Reports on the results of dredging under the supervision of Alexander Agassiz in the Gulf of Mexico (1877-78), in the Caribbean Sea (1878-79), and along the Atlantic Coast of the United States (1880) by the U.S. Coast Survey steamer "Blake".

v.19:no.2 (1897)

Being a map of the town of Winchester in the state of Massachusetts, U.S.A. as it is in the year nineteen hundred and twenty nine

drawn by Ernest Dudley Chase ; issued by the Winchester National Bank.

U, FE, AND LI ISOTOPE RATIOS IN THE MINERALIZED AND BARREN AREAS OF THE KOMBOLGIE BASIN

The Paleo- to Meso-Proterozoic Jabiluka unconformity related uranium mine is located within the Alligator River Uranium Field, found in the Northern Territories, Australia. The uranium ore is hosted in the late middle Paleoproterozoic Cahill Formation, which is unconformably overlain by a group of unmetamorphosed conglomerates known as the Kombolgie subgroup. The Kombolgie subgroup provided the source for oxidized basinal brines, carrying U as the mobile form U(VI), which interacted with reducing lithologies in the Cahill formation, thus reducing U(VI) to the solid U(IV), and leading to the precipitation of uraninite (UO2). In order to characterize fluid interaction with the ore body and compare that to areas without mineralization, several isotopic tracers were studied on a series of clay samples from drill core at Jabiluka as well as in barren areas throughout the ARUF. Among the potential tracers, three were selected: U (redox sensitive and recent fluid mobilization), Fe (redox sensitive), and Li (fractionated by hydrothermal fluids and adsorption reactions). δ238U values were found to be closely linked to the mineralogy, with samples with higher K/Al ratios (indicating high illite and low chlorite concentrations) having higher δ238U values. This demonstrates that 235U preferentially absorbs onto the surface of chlorite during hydrothermal circulation. In addition, δ234U values lie far from secular equilibrium (δ234U of 30‰), indicating there was addition or removal of 234U from the surface of the samples from recent (<2.5Ma) interactions of mobile fluids. δ57Fe values were found to be related to lithology and spatially to known uranium deposits. Decreasing δ57Fe values were found with increasing depth to the unconformity in a drill hole directly above the ore zone, but not in drill holes in the barren area. Similarly to δ238U, δ7Li is found to correlate with mineralogy, with higher δ7Li values associated with samples with more chlorite. In addition, higher δ7Li values are found at greater depth throughout the basin, indicating that the direction of the mineralizing fluid circulation was upwards from the Cahill formation to the Kombolgie subgroup.

Divided but United: European Trade Policy & EC-U.S. Agricultural Negotiations in the Uruguay Round. CES Germany & Europe Working Papers, No. 07.3, 1996

How has the integration of trade policy and negotiating authority in Europe affected the external bargaining capabilities of the European Community (EC)? This paper analyzes the bargaining constraints and opportunities for the EC created by the obligation to negotiate as a single entity. The nature of demands in external~ the voting rules at the EC level, and the amount of autonomy exercised by EC negotiators contribute to explaining, this paper argues, whether the EC gains some external bargaining clout from its internal divisions and whether the final international agreement reflects the position of the median or the extreme countries in the Community. The Uruguay Round agricultural negotiations illustrate the consequences of the EC's institutional structure on its external bargaining capabilities. Negotiations between the EC and the U.S. were deadlocked for six years because the wide gap among the positions of the member states at the start of the Uruguay Round had prevented the EC from making sufficient concessions. The combination of a weakened unanimity rule and greater autonomy seized by Commission negotiators after the May 1992 reform of the Common Agricultural Policy made possible the conclusion of an EC-U.S. agricultural agreement. Although the majority of member states supported the Blair House agreement, the reinstating of the veto power in the EC and the tighter member states' control over the Commission eventually resulted in a renegotiation of the U.S.-EC agreement tilted in favor of France, the most recalcitrant country.