نتایج جستجو برای: dacitic

تعداد نتایج: 177  

Ahmad Khakzad Hamid Harati Marzieh Hosseini Nematollah Rashidnejad Omran Peyman Afzal Simin Harati

Kahang Cu Porphyry deposit is situated in the central part of a major Iranian magmatic belt, Urumieh-Dokhtar, in central Iran.There are several sub-volcanic stocks (e.g., porphyric granitoids rocks, quartz monzonite, diorite and monzodiorite-monzogranite)within Eocene volcanic and pyroclastic rocks consisting of basaltic, trachy-andesite and dacitic rocks. Hydrothermal alterations at the Kahang...

Etemadi, Abbas, Malekzadeh Shafaroudi, Azadeh,

The Cheshmeh Zagh area is located on Khorasan Razavi Province, the southern parts of the Sabzevar zone, which is one of the most important metallogeny zones of Iran. Lithologically, the area includes a variety of Late Cretaceous volcanic rocks (dacite to basalt), intrusions (gabbro to synogranite), Oligo-Miocene sedimentary rocks, and Quaternary sediments. Alteration zones of propylitic, chlori...

Journal: :Frontiers in Earth Science 2021

We present a novel approach to use zircon as correlation tool well monitor for magma reservoir processes in silicic volcanic systems. Fingerprinting eruption products based on trace element content and U-Pb dates of offers promising, previously underestimated tephra perspective, particularly cases where the main minerals glass are altered. Using LA-ICP-MS analyses, rapid cost-effective method, ...

Journal: :The Journal of dairy research 2005
Alejo Pérez-Carrera Alicia Fernández-Cirelli

The Chaco Pampean Plain of central Argentina constitutes one of the largest regions of high arsenic (As) groundwaters known, covering around 1 x 10(6) km2 (Smedley & Kinniburg, 2002; Farías et al. 2004). The high-As groundwaters are from Quaternary deposits of loess (mainly silt) with intermixed rhyolitic or dacitic volcanic ash (Nicolli et al. 1989, Smedley et al. 1998,2002). Early in the last...

1997
D. S. Stevenson

The rates of passive degassing from volcanoes are investigated by modelling the convective overturn of dense degassed and less dense gas-rich magmas in a vertical conduit linking a shallow degassing zone with a deep magma chamber. Laboratory experiments are used to constrain our theoretical model of the overturn rate and to elaborate on the model of this process presented by Kazahaya et al. (19...

Journal: :Geologica Carpathica 2021

Major and trace element composition of silicate melt inclusions (SMI) their rock-forming minerals were studied in mafic garnet granulite xenoliths from the Bakony–Balaton Highland Volcanic Field (Western-Hungary). Primary SMIs occur clinopyroxene plagioclase plagioclase-rich domains granulites ilmenite vicinity these wall rock. Based on major elements, we demonstrated that have no connection wi...

Journal: :European Journal of Mineralogy 2021

Abstract. Clinopyroxene-only thermobarometry is one of the most practical tools to reconstruct crystallization pressures and temperatures clinopyroxenes. Because it does not require any information coexisting silicate melt or other co-crystallized mineral phases, has been widely used elucidate physiochemical conditions crystallizing magmas. However, previously calibrated clinopyroxene-only ther...

Journal: :Earth Sciences Research Journal 2022

The Cauca metallogenic belt is an inter-Andean area located along the Cauca-Romeral fault zone, which made up of a group twelve Miocene magmatic-hydrothermal Au-Ag-Cu mineral deposits positioned between Western and Central Cordillera Colombia. In addition to being widely developed region in exploration exploitation with known Au endowments over 1,700 tons, this represents exceptional metallogen...

ملک‌زاده شفارودی, آزاده, کریم‌پور, محمد‌حسن, زارعی, آرزو ,

Khanlogh magnetite-apatite deposit is located in northwest of Neyshabour. This area is situated in Binaloud structural zone and east of Tertiary Quchan-Sabzevar magmatic arc. Geology of the area is dacitic volcanic rock intruded by Oligocene subvolcanic rocks with composition of quartz monzodiorite and granodiorite. Miocene sedimentary rocks trusted on them. The magmatism in the area shows char...

جهانگیری, احمد, موید, محسن,

In the west of Marand in Ghekhlar area, the Upper MiocenePleistocene volcanic rocks, including intermediate to acidic basic alkaline and lampr~phyric, are extensive exposed. Trachy-andesite rocks of this area contain carbonatite-silicate xenoliths, which according to mineralogical studies, are calcite - carbonatite type. The minerals of calcite, diopside, anorthite, phlogopite, amphibole, ...

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