Zobrazeno 1 - 8
of 8
pro vyhledávání: '"F. C. Beavis"'
Autor:
F. C. Beavis
Publikováno v:
Australian Journal of Earth Sciences. 39:249-249
(1992). Discussion: Major fault zones related to the Omeo Metamorphic Complex, northeastern Victoria by V. J. Morand and D. R. Gray. Australian Journal of Earth Sciences: Vol. 39, No. 2, pp. 249-249.
Publikováno v:
Quarterly Journal of Engineering Geology. 11:279-290
Summary Embankment stability, inadequate catchment areas, seepage losses and high salinity are the main problems in the successful construction of small water storages in arid and semi-arid regions. It is essential for success that storages be correc
Autor:
F. C. Beavis
Publikováno v:
Journal of the Geological Society of Australia. 22:447-455
Three Australian Ordovician graptolite faunas are described; the short‐lived Anisograptid Fauna is followed by the Dichograptid Fauna, which in turn is succeeded by the Diplograptid Fauna. The Dichograptid Fauna consists of two sub‐faunas, the Te
Autor:
F. C. Beavis
Publikováno v:
Journal of the Geological Society of Australia. 28:191-204
Two bores were drilled in the weathered zone of a Precambrian dolomite at Fowler's Gap, 100 km N of Broken Hill, New South Wales. Five weathering units have been distinguished: fresh dolomite; weathered dolomite, type B; weathered dolomite, type A; f
Publikováno v:
Quarterly Journal of Engineering Geology. 15:29-45
Summary Examination of the weathered rock profile of low grade metapelites in arid Australia illustrates changes due to two different weathering environments. The most significant was a period of high rainfall which resulted in some important changes
Autor:
F. C. Beavis
Publikováno v:
Geological Magazine. 109:193-204
SummaryThe reference of Isograptus manubriatus (T. S. Hall) to the genus Maeandrograptus Moberg by Skevington (1968) is argued to be invalid. A new genus, Pseudisograptus has been introduced to which the manubriate isograptids I. manubriatus, I. hast
Autor:
F. C. Beavis
Publikováno v:
Geological Magazine. 107:429-438
SummaryTwo cleavages occur in the sandstones: coarse fissuring, and a fine irregular fracturing, which may form conjugate sets. Linear structures of five styles, all of which are parallel to the fold axis, are developed on the bedding due to the inte
Autor:
F. C. Beavis
Publikováno v:
Geological Magazine. 101:504-511
At a late stage of folding, strain slip cleavage was imposed on the pelitic sediments of the Ordovician greywacke-slate association in Central Victoria. The nature of the cleavage surfaces was controlled by the type of sediment in which they were dev