نتایج جستجو برای: fluid inclusions

تعداد نتایج: 233658  

Ajalli, , Tale Fazel, , Torkian, ,

Rasht Abad Cu±Au deposit is a part of the Tarom-Hashtjin metallogenic belt in the western Alborz-Azerbaijan zone. The exposed units in the area include volcanic, sub-volcanic calc-alkaline to shoshonitic rocks with Upper Eocene age and belongs to magmatic arcs setting. The most important alterations related to mineralization include low temperature silicification and sericitic alterations. Mine...

تقی‌پور, صدیقه, تقی‌پور, بتول ,

Kaj-Rostam Abad, Dashtak and Do Ab salt domes are located around Ardal and Farsoun village. This area is situated in High Zagros range (Chaharmahal and Bakhtiary Province). The study area is composed of Lower Cambrian volcano sedimentary complex including basalt, basaltic andesite, andesite, trachyte, pyroclastics, evaporite rocks and Precambrian sedimentary units. According to the mineralogica...

2004
Julien Foriel Pascal Philippot Patrice Rey Andrea Somogyi David Banks Bénédicte Ménez

The concentration of halogens (Cl, Br) and sulfate in seawater during the Archaean eon have important implications for the evolution of Earth’s hydrosphere and atmosphere and the development of early life. Insights into the composition of Archaean seawater and hydrothermal fluids can be obtained by direct analysis of fluid inclusions preserved in Archaean sediments and hydrothermal systems. Her...

Journal: :iranian journal of earth science 0
r. sharma wadia institute of himalayan geology, dehra dun (india) p. joshi geology department, kumaun university, nainital (india) p. verma wadia institute of himalayan geology, dehra dun (india)

a brief account of the representative and workable industrial minerals namely magnesite, talc and barite in lesser himalaya, is presented here emphasizing their genesis. deposits of magnesite and talc are found associated with neoproterozoic, plateform type, shelf-slope limestone-dolomite host rocks from inner lesser himalayan sequences. field, textural, geochemical signatures and fluid inclusi...

Journal: :Physical review. E, Statistical, nonlinear, and soft matter physics 2010
Naomi Oppenheimer Haim Diamant

The hydrodynamic theory of heterogeneous fluid membranes is extended to the case of a membrane adjacent to a solid substrate. We derive the coupling diffusion coefficients of pairs of membrane inclusions in the limit of large separation compared to the inclusion size. Two-dimensional compressive stresses in the membrane make the coupling coefficients decay asymptotically as 1/r(2) with interpar...

2001
William E. Glassley

It has been well established that fluids played an important part in determining chemical characteristics in many crustal terranes. Studies of fluid inclusions in eclogites have established that brines coexisted with the primary mineral assemblages during their metamorphic crystallization. These brines are currently multiply saturated in halide salts, carbonates, oxides, and sulfides. As a firs...

2012
Anne-Florence BITBOL

Lipid bilayers, which form the basis of biological membranes, are self-assembled structures that belong to the field of soft matter. They feature very rich physical properties. While each of the two monolayers of the membrane is a two-dimensional fluid, the membrane resists bending and stretching: it is elastic. Biological membranes are composed of different lipid species and contain various in...

Journal: : 2022

Investigation of mineralization and fluid inclusions the Lapeh-Zanak copper deposit, Central Alborz zone, Iran

2003
B. W. D. Yardley

Microthermometry is a widespread method of determining the chloride concentrations of saline fluid inclusions and remains the most reliable method for converting quantitative cation analyses (e.g. from LA–ICP–MS experiments) into absolute concentrations. For most saline fluids solute concentrations have been calculated as an equivalent weight percentage of NaC on the basis of phase transition t...

Calagari, AliAsghar, Miranvari, Azam Sadat, Siahcheshm, Kamal, Sohrabi, Ghahraman,

The Noghduz  prospecting area, as a part of the Arasbaran metallogenic zone is located about 20 km east of Ahar, East-Azarbaijan Province. The mineralization host rocks are andesite-trachy andesite with the age of  Late  Eocene. The hydrothermal alterations exposed in this area are silicic, argillic, and propylitic. Pyrite is the main hypogene sulfide mineral which is accompanied by lesser amou...

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