In 1984 the Ontario Geological Survey initiated a research project on the Sudbury structure (SS) in cooperation with the University of Muenster. The project included field mapping (1984-1989) and petrographic, chemical, and isotope analyses of the major stratigraphic units of the SS. Four diploma theses and four doctoral theses were performed during the project (1984-1992). Specific results of the various investigations are reported. Selected areas of the SS were mapped and sampled: Footwall rocks; Footwall breccia and parts of the sublayer and lower section of the Sudbury Igneous Complex (SIC); Onaping Formation and the upper section of the SIC; and Sudbury breccia and adjacent Footwall rocks along extended profiles up to 55 km from the SI...
From the proceedings of the Workshop on Impact Cratering: Bridging the Gap between Modeling and Obse...
Deformation and melting of the crust during the formation of large impact craters must have been imp...
The 1.85 Ga Sudbury structure provides a unique opportunity to study the sequence of events that occ...
In cooperation between the Ontario Geological Survey and the Institute of Geology and Institute of P...
Within the Sudbury Project of the University of Muenster and the Ontario Geological Survey special e...
The Sudbury Structure, Ontario, is the remnant of a 1.85 Ga old impact crater, 200--250 km in diamet...
The Sudbury Igneous Complex (SIC) represents the remnant of a crystalline impact melt sheet of the S...
Sudbury breccias occur as discordant dike breccias within the footwall rocks of the Sudbury structur...
One major objective of our Sudbury project was to define origin and age of the huge breccia units be...
Sudbury breccia is an impactite situated in the footwall of the 1.85 Ga Sudbury impact structure, si...
The ca. 1850 Ma Sudbury structure (SS) lies in the Canadian Shield at the paleocontinental margin be...
This paper reviews the origin, development, and present status of the widely accepted theory, propos...
The 1.85 Ga Sudbury impact structure is considered a remnant of a multi-ring basin with an estimated...
In recent years, many geoscientists have come to believe that the Sudbury event was exogenic rather ...
The Temagami Anomaly is one of the largest unexplained magnetic features in North America. It is sim...
From the proceedings of the Workshop on Impact Cratering: Bridging the Gap between Modeling and Obse...
Deformation and melting of the crust during the formation of large impact craters must have been imp...
The 1.85 Ga Sudbury structure provides a unique opportunity to study the sequence of events that occ...
In cooperation between the Ontario Geological Survey and the Institute of Geology and Institute of P...
Within the Sudbury Project of the University of Muenster and the Ontario Geological Survey special e...
The Sudbury Structure, Ontario, is the remnant of a 1.85 Ga old impact crater, 200--250 km in diamet...
The Sudbury Igneous Complex (SIC) represents the remnant of a crystalline impact melt sheet of the S...
Sudbury breccias occur as discordant dike breccias within the footwall rocks of the Sudbury structur...
One major objective of our Sudbury project was to define origin and age of the huge breccia units be...
Sudbury breccia is an impactite situated in the footwall of the 1.85 Ga Sudbury impact structure, si...
The ca. 1850 Ma Sudbury structure (SS) lies in the Canadian Shield at the paleocontinental margin be...
This paper reviews the origin, development, and present status of the widely accepted theory, propos...
The 1.85 Ga Sudbury impact structure is considered a remnant of a multi-ring basin with an estimated...
In recent years, many geoscientists have come to believe that the Sudbury event was exogenic rather ...
The Temagami Anomaly is one of the largest unexplained magnetic features in North America. It is sim...
From the proceedings of the Workshop on Impact Cratering: Bridging the Gap between Modeling and Obse...
Deformation and melting of the crust during the formation of large impact craters must have been imp...
The 1.85 Ga Sudbury structure provides a unique opportunity to study the sequence of events that occ...