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Wayne Andersen 《European Legacy》2005,10(2):163-175
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Since the 1949 introduction of proportional representation for the Senate there have only been two elections (1983 and 84) at which the ALP has gained more Senators in the chamber than the Coalition. The Coalition has held more seats than the ALP since 1987. The decline in Senate fortunes for the Labor Party has occurred despite (or, perhaps, because of) consecutive ALP Governments from 1972–75 and, more conspicuously, 1983–96. The professionalisation of politics through the 1980s and 1990s has dramatically changed the role major parties expect of their Senate teams. The Coalition and Labor Parties each use their Senators and Senatorial office resources as ‘shock troops’ in marginal seats, as well as points of constituency contact for electors in marginal seats or seats held by the opposition. Given that major party Senators are increasingly being used by the party machines as campaign tools, and are increasingly locating their offices and staffers in marginal seats, the numerical advantage the Coalition enjoys in the Senate is worthy of consideration. The additional campaign resources that Senators provide translates potentially into an electoral advantage in the House of Representatives for the Coalition. The Coalition's majority in the Senate may therefore be of as much interest outside the chamber as it is within it. 相似文献
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P. Upton D. Craw T. G. Caldwell P. O. Koons Z. James P. E. Wannamaker G. J. Jiracek C. P. Chamberlain 《Geofluids》2003,3(1):1-12
The currently active fluid regime within the outboard region of the Southern Alps, New Zealand was investigated using a combination of field observations, carbon‐ and oxygen‐stable isotopes from fault‐hosted calcites and interpretation of magnetotelluric (MT) data. Active faulting in the region is dominated by NE striking and N striking, oppositely dipping thrust fault pairs. Stable isotopic analyses of calcites hosted within these fault zones range from 10 to 25‰δ18O and from ?33 to 0‰δ13C. These values reflect mixing of three parent fluids: meteoric water, carbon‐exchanged groundwater and minor deeper rock‐exchanged fluids, at temperatures of 10–90°C in the upper 3–4 km of the crust. A broad, ‘U‐shaped’ zone of high electrical conductivity (maximum depth c. 28 km) underlies the central Southern Alps. In the ductile region of the crust, the high‐conductivity zone is subhorizontal. Near‐vertical zones of high conductivity extend upward to the surface on both sides of the conductive zone. On the outboard side of the orogen, the conductive zone reaches the surface coincident with the trace of the active Forest Creek Faults. Near‐surface flow is shown to dominate the outboard region. Topographically driven meteoric water interacts, on a kilometre scale, with either carbon‐exchanged groundwater or directly with organic material within Pliocene gravels, resulting in a distinctive low 13C signal within fault‐hosted calcites of the outboard region. The high‐strain zone in the lower crust focuses the migration of deeply sourced fluids upward to the base of the brittle–ductile transition. Interconnected fluid is imaged as a narrow vertical zone of high conductivity in the upper crust, implying continuous permeability and possibly buoyancy‐driven flow of deeply sourced fluids to higher levels of the crust where they are detected by the isotopic analysis of the fault‐hosted calcites. 相似文献
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Lazar JW 《Journal of the history of the neurosciences》2008,17(4):442-460
Three American neurologists (C. K. Mills, C. L. Dana, and M. A. Starr) explored the anatomical limits of the motor and tactile systems in the brain from 1884 to 1895. Their papers and critiques of one another show contemporary knowledge, limits of their thinking, and difficulties deciding between alternatives. The issue for them was whether there were separate sensory and motor regions or whether there was a combined sensory-motor region. They based their localization arguments on clinical and laboratory findings and on the conclusions of H. Munk and D. Ferrier. There is a discussion about why differences were unresolved. 相似文献
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J. Wayne Lazar 《Journal of the history of the neurosciences》2018,27(2):145-164
Henry Herbert Donaldson (1857–1938) was a leader in neurological research in the United States for several decades, beginning about 1890. A detailed account of three of his earliest publications shows the neuroanatomical procedures involved in the study of the relation of brain and intelligence during the late-nineteenth-century in America. Two of the articles, published in September 1890 and December 1891, were titled, “Anatomical Observations on the Brain and Several Sense-Organs of the Blind Deaf-Mute, Laura Dewy Bridgman (1829–1889)”; the third, published in August 1892, used the information from the first two to delimit the extent of the visual processing area of the human cortex. Donaldson’s procedures included brain cuttings and measures of macroscopic brain structures, histology of cellular structures, attempts to relate macroscopic brain structures with brain functions, data corrections, estimations, comparisons, and statistics. These procedures provide a view of the relative thoroughness, accuracy, and comparability of the various neuroanatomical techniques in use at that time and of Donaldson’s implementation of the techniques. Donaldson’s brain cutting techniques were much more comparable than his measurement techniques. The latter could be quite precise, but they were fraught with lack of standardized procedures that made corrections and estimations necessary when making data comparisons across studies. Donaldson emphasized these incompatibilities, implying a need for standardization. Statistical procedures were the least thorough and effective. His, and the field’s, total complement of statistical techniques consisted of mean and range, which severely limited his ability to make complicated assessments. This limitation was not necessarily supplemented by stringent control group comparisons. 相似文献