Zobrazeno 1 - 10
of 65
pro vyhledávání: '"D M Finlayson"'
LASER SOURCES A review of diode-pumped lasers D. Hanna and W.A. Clarkson Visible cw solid-state lasers G. Huber Fiber and waveguide lasers A. Tropper Optical parametric oscillators (OPO) M.H. Dunn and M. Ebrahimzadeh Physics of ultrashort pulse gener
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4a2fd759ae77ef9e8a172033f89d5d0
https://doi.org/10.1201/9781003209652
https://doi.org/10.1201/9781003209652
Autor:
C. E. Brown, D. M. Finlayson
Publikováno v:
Australian Journal of Earth Sciences. 66:907-911
The Woolshed Creek fossil site near the Royal Military College, Duntroon, Canberra, contains brachiopods Atrypa duntroonensis (early Homerian, early Silurian, ca 430.5 Ma) within a mudstone of the ...
Publikováno v:
Journal of Volcanology and Geothermal Research. 130:77-92
The attenuation structure around Rabaul volcano, New Britain, Papua New Guinea, is studied using broadband records from a pair of sites, inside and outside of the Rabaul caldera complex, using regional earthquakes. Estimates of attenuation for P and
Publikováno v:
Journal of Volcanology and Geothermal Research. 124:153-171
The recently active Rabaul volcano on the island of New Britain in eastern Papua New Guinea is associated with a subduction zone located near the triple junction formed by the Pacific, South Bismarck and Solomon lithospheric plates. Analysis of our 1
Autor:
Nicholas G. Direen, Richard Glen, D. M. Finlayson, K. C. Lawrie, R. J. Korsch, R. D. Shaw, L. E. A. Jones, D. W. Johnstone
Publikováno v:
Australian Journal of Earth Sciences. 49:323-348
In the Eastern Lachlan Orogen, the mineralised Molong and Junee‐Narromine Volcanic Belts are two structural belts that once formed part of the Ordovician Macquarie Arc, but are now separated by younger Silurian‐Devonian strata as well as by Ordov
Publikováno v:
Australian Journal of Earth Sciences. 49:311-321
A 2‐D crustal velocity model has been derived from a 1997 364 km north‐south wide‐angle seismic profile that passed from Ordovician volcanic and volcaniclastic rocks (Molong Volcanic Belt of the Macquarie Arc) in the north, across the Lachlan T
Autor:
D. W. Johnstone, K. D. Wake‐Oyster, D. M. Finlayson, J. H. Leven, C. D. N. Collins, C. Wright
Publikováno v:
Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::085868f3a0d0077449f3ec43071e30b2
https://doi.org/10.1029/gm048p0043
https://doi.org/10.1029/gm048p0043
Publikováno v:
Tectonophysics. 264:137-152
The Otway Basin is one of a number of basins formed along Australia's southern continental margin during the Late Jurassic-Early Cretaceous rifting of Australia from Antarctica. It lies on a transitional area of extended lithosphere between the margi
Autor:
D M Finlayson
Publikováno v:
Journal of Physics: Condensed Matter. 6:8277-8283
A negative magnetoresistance is reported for the variable-range hopping regime of a straightforward sample of CdSe. The behaviour is consistent with the theory of Nguyen et al (1985). When a fairly high concentration of Cr is added, the magnetoresist