Titlebook: Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments; Proceedings of the D Günther H. Friedrich,Peter M. Herzig Conference

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書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments影響因子(影響力)




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments影響因子(影響力)學(xué)科排名




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments被引頻次




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments被引頻次學(xué)科排名




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments年度引用




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments年度引用學(xué)科排名




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments讀者反饋




書(shū)目名稱Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments讀者反饋學(xué)科排名

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Relation of Permian Base Metal Occurrences to the Variscan Paleogeothermal Field of the Fore-Sudeticerous, older Paleozoic, and Precambrian basement rocks of the Fore-Sudetic Monocline of southwest Poland. Surprisingly high temperatures determined for these processes (ranging from 180 to 350°C), and the locally extensive alteration indicate the importance of geothermal influence. The high-temperat

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Base Metal Mineralization and Maturation of Organic Material in the Kupferschiefer of the Lower Rhin covers a region of 600 km.. It represents the most southern part of the former Zechstein sea in this area and is situated north of the Rhenohercynian zone in the sub-Variscan foreland of the Variscan Mountains. The folded Carboniferous rocks of the Variscan basement are discordantly overlain by the

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The Origin of the Kipushi (Cu, Zn, Pb) Deposit in Direct Relation with a Proterozoic Salt Diapir. Coal wealth and its economic importance. This is also the case of the uranium deposit of Shinkolobwe (U, Ni, Co, Au, R.E.E., Pd, Pt), which is situated in the central part of the copper belt..Both are clearly epigenetic and are located in the sedimentary rocks of the Katanga System (Upper Proterozoic)

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