The identification of gamma ray induced EAS

Some of the penetrating particles in gamma-induced EAS from Cygnus X-3 observed by a single layer of flash-bulbs under 880 g cm/2 concrete, may be punched through photons rather than muons. An analysis of the shielded flash-tube response detected from EAS is presented. The penetration of the electro-magnetic component through 20 cm of Pb is observed at core distances approx. 10 m

2-Player Nash and Nonsymmetric Bargaining Games: Algorithms and Structural Properties

The solution to a Nash or a nonsymmetric bargaining game is obtained by maximizing a concave function over a convex set, i.e., it is the solution to a convex program. We show that each 2-player game whose convex program has linear constraints, admits a rational solution and such a solution can be found in polynomial time using only an LP solver. If in addition, the game is succinct, i.e., the coefficients in its convex program are ``small'', then its solution can be found in strongly polynomial time. We also give a non-succinct linear game whose solution can be found in strongly polynomial time

Stories in distress: Three case studies in Australian media coverage of humanitarian crises

This article reviews three case studies in the Australian media reporting of international humanitarian crises. The case studies cover a six-month period in 1999 and draw on all media over that period. Thethree case studies are: the violence in East TImor at the time of the 1999 independence ballot, the imprisonment in Yugoslavia of Prall and Wallace, two employees of CARE Australia, and the floods in Mozambique. While the three case studies collectively exhibit many of the standard characteristics ofmedia coverage ofhumanitarian issues, individually they differ significantly in the scale and orientation ofcoverage. Wesuggest that a significantfactor in these differences was the relationship between the sources for the stories and the journalists, which in turn depended on other factors. We review the adequacy of the Hall and Ericson positions on the source-journalist relationship in explaining these differences, and suggest that a field analysis derivedfrom Bourdieu is helpful in explaining the involvement ofsources from the political, economic and military fields, which in turn impacted on the relationship ofthe media to the stories

Chemical Trends in the Ice Springs Basalt, Black Rock Desert, Utah

The Holocene Ice Springs volcanic field of west-central Utah consists of 0.53 km3 of tholeitic basalts erupted as a sequence of nested cinder cones and associated lava flows. Whole rock x-ray fluorescence and atomic absorption analysis of ninety-six samples of known relative age document statistically significant inter- and intra- eruption chemical variations. Elemental trends include increases in Ti, Fe, Ca, P, and Sr and decreases in Si, K, Rb, Ni, Cr, and Zr with decreasing age. Microprobe analyses of microphenocrysts of olivine, plagioclase, and Fe-Ti oxides and of groundmass olivine, plagioclase, and clinopyroxene indicate limited chemical variation between mineral assemblages of the eruptive events. Petrographic analyses have identified the presence of minor amounts of silicic xenoliths, orthopyroxene megacrysts, and plagioclase xenocrysts. Potassium-argon determinations establish the existence of excess argon in the basaltic cinder (30.05 x 10 -12 moles/gm) and in distal lava flows (8.29 x 10 -12 moles/gm) which suggest apparent ages of 16 and 4.3 million years respectively. Strontium isotopic data (Puskar and Condie, 1973) show systematic variations from oldest eruptions (87Sr/86Sr=0.7052) to youngest eruptions (87Sr/86Sr=0.7059). Theoretical evaluation of observed major element, trace element, isotopic, and thermophysical properties of the lavas and cinders limits the importance of proposed magmatic differentation processes. The data are compatible with model involving crystal fractionation, crustal assimilation, and magma mixing. Initial modification of mantle derived melts resulted from olivine fractionation at depth. Subsequent combination of 6 to 8% fractionation of plagioclase, minor olivine, and magnetite at shallow depths, less than one percent assimilation of silicic crustal basement rocks, and interaction of compositionally similar magma pulses explains the overall inter-eruption chemical trends. The intra-eruption variations follow the overall trends and a similar combination of processes of lesser magnitude accounts for the intra-eruption variations

Average features of the muon component of EAS or = 10(17) eV

Three 10 sq m liquid scintillators were situated at approximately 0 m, 150 m and 250 m from the center of the Haverah Park array. The detectors were shielded by lead/barytes giving muon detection thresholds of 317 MeV, 431 MeV and 488 MeV respectively. During part of the operational period the 431 MeV threshold was lowered to 313 MeV for comparison purposes. For risetime measurement fast phototubes were used and the 10% to 70% amplitude time interval was parameterized by T sub 70. A muon lateral density distribution of the form rho mu (R theta) = krho(500)0.94 1/R(1 + R/490)-eta has been fitted to the data for 120 m R 600 m and 0.27 (500) 2.55. The shower size parameter (500) is the water Cerenkov response at 500 m from the core of the extensive air showers (EAS) and is relatable to the primary energy. The results show general consistency