| | Journal (article/letter/editorial) | Mo deposits in Northwest China: Geology, geochemistry, geochronology and tectonic setting...Yan-Jing, Zhou, Ke-Fa, Mo deposits in Northwest China: Geology, geochemistry, geochronology and tectonic...Northwest China: geology, geochemistry, IP T geochronology and tectonic setting a Xinjiang Research...Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Key Laboratory of Orogen...Beijing 100871, China State Key Laboratory of Geological Processes and Mineral Resources, China University | | | Report (volume) | Aspects of the Tectonic Evolution of China Geological Society Special Publications Society Book Editors...(eds) 2004. Aspects of the Tectonic Evolution of China. Geological Society, London, Special Publications... C. (eds) Aspects of the Tectonic Evolution of China. Geological Society, London, Special Publications...PUBLICATION NO. 226 Aspects of the Tectonic Evolution of China E D I T E D BY J. MALPAS, C. J. N. FLETCHER, J...G. Determining Precambrian crustal Evolution in China: a case-study from Wutaishan, Shanxi Province, demonstrating | | | Journal (article/letter/editorial) | A1141 Mineralogy, chemistry and distribution of mine tailings from the Murgul (Artvin) Cu deposit and...edu.tr) Murgul Cu deposit is the largest copper mine of Turkey and is in production since pre-Republican...impact of mine tailings disposed of into the streams draining the deposit. Due to disposal of mine waste...the streams, particles originating from the Murgul mine are highly enriched in the alluvium. Stream sediment...to quartz content due to dilution at times of no-mine production. However, the second group of samples | | | Journal (article/letter/editorial) | (clinochloreādaphnite), tremolite (tremoliteāFe-actinolite) and carbonate (magnesiteāsideriteācalcite)....mineral carbonation including mineral carbonation of mine tailings, the formation of soapstone and listvenitization...mineralogy with reference to an occurrence at Cregganbaun, Co. Mayo, Republic of Ireland. Mineralium Deposita 30...Geology 26, 375ā378. Klein, F., Bach, W., 2009. FeāNiāCoāOāS phase relations in peridotite seawater interactions...and origin of listwanites in the Sartohay and Luobusa Ophiolites, China. International Geology Review 47 | | Menzel, Manuel D., Garrido, Carlos J., LĆ³pez SĆ”nchez-VizcaĆno, Vicente, Marchesi, Claudio, Hidas, KĆ”roly, Escayola, Monica P., Delgado Huertas, Antonio (2018) Carbonation of mantle peridotite by CO2-rich fluids: the formation of listvenites in the Advocate ophiolite complex (Newfoundland, Canada) Lithos, 323. 238-261 doi:10.1016/j.lithos.2018.06.001 | Journal (article/letter/editorial) | Service (Canada). Major elements (ISO-accredited) and Co, Cu, Cr, Ni, V, and Zn were measured by X-ray fluorescence...to talc-carbonatetremolite schists, fuchsite-actinolite schists and listvenites (van Staal et al., 2013)...conditions (as indicated by the stability of tremolite/actinolite). CR The internal structure of the Central...mineralogy with reference to an occurrence at Cregganbaun, Co Mayo, Republic-of-Ireland. Mineralium Deposita 30...mineralization in the Sayi gold deposit, Xinjiang, NW China. Ore Geology Reviews 70, 61-79. Quesnel, | | SƤntti, Jaakko, Kontinen, Asko, Sorjonen-Ward, Peter, Johanson, Bo, Pakkanen, Lassi (2006) Metamorphism and Chromite in Serpentinized and Carbonate-Silica-Altered Peridotites of the Paleoproterozoic Outokumpu-Jormua Ophiolite Belt, eastern Finland. International Geology Review, 48 (6) 494-546 doi:10.2747/0020-6814.48.6.494 | Journal (article/letter/editorial) | rocks are intimately associated with the Outokumpu Cu-Co-Zn-Ni deposits and have generally been regarded as...known for hosting several economically important Cu-Co-Zn sulfide deposits (GaĆ”l and Parkkinen, 1993). The...rock transported from the nearby, abandoned talc mine. The size and distribution of the chromitite blocks...and 3 chromites, particularly in proximity to Cu-Zn-Co sulfide ores, although this is not invariably the...Sp + Fo + En + H2O, Al-Chl out and En + Sp = Fo + Co (Fawcett and Yoder, 1966; Jenkins and Chernosky, |
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