2138) The Lateral Stability of Beam-Columns(Structure)
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Op-petr120032 2115..2138
The central region of the mainland Lewisian gneiss complex of NW Scotland is a granulite-facies migmatite terrane.With the exception of ultramafic and rare calc-silicate rocks, all other lithologies partially melted during Neoarchaean, ultrahigh-temperature (Badcallian) metamorphism. The clearest evidence is preserved within large layered mafic^ultramafic bodies that exhibit macroscopic feature...
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ژورنال
عنوان ژورنال: Transactions of the Architectural Institute of Japan
سال: 1963
ISSN: 0387-1185,2433-0027
DOI: 10.3130/aijsaxx.89.0_210