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Obituary Notice Richard 8t John Lambert 1928-1992 R. S. Lambert died in Edmonton, Canada in December 1992. After graduating in Natural Sciences and taking a PhD at Cambridge University, he followed a career as a university teacher at Oxford University and as Chair- man of the Department of Geology at the University of Edmonton . He made an immense contribution to the understanding of the metamorphic rocks of the Scottish Highlands. He demonstrated that Lewisian rocks in the Moine schists are tectonically emplaced above the base of the structural sequence, and proved that changes in the composition of white mica play a crucial role in the sequence of minerals in the low grade. zones .of Barrovian metamorphism. In collaboration with members of the Age and Isotope Research Group at Oxford, he linked isotopic studies with carefully documented models of metamorphic evolution, to produce a better understanding of both age-dating and metamorphic processes. In all these fields, subsequent research has confirmed his general conclusions, although structural and thermal models have been refined. In the late 1960s, he argued against the rigid appli- cation of metamorphic facies that was fashionable, emphasizing instead that metamorphic processes involve continuous changes of temperature and defor- mation. Recent advances in analytical techniques are showing how far-sighted he was. He continued to pursue his wide interests in geology after he moved to Canada in 1970 for example by publications about the allo- chthonous terranes of the Western Cordill era of Canada and the Archaean of China. Many Geologists' Association members have gained from his teaching of extra-mural evening classes during his years at Oxford, an unusual and very valuable application of his wide knowledge of the ph ysical and chemical aspects of geology . ROGER MAsON

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Obituary Notice

Richard 8t John Lambert 1928-1992

R. S. Lambert died in Edmonton, Canada in December1992. After graduating in Natural Sciences and takinga PhD at Cambridge University , he followed a career asa university teacher at Oxford University and as Chair­man of the Department of Geology at the University ofEdmonton. He made an immense contribution to theunderstanding of the metamorphic rocks of the ScottishHighlands. He demonstrated that Lewisian rocks in theMoine schists are tectonically emplaced above the baseof the structural sequence, and proved that changes inthe composition of white mica play a crucial role inthe sequence of minerals in the low grade. zones .ofBarrovian metamorphism. In collaborat ion withmembers of the Age and Isotope Research Group atOxford, he linked isotopic studies with carefullydocumented models of metamorphic evolution, toproduce a better understanding of both age-dating andmetamorphic processes. In all these fields , subsequent

research has confirmed his general conclusions,although structural and thermal models have beenrefined .

In the late 1960s, he argued against the rigid appli­cation of met amorphic facies that was fashionable,emphasizing instead that metamorphic processesinvolve continuous changes of temperature and defor­mation. Recent advances in analytical techniques areshowing how far-sighted he was. He continued to pursuehis wide interests in geology after he moved to Canadain 1970 for example by publications about the allo­chthonous terranes of the Western Cordillera ofCanada and the Archaean of China. Many Geologists'Association members have gained from his teaching ofextra-mural evening classes during his years at Oxford ,an unusual and very valuable application of his wideknowledge of the physical and chemical aspects ofgeology .

ROGER MAsON