Some Geological Conditions Controlling the Formation of Iron Deposits in Canada

- Organization:
- Canadian Institute of Mining, Metallurgy and Petroleum
- Pages:
- 11
- File Size:
- 3169 KB
- Publication Date:
- Jan 1, 1925
Abstract
In order that a logical conclusion may be reached regarding the possible occurrence of commercial iron deposits in Canada it is necessary to consider some important producers found elsewhere on this continent. A study of such deposits reveals the fact tl:~at a number of distinct types are producing large tonnages of ore. These types may be classified according to origin and occurrence as follows: (1) Bedded sedimentary deposits. (2) Contact metamorphic deposits. (3) Residual ores. (4) Lenses in metamorphic rocks and m some cases of uncertain origin. In addition to the types listed there are other deposits which have contained or do contain considerable ore and they either have not been worked on a large scale or they have been nearly exhausted. These include the following types: (1) Magmatic segregations. These are mostly titaniferous magnetites. (2) Dikes of magnetite of igneous origin. (3) Bog and lake ores in glacial drift. (4) Black sand placers.
Citation
APA:
(1925) Some Geological Conditions Controlling the Formation of Iron Deposits in CanadaMLA: Some Geological Conditions Controlling the Formation of Iron Deposits in Canada. Canadian Institute of Mining, Metallurgy and Petroleum, 1925.