- About
-
The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
Search results
Showing 31 to 40 of 92 (0.035 seconds)Spelling suggestions: "subject:"deology -- québec (province)"" "subject:"deology -- québec (rovince)""
| 31 |
Stratigraphy of the Philipsburg, Rosenberg thrust sheets, Southern Quebec.Gilmore, Ralph Gawen. January 1971 (has links)
No description available.
|
| 32 |
Studies of geologic structures with the VLF method.King, Warren F. January 1971 (has links)
No description available.
|
| 33 |
A geochronologic and stratigraphic study of the Precambrian rocks north of Montreal.Barton, Jackson Mounce. January 1971 (has links)
No description available.
|
| 34 |
Geology of the Mutton Bay Intrusion and surrounding area, North Shore, Gulf of St. Lawrence, QuebecDavies, Raymond January 1968 (has links)
Geology and structure of 1,000 square miles of granulite-upper amphibolite facies gneisses cut by syn- and late-kinematic intrusions are described. The circular post-kinematic Mutton Bay alkaline syenite (631 m.y.) is divided into three main intrusive groups on the basis of chemistry, mineralogy, and field relations. Differentiation includes gravity settling and flow differentiation, while intrusion involved early stoping and assimilation with late faulting. Depth of the present level below the roof of the intrusion is estimated at 6-8 miles and temperature of crystallization of felspars in the early magmas at greater than 1015°C at less than 500 bars water pressure. Orthoclase inverted to microcline in foliated rocks that intruded as crystal mushes. A giant gabbro dyke with syenite differentiate (470 m.y.) is intruded by diabase and trachyte dykes. Carbonate enrichment in the trachytes is accompanied by high potash felspar content. Sandstone dykes are the only Paleozoic sediments.
|
| 35 |
Trace element partition in sulphides, Noranda, Quebec.Beaton, William Douglas. January 1970 (has links)
No description available.
|
| 36 |
Late quaternary events in northern Ungava, QuebecMatthews, Barry. January 1968 (has links)
No description available.
|
| 37 |
Geology of the Mutton Bay Intrusion and surrounding area, North Shore, Gulf of St. Lawrence, QuebecDavies, Raymond January 1968 (has links)
Geology and structure of 1,000 square miles of granulite-upper amphibolite facies gneisses cut by syn- and late-kinematic intrusions are described. The circular post-kinematic Mutton Bay alkaline syenite (631 m.y.) is divided into three main intrusive groups on the basis of chemistry, mineralogy, and field relations. Differentiation includes gravity settling and flow differentiation, while intrusion involved early stoping and assimilation with late faulting. Depth of the present level below the roof of the intrusion is estimated at 6-8 miles and temperature of crystallization of felspars in the early magmas at greater than 1015°C at less than 500 bars water pressure. Orthoclase inverted to microcline in foliated rocks that intruded as crystal mushes. A giant gabbro dyke with syenite differentiate (470 m.y.) is intruded by diabase and trachyte dykes. Carbonate enrichment in the trachytes is accompanied by high potash felspar content. Sandstone dykes are the only Paleozoic sediments.
|
| 38 |
Late quaternary events in northern Ungava, QuebecMatthews, Barry. January 1968 (has links)
No description available.
|
| 39 |
Geology of the Mutton Bay Intrusion and surrounding area, North Shore, Gulf of St. Lawrence, QuebecDavies, Raymond January 1968 (has links)
No description available.
|
| 40 |
A study of the variation in chemical composition of certain dykes at the Campbell Chibougamau Mine.Blecha, Matthew. January 1966 (has links)
No description available.
|
Page generated in 0.0407 seconds