Results 181 to 190 of about 9,387 (221)
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Strain analysis of a shear zone in a granodiorite
Tectonophysics, 1978Abstract A ductile shear zone in a late Precambrian granodiorite, from the Rouergue (southwest part of the French Massif Central) has been studied. A single episode of deformation is responsible for the formation of a foliation and a well-defined lineation which are localized into an elongated zone, a few decimeters wide. The strain features can be
J.P. Burg, Ph. Laurent
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The Criffell-Dalbeattie granodiorite complex
Quarterly Journal of the Geological Society of London, 1956Summary The Criffell-Dalbeattie granodiorite complex is composed of three granodiorie' and associated quartz-dioritic rocks. Four-fifths of the area of exposed “ granitic ” rocks is occupied by the main Criffell-Dalbeattie granodiorite and the greater part of the paper is devoted to a study of the petrology, structure and emplacement of this ...
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Dissolution of cristobalite in granodiorite and felsite melts
Glass and Ceramics, 2009The process of dissolution of cristobalite during the calcination of acid-resistant articles based on Buskul’skoe clay using granodiorite and felsites is simulated. The mechanism governing the dissolution of cristobalite in their melts is determined. The process of dissolution of cristobalite in felsite and granodiorite melts can be divided into two ...
I. D. Kashcheev +4 more
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The granodiorite in ceramic production
AIP Conference Proceedings, 2022V. A. Lodyanaya +2 more
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The petrology of the Samford granodiorite [PDF]
, 1955 The post-orogenic Samford granodiorite is emplaced in geosynclinal deposits which have undergone low grade metamorphism. Detailed investigation of contact zones has shown that there can be all gradations from hornfels to a granodiorite due to recrystallisation and replacement. During these changes there was a concentration of femic material, and in the
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The Mountsorrel Granodiorite and Associated Igneous Rocks
Geological Magazine, 1934The igneous rocks of the Mountsorrel area, by reason of their accessibility and economic value, have attracted the attention of geologists since the middle of last century. The latest and most comprehensive account of the district is that of E. E. Lowe (1) and at the end of the paper a useful bibliography of earlier publications is given.
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A gabbro—granodiorite association in Singapore Island
Quarterly Journal of the Geological Society of London, 1964The syntectonic tin-bearing granite batholith system of the Thai-Malayan orogeny is associated in several places from north Thailand to Singapore with satellitic bodies of basic composition. In Singapore Island such a body of gabbroic composition is marginally situated within the batholith, and exposures indicate that it is pre-orogenic.
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