نتایج جستجو برای: cu fe skarn
تعداد نتایج: 131158 فیلتر نتایج به سال:
Garnet is the most abundant calc-silicate mineral in the Darreh Zereshk skarns, and occurs as grained euhedral, to massive anhedral, isotropic to anisotropic crystals and display concentric and sector zoning or no zoning. Based on mineralogical investigations and paragenetic relations, garnet formed during progrademetasomatic stage of skarn formation. Geochemically they display two different pa...
the cheshin meta-calcareous rocks (permo triassic) in southeast hamedan outcrop in association with a variety of pelitic schists and hornfels rocks. the intrusion of the alvand batholith (jurassic age) into pelitic and calcareous host rocks has produced metamorphic rocks in the hamedan area (cheshin village). on the basis of the dominance of calcite/dolomite, silicate and ore minerals, the calc...
Campiglia Marittima Skarn (Tuscany): A Challenging Example for the Evolution of Skarn-Forming Models
Campiglia Marittima (hereafter Campiglia) has a long record of attracting interest on its ore deposits that have been intermittently exploited from the Copper Age to late XX century. Since XIX century, key locality for debate skarn-forming processes due presence mining activities ensuring access ever new rock exposures. The pioneering study vom Rath and comparison with attractive chemical model...
در این پژوهش بس لایه های co-cu/cu و fe-co-cu/cu بر روی زیر لایه شیشه /طلا به روش الکتروانباشت لایه نشانی گردید. ناهمواری های سطحی این لایه ها به وسیله میکروسکوپ نیروی اتمی بررسی شده و سپس با رسم نمودار ناهمواری سطحی بر حسب طول اسکن در مقیاس لگاریتمی نوع و اندازه ناهمواری های سطحی مورد محاسبه قرار گرفت. ساختار بس لایه ها توسط پراش اشعه ایکس مورد مطالعه قرار گرفت و پیک های مشخصه و ساختار بلوری لا...
Abstract New mineralogical, geochemical, and geochronological data are presented for the Island Dam prospect, Olympic Cu-Au Province, South Australia. Skarn assemblages comprising actinolite/phlogopite + K-feldspar magnetite suggest presence of calcareous protoliths at indicate high-temperature alkali-calcic alteration in early stages IOCG mineralization, as seen other deposits region. Dating l...
The Hunt Mo skarn deposit is one of the best examples of a late tectonic, granitic pegmatite-related, skarn system in the Grenville province. An Re-Os age of 1069 ± 11 Ma was obtained from a molybdenite crystal (6.4 ppm Re) hosted in proximal skarn (sample 50O) consistent with a contact metasomatic origin related to the granitic body. Although less evolved than other Grenvillian pegmatites, the...
Regional setting and geochronology of the Late Cretaceous Banatitic Magmatic and Metallogenetic Belt
Abstract The 1,500-km-long Banatitic Magmatic and Metallogenetic Belt (BMMB) of Romania, Serbia and Bulgaria is a complex calc-alkaline magmatic arc of Late Cretaceous age. It hosts a variety of magmatic-hydrothermal Cu, Au, Mo, Zn, Pb and Fe deposits, including Europe’s only world-class porphyry-copper deposits. Regional metallogeny can be linked to subduction of the Vardar Ocean during the La...
Khut skarn deposit, located in the 50 Km NW of Taft,has formedin the result of Khut granodiorite intrusion into the upper Triassic impure carbonate rocks.Field evidences and mineralogical studies show Khut skarn is calcic type and exoskarn is the major skarn zone in area which associated with ore mineralization.The microprobe analyses show that there are two major types of garnet at garnet-pyro...
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