Publications

Borowitzka, MA & Larkum, AWD 1974, 'Chloroplast development in the caulerpalean algaHalimeda', Protoplasma, vol. 81, no. 2-3, pp. 131-144.
View/Download from: Publisher's site

Larkum, AWD & Boardman, NK 1974, 'The effect of nigericin and valinomycin on CO₂ fixation electron transport and P518 in intact spinach chloroplasts', FEBS Letters, vol. 40, no. 1, pp. 229-232.
View/Download from: Publisher's site

Leitch, EC 1974, 'The geological development of the southern part of the New England Fold Belt', Journal of the Geological Society of Australia, vol. 21, no. 2, pp. 133-156.
View/Download from: Publisher's site
View description>>

Two major divisions of the New England Fold Belt, Zone A and Zone B, are separated by the Peel Fault. Deposition in these two zones was probably contemporaneous (Lower Palaeozoic - Lower Permian). Terminal orogenesis in both zones was also contemporaneous (Middle Permian) but whereas in Zone A deformation was only moderate, metamorphism was of burial type, and granitic emplacement was uncommon, in Zone B many rocks were severely deformed and regionally metamorphosed, and both syn-tectonic and post-tectonic granites are widespread. Pre-orogenic palaeogeography is envisaged in terms of an evolving volcanic chain - fore-chain basin - trench system, with an outer non-volcanic arc developed in the Carboniferous. Cessation of movement on a subduction zone dipping westward beneath the volcanic chain is believed to have caused the Middle Permian deformation, but neither metamorphism nor the granitic rocks are directly related to subduction. © Taylor & Francis Group, LLC.

Mueller, PH & Platen, E 1974, 'Rank Strategies in Sequential Selection Problems.', Wiss Z Tech Univ Dres, vol. 23, no. 5, pp. 1069-1076.
View description>>

A Bellman equation for the determination of an optimal strategy is derived for the so-called ″optimum selection problem″ , under the assumption of an existing rank sequence for individual objects. This ″optimum selection problem″ involves the selection of m from n sequentially observable objects without the possibility of supplementary examination. the method is based on an additive result functional whose The results, in case of the selection of an object, depend on their rank number, on the number of the already observed and on the number of the already selected objects. In the majority of practical applications, the elementary result is a monotonous function of the rank number. It is shown that optimum strategy is pure strategy and, in the case of a monotonous results functional, it is, moreover, a so-called simple strategy. These optimal simple strategies can be relatively easily represented. Some special sequential selection problems are solved.

SABINE, TM, SMITH, GB & REEVE, KD 1974, 'CRITICAL CONCENTRATION FOR MAGNETIC ORDER IN SOLID-SOLUTIONS OF UO2 WITH THO2 AND ZRO2', JOURNAL OF PHYSICS C-SOLID STATE PHYSICS, vol. 7, no. 24, pp. 4513-4521.
View/Download from: Publisher's site

Winterer, EL, Lonsdale, PF, Matthews, JL & Rosendahl, BR 1974, 'Structure and acoustic stratigraphy of the Manihiki Plateau', Deep Sea Research and Oceanographic Abstracts, vol. 21, no. 10, pp. 793-813.
View/Download from: Publisher's site