نتایج جستجو برای: phlogopite
تعداد نتایج: 311 فیلتر نتایج به سال:
the release rate of potassium (k) from micaceous minerals plays a significant role in supplying k to plants. the objective of this study was to determine the most appropriate kinetic equation to describe potassium release from micaceous minerals as influenced by organic acids. muscovite and phlogopite were made to react with 0, 500, 2000 and 4000 ?m solutions of oxalic, citric and malic acids f...
The Anarak ophiolite, with E-W trending, located at north of Anarak. In addition to the gabbros in Anarak ophiolite sequence, intrusion of metasomatized gabbros injected into the ophiolite of Anarak in the form of stocks and dykes. metasomatized gabbros are younger than Anarak ophiolite and older than Anarak metamorphic assemblage and contain diopside, augite, actinolitic hornblende, actinolite...
The Ma’danjoo prospect area is one of the eastern anomalies of Khaf’s Sangan iron mine in southeast of Mashhad. Geological units in the area include Jurassic sedimentary rocks, skarn, and Tertiary subvolcanic intrusion with monzonitic composition. Skarns have been seprated in to 7 zones on the basis of abundance and type of the calc-silicate including: garnet, pyroxene-garnet, pyroxene, phlogo...
Experimental approaches attempt to determine the routes by which crustal carbonatite magmas can be derived from C02-bearing peridotite at high pressures. The intimate association of kimberlite and carbonatite on a small scale il· lustrates links in the processes. Carbonation of peridotite by C02 can cause the generation of near-solidus carbonatitic liquid from mantle peridotite at depths greate...
Aillikites are kimberlite-like rocks, important for understanding the composition and processes occurring in mantle. Melt inclusions represent a reliable source of information. The paper provides first results studies (Raman, EDS) on primary secondary melt olivine from Ilbokich uplift aillikites. is close to that parent It was significantly enriched CO 2 , H O, phosphorus titanium. Phlogopite, ...
چکیده منطقه مورد مطالعه بخشی از زون سنندج-سیرجان می باشد که در شمال و شمال غربی شهرستان نهاوند قرار دارد. سنگ های دگرگونی منطقه به دو گروه اصلی فلدسپات - کوارتز شیست و مرمر تقسیم می شوند. سه دسته دگرشکلی pre d1، d1 و d2، فابریک های منطقه را بوجود آورده اند. دگرشکلیpre d1 ، با دگرگونی m1 مطابقت دارد و دگرشکلی d1 دگرشکلی اصلی در منطقه است و با دگرگونی m2 هم خوانی دارد. دگرشکلی d3 به صورت ریزچین ...
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