نتایج جستجو برای: secondary minerals
تعداد نتایج: 324064 فیلتر نتایج به سال:
The Fragnè mine, located in the Lanzo valley municipality of Chialamberto (Turin, Piedmont Region), represented most important regional site for Fe–Cu sulfide exploitation over a period more than eighty years (1884–1965). entire mining area is part structural complex Lower Unit Western Alps, characterized by presence amphibolite, metabasite (“prasinite”), and metagabbroic rocks. In particular, ...
Identification of phyllosilicates on Mars suggests the existence an aqueous environment, indicating active period in its evolutionary history. This study analysed surface mineralogy caldera and flank regions Tharsis Montes using remote spectral analysis. Though a thick layer dust obscures volcanic province, relatively lesser provide unique window for exploration. The reflectance data obtained f...
Thallium is a highly toxic metal and predominantly hosted by sulfides associated with low-temperature hydrothermal mineralization. Weathering oxidation of generate acid drainage high concentration thallium, posing threat to surrounding environments. may also be incorporated into secondary sulfate minerals, which act as temporary storage for thallium. We present state-of-the-art review on the fo...
The Damanghor gold mineralization occurrence is located in north of Bardaskan, Khorasan Razavi Province, and Taknar zone.The geology of the area consists of Precambrian green sericite schist and metarhyolite, intruded by diabase. Mineralization in this area is in vein form with N50E stribe and 70NW dip and hosted by schist and metarhyolite with 300 meters length and 2 to 35 meters width. Dissem...
Gabbroic complex of Soltan Abad is Located about 35 Km east of Sabzevar. According to tectonic classification, the study area is part of Sabzevar ophiolitic zone. The composition of these intrusion bodies are vary from gabbro to gabbro-diorite. The main minerals of gabbroic rocks are plagioclase (bytonite), clino-pyroxene and ortho-pyroxene (enstatit – hyperestene) and accessory minerals are ap...
Hypogene alteration of ussingite from the southern part of the Ilimaussaq intrusion in South Greenland has resulted in the formation of three associations: gmelinite--apophyllite, gmeliniteherschelite-earthy-natrolite, and earthy natrolite alone. Ossingite reacted with late magmatic fluids, producing the secondary minerals either by in situ replacement of the ussingite or in cavities, which may...
Nowadays, acid mine drainage (AMD) is one of the most important problems in coal mine contamination. The Karmozd coal mines in Mazandaran Province are one of the largest and oldest coal extractions in Central Alborze Coal Basin. The samples of coals, host rocks, mine drainages and secondary surface minerals have been collected in summer season of 2005. On the basis of hydrogeochemistry studies ...
Mashkan deposit is located northern Soltanabad, Sabzevar, Khorasan Razavi province, and tectonically, between Eastern Alborz zone, north Sabzevar ophiolite zone and Binalood zone. Geology of the area includes sedimentary rocks like sandstone, limestone, conglomerate, shale, marl and Eocene volcanic units. Barite mineralization as vein-veinlets with the mainly NW-SE trend has cut off the rock un...
In southwest of the Jandaq City (northeast of Isfahan Province) and northwest of the Central-East Iranian Microcontinent (CEIM), the Eocene dykes with trachy-andesitic composition cross cut the quartz monzodioritic intrusion. The texture of these dykes is granular, intergranular and porphyritic. The studied dykes are composed of plagioclase (andesine and labradorite), clinopyroxene (diopside an...
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