نتایج جستجو برای: pyroclastic units
تعداد نتایج: 172732 فیلتر نتایج به سال:
Abstract Tandem in situ and isotope dilution U-Pb analysis of zircons from pyroclastic volcanic rocks both glacial non-glacial sedimentary strata the Pocatello Formation (Idaho, northwestern USA) provides new age constraints on Cryogenian glaciation North American Cordillera. Two dacitic tuffs sampled within glacigenic lower diamictite interval Scout Mountain Member yield high-precision chemica...
The Tolhuaca hydrothermal system is one of the few attested geothermal resources in Chile. While recent investigations provided some insights into depth and temperature reservoirs chemical mineralogical evolution system, little still known about CO2 degassing local shallow control fluid pathways. Here, we document soil distributions southern part at its northern fumaroles, provide a first estim...
Study area is located in Kerman Province and NE Baft city near to Rabor town. This section is in the structural division of Iran classified as Urumieh-Dokhtar magmatic belt which in Kerman area is called- Dahaj-Sarduieh belt that extended parallel to Urumieh-Dokhtar magmatic belt. These rocks comprise of andesite, andesite-basalt, dacite and rarely basalt and trachy-andesite with Eocene age tha...
Zavarian epitermal gold (copper) deposit is located in an intracontinental volcanic cone (stratovolcano) with the Early Miocene age, in the middle of the Urmia-Dokhtar magmatic arc. The host rocks of this mineralization include a set of basaltic, andesitic-basaltic, andesitic, dacitic, as well as granodiorite and tonal units that have been exposed in volcanic form (lava and pyroclastic) and sem...
This work describes the structural and lithological controls that affect distribution, orientation, precipitation mechanism of mineralization in Martinetas district, from context analysis role played by geological units host mineralization. is a low sulfidation epithermal gold silver mining district located northeastern sector Deseado Massif, Argentina. The characterized numerous quartz veins, ...
The Rahmatabad Kaolin deposit is located about 25 km southwest of Nain. This deposit is formed by alteration process from Eocene volcanic rocks and pyroclastic units. Mineralogical studies display that the kaolinite, jarosite, hematite, quartz, calcite, anortite, alunite, diaspore, chlorite, montmorillonite, illite, albite, orthoclase, halite, sanidine, goethite, malachite, azurite and sericite...
Abstract. Gravitational instabilities can be significant threats to populations and infrastructure. For hazard assessment, it is important estimate the geometry volume of potential unstable masses. This characterization particularly difficult in volcanic contexts due succession deposition erosion phases. Indeed, results complex layering geometries which interfaces between geological layers may ...
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