Author:
Publisher:
ISBN:
Category :
Languages : fr
Pages :
Book Description
Rapports concernant le réseau des chemins de fer du Jura bernois
Rapport concernant le réseau des chemins de fer du Jura bernois
Rapport de la direction des chemins de fer du Jura bernois au conseil dadministration concernant les résultats probables de lexploitation du réseau complet
Integrated Stratigraphy of the Oxfordian and Kimmeridgian (Late Jurassic) in northern Switzerland and adjacent southern Germany
Author: Reinhart A. Gygi
Publisher: Birkhäuser
ISBN: 3034877781
Category : Science
Languages : en
Pages : 150
Book Description
1. 1 Geographical and 1. 2 Previous work palaeogeographical setting Stratigraphic exploration of the Swiss Jura range began before The measuring of detailed sections and the excavation of fossils 1820. MERIAN (1821) described the Jurassic sediments in the ar were done in an area which is confined to the west by a line be ea of Basel for the first time and gave a short and appropriate tween Boncourt in Canton Jura and Biel in Canton Bern description of the principal lithostratigraphic units. Merian (fig. 1). The belt of outcrops becomes narrower towards the east was aware that fossils were a means for correlation, but he stated and then runs northeast from Canton Aargau to Mohringen on that fossils were not known well enough at the time for this the Danube river in southern Germany. This whole area is purpose. Therefore he correlated strictly lithostratigraphically. where the Burgundy platform (PuRSER 1979) interfingers with He correlated the marls of the Biirschwil Formation of the early sediments of the rhodano-swabian epicontinental sea which and middle Oxfordian in the central Jura with the marls of the was situated adjacent to northern Tethys (fig. 63). The whole Effingen Member of the middle and late Oxfordian in the east area was transformed into an epicontinental sea (fig. 2) by the ern Jura range (fig. 3)."
Publisher: Birkhäuser
ISBN: 3034877781
Category : Science
Languages : en
Pages : 150
Book Description
1. 1 Geographical and 1. 2 Previous work palaeogeographical setting Stratigraphic exploration of the Swiss Jura range began before The measuring of detailed sections and the excavation of fossils 1820. MERIAN (1821) described the Jurassic sediments in the ar were done in an area which is confined to the west by a line be ea of Basel for the first time and gave a short and appropriate tween Boncourt in Canton Jura and Biel in Canton Bern description of the principal lithostratigraphic units. Merian (fig. 1). The belt of outcrops becomes narrower towards the east was aware that fossils were a means for correlation, but he stated and then runs northeast from Canton Aargau to Mohringen on that fossils were not known well enough at the time for this the Danube river in southern Germany. This whole area is purpose. Therefore he correlated strictly lithostratigraphically. where the Burgundy platform (PuRSER 1979) interfingers with He correlated the marls of the Biirschwil Formation of the early sediments of the rhodano-swabian epicontinental sea which and middle Oxfordian in the central Jura with the marls of the was situated adjacent to northern Tethys (fig. 63). The whole Effingen Member of the middle and late Oxfordian in the east area was transformed into an epicontinental sea (fig. 2) by the ern Jura range (fig. 3)."
Rapport de la Direction des chemins de fer du canton de Berne concernant A. La Justification financière de la Compagnie du Jura bernois et B. L'apport des lignes de l'Etat comme participation à l'entreprise du réseau jurassien
Rapport au grand-conseil concernant l'établissement de chemins de fer dans le Jura
Author:
Publisher:
ISBN:
Category :
Languages : fr
Pages : 52
Book Description
Bernische-Jurabahnen.
Publisher:
ISBN:
Category :
Languages : fr
Pages : 52
Book Description
Bernische-Jurabahnen.
Rapport de la direction des chemins de fer du canton de Berne concernant la justification financière de la compagnie du Jura bernois, lapport des lignes de lEtat comme participation à lentreprise du réseau jurassien
Author:
Publisher:
ISBN:
Category :
Languages : fr
Pages : 117
Book Description
Bernische-Jurabahnen.
Publisher:
ISBN:
Category :
Languages : fr
Pages : 117
Book Description
Bernische-Jurabahnen.
Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland
Author: Reinhart A. Gygi
Publisher: Springer Science & Business Media
ISBN: 303480136X
Category : Science
Languages : en
Pages : 214
Book Description
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.
Publisher: Springer Science & Business Media
ISBN: 303480136X
Category : Science
Languages : en
Pages : 214
Book Description
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.