Zobrazeno 1 - 10
of 64
pro vyhledávání: '"C.G. Murray"'
Autor:
I. W. Withnall, P. R. Blake, Barry G. Fordham, L. J. Hutton, R. J. Holcombe, Christopher R. Fielding, Scott E. Bryan, C.G. Murray, M. A. Hayward, G. A. Simpson
Publikováno v:
Australian Journal of Earth Sciences. 50:271-293
Autor:
C.G. Murray, P.L. Wellman, K.D. Wake-Dyster, J. H. Leven, D. W. Johnstone, R. J. Korsch, D. M. Finlayson, H.J. Harrington
Publikováno v:
Tectonophysics. 173:211-230
Crustal architecture can be recognised from Seismic fabric characteristics and velocity information. Across Phanerozoic eastern Australia, three major crustal sub-divisions are identified from data in southern Queensland. They occur under (west to ea
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Autor:
C.G. Murray
Publikováno v:
Journal of Dentistry. 3:225-228
Nikalium has been found a suitable partial denture base material, except that it has a tendency to corrode in the oral environment. The use of a tin-nickel alloy as a protective coating for Nikalium partial dentures is described. The mechanical suita
Publikováno v:
Journal of Electroanalytical Chemistry and Interfacial Electrochemistry. 164:205-210
Dans le but d'obtention de surfaces electrocatalytiques, preparation electrochimique des revetements contenant des particules de tamis moleculaires (Linde 3A et 4A) sur des electrodes a disque tournant de carbone vitreux et de platine. Dans ce but de
Publikováno v:
Tectonophysics. 48:327-364
The eastern part of the Tasman Orogenic Zone (or Fold Belt System) comprises the Hodgkinson—Broken River Orogen (or Fold Belt) in the north and the New England Orogen (or Fold Belt) in the centre and south. The two orogens are separated by the nort
Autor:
C.G. Murray
Publikováno v:
Ore Geology Reviews. 1:315-400
The northern part of the Tasman Fold Belt System in Queensland comprises three segments, the Thomson, Hodgkinson- Broken River, and New England Fold Belts. The evolution of each fold belt can be traced through pre-cratonic (orogenic), transitional, a
Autor:
A.G. Kirkegaard, C.G. Murray
Publikováno v:
Tectonophysics. 48:299-325
The Thomson Orogen forms the northwestern segment of the Tasman Orogenic Zone. It was a tectonically active area with several episodes of deposition, deformation and plutonism from Cambrian to Carboniferous time. Only the northeastern part of the oro
Autor:
C.G. Murray
Publikováno v:
Earth and Planetary Science Letters. 9:34-38
The products of volcanism in the African rift valleys differ in composition and volume from those in the median valleys of oceanic ridges. These dissimilarities can be explained in terms of a petrogenetic model which requires a low heat flow under th
Autor:
GrahamS. Simpson, C.G. Murray
Publikováno v:
The Lancet. 210:745-749