Mineral Deposit Research: Meeting the Global Challenge: Proceedings of the Eighth Biennial SGA Meeting, Beijing, China, 18 - 21 August 2005Jingwen Mao, Frank P. Bierlein In June 1965, a small group of European economic geologists gathered in Heidelberg, Germany, at the invitation of Professor G. C. Amstutz and decided to establish the Society for Geology Applied to Mineral Deposits (SGA) and to start a journal to be called Mineralium Deposita. The first issue of the journal came out in May 1966, and has now matured to a leading journal in economic geology The first Biennial SGA Meeting was held successfully in Nancy, France, in 1991, with subsequent meetings in Grenada (Spain; 1993), Prague (Czech Republic; 1995), Turku (Finland; 1997), London (United Kingdom; 1999), Krakov (Poland; 2001) and Athens (Greece; 2003). In 2002, th the SGA Council decided that its 8 Biennial Meeting in 2005 should be held in Beijing, China, making this the first Biennial Meeting to be convened outside - th rope. Significantly, 2005 also marks the 40 anniversary of the SGA. The decision to host this year’s premier meeting in Beijing reflects the Society’s successful transition from its traditional European focus to a truly global organization, with 24% of SGA members situated in North America, 13% in Australia and Oceania, and 5% in Asia. Over the last 27 years China has made dramatic progress towards political and economic reform, and opening the nation to the outside world. China’s rapid e- nomic development demands increasing amounts of minerals, fuels and materials, and this is currently a major driver for the global economic markets. |
Contents
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Chapter 18 Synchronous vertical and horizontal tectonism during the late stage | 29 |
Chapter 115 New classification of magmatic sulphide deposits in China | 57 |
Chapter 117 Mineral systems hydridic fluids the Earths core mass extinction events | 65 |
Chapter 119 Modes of occurrence of H2 in mantlederived rocks | 75 |
Chapter 21 Iron transport in redbeds during the genesis of sedimenthosted | 85 |
Chapter 23 Diagenetic origin of the Luzhou copper deposit Yunnan Province China | 91 |
Chapter 25 Stratiform Sb and Au mineralizations in the Hercynian DúricoBeirã area | 97 |
Chapter 433 Mineral chemistry of FeTi oxides from the Xinjie PGEbearing layered | 481 |
Chapter 435 The Shaxi porphyry CuAu deposit Anhui Province eastern China | 491 |
Chapter 439 REENb Fe UThbearing alkaline skarns of China | 507 |
The Worlds first reported sedimenthosted thalliumonly deposit | 515 |
Chapter 52 Models for epigenetic gold exploration in the northern Cordilleran Orogen | 525 |
Chapter56 Age and origin of advanced argillic alteration at the Bor CuAu deposit Serbia | 541 |
Chapter 58 Carlinlike gold mineralization in the Gaspé Peninsula Canadian Appalachians | 551 |
Chapter 510 Deformation history and multiple gold mineralisation events | 557 |
Chapter 28 FluidsystemandoreformingdynamicsoftheYuebeiBasinChina | 107 |
Interplay between | 115 |
Chapter 212 Geochemistry and provenance of clastic metasedimentary host rocks | 125 |
Chapter 217 Origin and significance of calcitemarcasitepyrite mineralisation in siliciclastic Lower | 140 |
Chapter 221 Geological and geochemical characteristics of the Changba | 157 |
Chapter 225 Origin of the Nchanga coppercobalt deposits of the Zambian Copperbelt | 171 |
Chapter 229 Geochemistry and gold content of the Triassic cabonaceous cherts | 187 |
Chapter 231 Preliminary study of the source of base metals in MVT deposits | 197 |
Chapter 235 Mirrorimage coupling between sedimentary depression and | 211 |
Chapter 31 Geochemistry geothermometry and KAr dating of episyenitic rocks | 227 |
Chapter 311 Study of methods and techniques of aeroradiometric weak information | 261 |
Chapter 315 Hydrothermal alteration of the graphitized organic matter | 279 |
Chapter 317 Features of mylonite and its relationship to uranium oreformation | 285 |
Chapter 320 New discovery in the study of remote sensing image characteristics | 295 |
Chapter 322 Uranium deposits in the Arlit area Niger | 303 |
Chapter 324 Reduction of fluids in the Bashbulak sandstone type uranium deposit | 311 |
Chapter 327 Late MesozoicCenozoic tectonosedimentary evolution | 319 |
Chapter 329 Geology and origin of the Dongsheng uranium deposit in the Ordos basin | 327 |
Chapter 334 Alkalimetasomatism and uranium mineralization | 345 |
Chapter 41 Factors controlling palladium and gold contents in the Aksug | 353 |
Chapter 43 Endoskarn and CuZn mineralization at the Empire mine Idaho USA | 363 |
Chapter 45 Copper mineralization in the western Longbohe area SE Yunnan China | 369 |
