Introductory statement - Prospecting for ore minerals is often carried on by examining the bedrock at or very near the earth’s surface. The bedrock, however, over large areas of the earth, is covered by layers of material called overburden. It has been demonstrated that under certain conditions the bedrock can be examined indirectly by chemical analyses of the soils or plants covering it. Canada, particularly in the north, has large areas covered by deposits in the form of peat bogs or muskegs. The examination of bedrock under peat bogs or muskegs by chemical analyses has not been practised in Canada, but it has been tried with some success in Finland. The present study was organized under the name “Operation Muskeg” to be carried out by a ...
The lowering of water level caused by bog drainage increases the exposure of the upper layers of pea...
Abstract. Crystalline bedrock and Quaternary sediments are the parent materials for soil, which is a...
Peat is a naturally existing sedimentary material that is both common and unusual; its origins are d...
Muskeg is a very important component of the terrain of Canada. Research into this complex material h...
Surface moss and peat analyses are presented from five North American ombrotrophic bogs: three sites...
Five peat-forming environments were investigated for their organic petrological, mineralogical and g...
The peat and pore-water biogeochemistry of an Irish oceanic raised bog are reported with a view to u...
Abstract. Bogs, economically valuable wetlands, are subjected to exploitation in southern Canada. We...
Abstract: Many North American peatlands previously mined for horticultural peat have been abandoned ...
As the discovery of porphyry Cu deposits from outcropping mineralised or altered bedrock decreases, ...
Determining whether a wetland is ombrotrophic or minerotrophic is foundational for further studies o...
T HE various types of peatlands differ from one another in many respects. An important factor contro...
This item is only available electronically.Biogeochemical methods can be employed to assist in detec...
This item is only available electronically.The northwestern Flinders Ranges hosts a variety of Pb/Zn...
Peat is a soil consisting of semi-decomposed plant material which accumulates in situ as a result of...
The lowering of water level caused by bog drainage increases the exposure of the upper layers of pea...
Abstract. Crystalline bedrock and Quaternary sediments are the parent materials for soil, which is a...
Peat is a naturally existing sedimentary material that is both common and unusual; its origins are d...
Muskeg is a very important component of the terrain of Canada. Research into this complex material h...
Surface moss and peat analyses are presented from five North American ombrotrophic bogs: three sites...
Five peat-forming environments were investigated for their organic petrological, mineralogical and g...
The peat and pore-water biogeochemistry of an Irish oceanic raised bog are reported with a view to u...
Abstract. Bogs, economically valuable wetlands, are subjected to exploitation in southern Canada. We...
Abstract: Many North American peatlands previously mined for horticultural peat have been abandoned ...
As the discovery of porphyry Cu deposits from outcropping mineralised or altered bedrock decreases, ...
Determining whether a wetland is ombrotrophic or minerotrophic is foundational for further studies o...
T HE various types of peatlands differ from one another in many respects. An important factor contro...
This item is only available electronically.Biogeochemical methods can be employed to assist in detec...
This item is only available electronically.The northwestern Flinders Ranges hosts a variety of Pb/Zn...
Peat is a soil consisting of semi-decomposed plant material which accumulates in situ as a result of...
The lowering of water level caused by bog drainage increases the exposure of the upper layers of pea...
Abstract. Crystalline bedrock and Quaternary sediments are the parent materials for soil, which is a...
Peat is a naturally existing sedimentary material that is both common and unusual; its origins are d...