland

  • Reinhart A. Gygi

Table of contents

  1. Front Matter
    Pages i-v
  2. Reinhart A. Gygi
    Pages 9-23
  3. Reinhart A. Gygi
    Pages 35-39
  4. Reinhart A. Gygi
    Pages 41-106
  5. Reinhart A. Gygi
    Pages 107-125
  6. Reinhart A. Gygi
    Pages 131-150
  7. Reinhart A. Gygi
    Pages 161-163
  8. Reinhart A. Gygi
    Pages 165-167
  9. Reinhart A. Gygi
    Pages 169-190
  10. Reinhart A. Gygi
    Pages 191-202
  11. Back Matter
    Pages 203-216

About this book

Introduction

The book summarizes about 40 years of the author’s research on sedimentary geology in an epicontinental (shelf) sea during the Late Jurassic in northern Switzerland. It presents a synopsis of the interplay of varying paleoclimate, of sea level variations, of varying water depth, of sea floor topography, of vertical and lateral facies changes, of processes of sedimentation like aggradation and progradation, of compaction, of the great regional differences in rates of sedimentation and in isostatic equilibration of the lithosphere under load, and of concomitant synsedimentary tectonics. Regional variation in isostatic adjustment of the lithosphere to the increasing load of sediments is analyzed by means of time correlations based on a detailed biochronology of ammonites in combination with mineral stratigraphy using the comparatively stable clay mineral kaolinite, and with sequence stratigraphy.

Keywords

ammonite zonation eustatism paleobathymetry paleoclimate paleoecology

Authors and affiliations

  • Reinhart A. Gygi
    • 1
  1. 1.ZürichSwitzerland

Bibliographic information