Chapter 49 Geochemical characteristics and genesis of Narich rocks in the Bayan | 385 |
Chapter411 Timing of volatile and magma ascent in the formation | 393 |
Chapter 413 Three largescale metallogenic events related to the Yanshanian Period | 401 |
Chapter 415 Geochemical characteristics of ores from the Tangziwa deposit | 408 |
Chapter 417 PbZnCu mineralization in the Filfila Massif northeastern Algeria | 419 |
Chapter 419 Numerical simulations of heat and mass transfer for the Tongchang | 425 |
Chapter 421 A study of clay mineralogy and illite Kübler index with | 432 |
Chapter 423 Rutile the tintungsten host in the intrusive tourmaline breccia | 443 |
Chapter 425 The La Fortuna CuAu porphyry deposit Chile | 451 |
Chapter427 Nodular chromite deposits in some Tethyan ophiolites | 457 |
Chapter 429 Magmatic sulfide deposits in the Permian Emeishan large igneous province | 465 |
Chapter 511 Structural control of mineralization in metamorphic core complexes | 563 |
Chapter 513 New observations on WSbAu mineralization at Woxi western Hunan China 569 | 571 |
Chapter 515 Tectonic setting ofepithermal deposits in mainland China | 577 |
Chapter 517 Analysis of Au content in sedimentary rocks around | 585 |
A key to tectonic evolution | 593 |
Chapter 63 Geological features and sulphur isotope study of the Meixianstyle | 607 |
Chapter 66 Massive sulfide deposits in continental volcanic basins | 621 |
Chapter 68 Volcanic stratigraphy chemical stratigraphy and alteration system | 627 |
Chapter 610 Ttype mineralisation a pseudoepithermal style of VHMS | 635 |
Chapter 612 Transport and deposition of selenium in felsic volcanichosted massive | 643 |
Chapter 614 Backarc basin constraints on the genesis of Ordovician volcanogenic massive | 651 |
Chapter 616 Unraveling mineral isotope signatures from wholerock oxygen | 659 |
Chapter 617 Osmium isotope systematics in the Iberian Pyrite Belt | 665 |
Chapter 619 Local and regional geochemical variations in VHMSrelated | 671 |
Chapter 620 Volcanic sequences lithostratigraphy and geochemistry of altered rocks | 674 |
Chapter 624 Felsic pyroclastic and effusive volcanic facies hosting the Neves Corvo | 691 |
Chapter 626 Trace and rare earth element chemistry of garnet and apatite as discriminant | 699 |
Chapter 628 Gold and silver in CuZn massive sulphide deposits of the Urals | 709 |
Chapter 631 Anhydritepyritemagnetitepyroxenetype deposits in volcanic basins | 719 |
Chapter 74 A nonmagmatic component in fluids of South American | 737 |
Chapter 75 Origin of hydrothermal oreforming processes in the Dapingzhang | 739 |
Chapter 79 Potassic alteration and veining and the age of copper emplacement | 755 |
Chapter 714 Geochemical characteristics of HeAr and Pb isotopes in the Dajiangping | 773 |
Chapter 718 The ReOs age for molybdenite from the Variscan StrzegomSobótka massif | 789 |
Chapter 721 Jurassic magmatism and AuAg mineralization in the Deseado Massif | 803 |
Chapter 727 Constraints on the source and evolution of mineralising fluids | 825 |
Chapter 729 Metamorphic to magmatic transition captured at the Myszków MoW deposit | 833 |
Chapter 731 Sources of rhenium and osmium enrichment in fumaroles | 841 |
Chapter 733 Stable isotope composition of the Dalucao rare earth deposit | 849 |
Chapter 734 Preliminary study on the Chinese continental mineralization system | 855 |
Fractionates | 863 |
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Common terms and phrases
Abstract activity alteration amounts analysis associated Australia base basin belt bismuth bodies carbonate changes characteristics China Chinese complex composition concentrations consists contain contents controlled copper crust crystals deposits developed distribution early Earth eastern elements enrichment et al evolution exploration fault field fluid fluid inclusions formation formed geochemistry Geol Geological gold gold deposits grains granite Group host hydrothermal important inclusions indicate intrusions isotope late layers lead located lower magmatic mainly major mantle massive metal metamorphic mineralization North occur ore-forming orebodies origin oxide phase porphyry posits present processes Province pyrite quartz range ratios region relatively Research rocks salinity samples sandstone Science sedimentary sediments sericite setting significant similar skarn South stage structure suggest sulfide sulphide tectonic temperature textures thick tion units University upper uranium uranium deposits values veins volcanic western zone
Popular passages
Page 16 - Natapov, .LM, 1999. Layered mantle lithosphere in the Lac de Gras Area, Slave craton: composition, structure and origin. J. Petrol. 40, 705-727.