Zobrazeno 1 - 10
of 48
pro vyhledávání: '"Chlorargyrite"'
Publikováno v:
Известия Томского политехнического университета: Инжиниринг георесурсов, Vol 329, Iss 12 (2018)
The rare abundance of natural iodine-bearing minerals of the chlorargyrite-bromargyrite series, their water solubility, comparatively small sizes, mineral forms (single micrograins, crusts, incrustations, micron-sized crystals), small hardness 1,5–
Externí odkaz:
https://doaj.org/article/29449b7c16804f6d98769e3eddd67981
Publikováno v:
Izvestiya Tomskogo Politekhnicheskogo Universiteta Inziniring Georesursov. 329:80-93
The rare abundance of natural iodine-bearing minerals of the chlorargyrite-bromargyrite series, their water solubility, comparatively small sizes, mineral forms (single micrograins, crusts, incrustations, micron-sized crystals), small hardness 1,5–
Publikováno v:
Journal of Geochemical Exploration. 195:143-156
The Dongyang gold deposit is located in Fujian Province in southeastern China, mainly hosted by a NW–SE trending Late Jurassic porphyritic rhyolite, and classified as a low-sulfidation epithermal gold deposit. The units associated with the gold min
Autor:
Aneli M. Barbosa-Dekker, Robert F. H. Dekker, Eulogio Castro, Antonio Jesús Muñoz, Encarnación Ruiz, Francisco Espínola
Publikováno v:
Journal of Hazardous Materials. 420:126598
Two biomass types of Botryosphaeria rhodina MAMB-05 (VMSM and M3) were evaluated to determine their effectiveness in removing Ag(I) ions from synthetic solutions. Both biomass types obtained good results in the biosorption process with maximum biosor
Publikováno v:
Minerals
Volume 9
Issue 12
Volume 9
Issue 12
The Oleninskoe intrusion-related gold&ndash
silver deposit is the first deposit in the Precambrian of the Fennoscandian Shield, where mustard gold has been identified. The mustard gold replaces kü
stelite with impurities of Sb and, prob
silver deposit is the first deposit in the Precambrian of the Fennoscandian Shield, where mustard gold has been identified. The mustard gold replaces kü
stelite with impurities of Sb and, prob
Autor:
Lucilla Fabrizi, Laura Medeghini, Fiorenzo Catalli, Melania Di Fazio, Caterina De Vito, Francesca Di Turo
The aim of this research was to characterize ten Provisini, one of the most common silver coins in the Middle Age, dating back to the 13th century A.D. These coins are composed by Ag-Cu alloy and were coined in the Roman mint. A non-destructive, micr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f1a32d0b99f36dce33ab1450fff915ed
http://hdl.handle.net/11573/1159308
http://hdl.handle.net/11573/1159308
Publikováno v:
Acta Geologica Sinica - English Edition. 90:1321-1340
The Gaoshan gold-silver deposit, located between the Yuyao-Lishui Fault and Jiangshan-Shaoxing fault in Longquan Area, occurs in the Suichang-Longquan gold-silver polymetallic metallogenic belt. This study conducted an investigation for ore-forming f
Autor:
Inna S. Lykova, Nikita V. Chukanov, Evgeniy A. Vlasov, Natalia V. Zubkova, Vasiliy O. Yapaskurt, Dmitry I. Belakovskiy, Andrey A. Zolotarev, Igor V. Pekov, Andrey V. Apletalin, Dmitry Yu. Pushcharovsky
Publikováno v:
European Journal of Mineralogy. 28:459-466
Raisaite, CuMg[Te 6+ O 4 (OH) 2 ] · 6H 2 O, is a new mineral found at the Sentyabr’skoe deposit, Ilirney ore district, Western Chukotka, North-Eastern Region, Russia. It is associated with gypsum, malachite, azurite, cerussite, anglesite, brochant
Autor:
Alexander V. Zotov, N. N. Akinfiev
Publikováno v:
Geochimica et Cosmochimica Acta. 178:178-194
The solubility of chlorargyrite, AgCl(cr./l.), in pure water at 623, 673 and 753 (±2) K as a function of pressure in a wide range aqueous densities (0.01–0.7 g·cm −3 ) was determined using various experimental approaches. Combined theoretical q
Publikováno v:
European Journal of Mineralogy. 28:1019-1024
The type specimen of partzite has been reinvestigated by powder X-ray diffraction and electron microprobe traverses. Re-examination of the type material shows that it is a mixture of several phases, intergrown on a submicrometre scale and hence not f