161 |
Physico-chemical characterisation of kerogen from the South Wales coalfield and elsewhereRahman, Mokhlesur January 1990 (has links)
No description available.
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162 |
The application of regional geochemistry in determining the causes and predicted incidence of bovine hypocupraemiaLeech, A. F. January 1984 (has links)
No description available.
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163 |
The relationship between fluids and structure at the Patchway gold mine, ZimbabweHerrington, Richard Jeremy January 1991 (has links)
No description available.
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164 |
Developments in surveying technology and their application to engineering geologyKennie, T. J. M. January 1991 (has links)
No description available.
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165 |
Basaltic volcanism, volcanoes and volcanic rocks of marine and lacustrine environmentsJones, John Gilbert January 1968 (has links)
Intraglacial basaltic volcanoes near Laugarvatn, south-west Iceland, range from simple pillow lava piles to tuyas - volcanoes of tablemountain form in which a superstructure combining a carapace of sheet lava on a pedestal of breccia envelops a tuff-mantled pillow lava pile. The pillow lava piles are inferred to be the product of effusion of lava into glacial meltwater, and the tuff cappings which most exhibit record a later phase of explosive emergence from the meltwater pond. The sheet lava and flow-foot breccia of the tuyas are believed to record an ultimate phase of lava effusion in air, following earlier phases of aqueous effusion and explosive emergence, in which flows advanced outwards into encircling meltwater on deltas of breccia formed at their fronts. The little that is known of the morphology and constitution of marine basaltic volcanoes suggests that they are basically similar to the Laugarvatn volcanoes and that concepts derived from the study of the latter have general application. Examination of the structural characteristics of Icelandic and Welsh pillow lavas suggests a mode of formation and propagation akin to the digital advance of pahoehoe: and a vesicularity study indicates the potential importance of pillow lavas as depth indicators. Review of the literature suggests that explosive activity, induced by extraneous water, is characteristic of eruption of basalt lava from a wet vent in shallow water and in air. Observations of the immersion of basalt lava are reviewed, and the significance of structural records of immersion is indicated. A re-examination of the type 'peperites' suggests that they are the product, not of brecciation of lava intruded into wet sediment as is currently accepted, but of explosive projection of basaltic ejecta into steadily accumulating lime mud.
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Site investigation : its cost and benefit in PortugalCarvalho, J. A. R. January 1981 (has links)
No description available.
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167 |
Cenozoic evolution of the proto-Nile delta : with special reference to the Messinian salinity crisisBarber, P. M. January 1982 (has links)
No description available.
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168 |
Mineralogy and geochemistry of metalliferous sediments from the Bauer Deep, Southeast Pacific, and the Atlantis II Deep, Red SeaCole, Thomas George January 1982 (has links)
No description available.
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169 |
The micropalaeontology of the Middle Triassic to Upper Miocene sediments of Seram, Eastern IndonesiaAl-Shaibani, S. K. January 1983 (has links)
No description available.
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170 |
An investigation of some potential Jurassic hydrocarbon source rocks of Southern EnglandEbukanson, E. J. January 1984 (has links)
No description available.
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