• Corpus ID: 150081732

Sedimentology, Lithostratigraphy and Geochronology of the Paleoproterozoic Gordon Lake Formation, Huronian Supergroup, Ontario, Canada

@inproceedings{Hill2019SedimentologyLA,
  title={Sedimentology, Lithostratigraphy and Geochronology of the Paleoproterozoic Gordon Lake Formation, Huronian Supergroup, Ontario, Canada},
  author={Carolyn Hill},
  year={2019}
}
................................................................................................................................i Co-Authorship Statement................................................................................................... iii Acknowledgments...............................................................................................................iv Table of 
1 Citations
Evidence of magmatism and rifting in the southern superior craton from the Temagami geophysical anomaly
Abstract The Temagami Geophysical Anomaly (TGA) is situated in the Paleoproterozoic Huronian Supergroup near the southern margin of Archean Superior craton, along strike from the Temagami Greenstone

References

SHOWING 1-10 OF 211 REFERENCES
Sedimentology and geochemistry of the mixed carbonate-siliciclastic Espanola Formation, Paleoproterozoic Huronian Supergroup, Bruce Mines-Elliot Lake Area, Ontario, Canada
.......................................................................................................................... i Acknowledgments
Factors Controlling the Composition and Lithofacies Characteristics of the Paleoproterozoic Bar River Formation, Huronian Supergroup
............................................................................................................................. ii Acknowledgments
Possible Metazoans from the Early Proterozoic of the Canadian Shield
DURING 1960, Mr. C. E. Bye, of Sault Ste. Marie, discovered the markings that are described here in the Lorrain Formation of Huronian age in Johnson Township, District of Algoma, Ontario. The
Quartz arenites: review and interpretation
Abstract Quartz arenites (orthoquartzites) are exceptional sands (Pettijohn et al., 1972) that, in the past, have formed extensive and commonly thick formations. They are somewhat enigmatic in that
Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic), Ontario, Canada: A chemostratigraphic approach
The Gowganda Formation (dated as about 2.3 Ga) is widely (but not universally) interpreted as glaciogenic, and our chemostratigraphic study supports such an interpretation. The bulk compositions of
The Paleoproterozoic upper Gowganda Formation, Whitefish Falls area, Ontario, Canada: subaqueous deposits of a braid delta
The upper Gowganda Formation is part of the Paleoproterozoic Huronian Supergroup (ca. 2.5–2.2 Ga) of the north shore of Lake Huron. The upper Gowganda Formation rests with sharp conformable contact
Tectonic Taphrogenesis and Paleoseismic Records from the Yishu Fault Zone in the Initial Stage of the Caledonian Movement
: The Yishu fault zone (mid-segment of the Tanlu fault zone) was formed in the Presinian. Periodic tectonic activities and strong seismic events have occurred along the fault zone. During the
Anatomy of North America: thematic geologic portrayals of the continent
Abstract Six thematic tectonic maps are used to analyse the makeup of the North American continent. Themes are: 1. (1) major tectonic elements of the continent 2. (2) time of last major deformation
Geochemistry of Precambrian carbonates. IV - Early Paleoproterozoic (2.25 +/- 0.25 Ga) seawater
In an effort to narrow down the first- and second-order variations in isotopic composition of the Early Paleoproterozoic (2.25 ± 0.25 Ga) seawater, we report a comprehensive study of mineralogy,
Contradictory correlations of Paleoproterozoic glacial deposits: Local, regional or global controls?
Abstract There is little agreement among recently proposed correlation schemes for Paleoproterozoic glaciogenic rocks scattered thinly around the globe. Correlations are hindered by the dearth of
...
1
2
3
4
5
...