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Mineral Deposits of Turkey in Relation to Tethyan Metallogeny: Implications for Future Mineral Exploration
The LaRonde Penna Au-Rich Volcanogenic Massive Sulfide Deposit, Abitibi Greenstone Belt, Quebec: Part I. Geology and Geochronology
Abstract In 1967 and 1969, two oceanographic cruises were made in the Black Sea under the guidance of the Woods Hole Oceanographic Institute: The cruises included scientists from many countries and disciplines. Their aims were to determine the recent geological and geochemical evolution of the Black Sea, to map the shallow structure of the basin, and to study the interaction between the oxidized surface waters and the anoxic waters beneath them. The results were published 23 years ago, as AAPG Memoir 20 (Ross and Degens, 1974). During the 1969 cruise, the vessel Atlantis II collected 40 piston cores, which formed the basis of most of the subsequent geological studies that were restricted to very recent sedimentation. Speculations concerning the origin of the basin and the relationship of the geology offshore to that exposed around the margins of the Black Sea were rooted in pre-plate tectonic concepts of basin formation and were in any case hampered by a lack of relevant data (Brinkmann, 1974). In 1976, the Glomar Challenger visited the Black Sea on Leg 42B of the Deep Sea Drilling Project and drilled and cored three deep-water sites (379, 380, and 381). Well 381 north of the Bosporus encountered sediments as old as Miocene, including some apparently deposited in shallow water (Ross, 1978). The next major volume in Western literature to deal with the Black Sea was published a decade later, collecting papers presented two years earlier at a conference in Yalta. In this volume, a number of seismic reflection lines
A quantitative link among mineral deposit modeling, geoscience mapping, and exploration-resource assessment
Abstract Constructed on four sheets, each about 42 inches by 55 inches, the Geothermal Map of North America helps readers estimate uppercrustal temperatures, such as temperatures in sedimentary basins.
Abstract This volume includes sections on Mineral Deposits (7 chapters on metals and 4 on industrial minerals); Oil and Gas (3 chapters on principles and 12 synthesizing major oil and gas basins); and Coal (3 chapters on principles and 5 synthesizing major coal provinces, including Alaska). Six large plates summarize distribution resources of all resources discussed in the text, two more plates compare cross-sections of major oil and gas basins at a common horizontal and vertical scale, and another shows a major reconstruction of a Pennsylvanian coal swamp.