Our Group organises 3000+ Global Conferenceseries Events every year across USA, Europe & Asia with support from 1000 more scientific Societies and Publishes 700+ Open Access Journals which contains over 50000 eminent personalities, reputed scientists as editorial board members.
T
ourmaline is one of the accessory and mafic minerals which occurs in peraluminous granitic pegmatites from the North
of Golpayegan (Ochestan area). The mineral assemblage of these pegmatites consists of turbidity K-feldspar (perthitic
orthoclase and microcline), plagioclase (albite), quartz, muscovite (primary and secondary), zoned tourmaline (dravite) and
biotite (Mg-biotite) in order of decreasing abundances. The leucocratic matrix is dominated by large K-feldspar with broad
perthitic exsolution lamellae. Twinned crystals of plagioclase have undergone sericitisation. Anhedral quartz shows intensive
oscillatory extinction and subgrain formation. Muscovites present as large and fine grains which sometimes curved and growth
next to tourmaline and in or between feldspars. Tourmaline is usually euhedral and shows optical zonation (yellowish green color
shifted to yellow at the rim). Small biotite is trapped between quartz and feldspar. Zoned tourmalines in pegmatite are mainly
restricted to the sodium replacement and yellow tourmaline are driven from biotite which attacked by boron introduce. Evidences
of alkali metasomatism such as coarsening domains in perthite, growth of new micas (sodic metasomatism), replacement of
albitic plagioclase by microcline, distinct reddish coloration microclines in hand specimens and turbidity of the feldspar crystals
in thin-section (Potassic metasomatism) are seen in these pegmatites. Based on the occurrence of H
+
metasomatism which follow
albitisation process and Quartz +Muscovite + (Na
+
, K
+
)=Perthite + H
+
reaction, there is the possibilithy of tourmalinization
through K(Fe,Mg)
3
AlSi
3
O
10
(OH)
2
+1.67KAl
2
AlSi
3
O
10
(OH)
2
+NaCl(
aq
)+1.67HCl(
aq
)+3B(OH)3(
aq
)=Na(Fe,Mg)
3
Al
6
B
3
O
9
Si
6
O
18
(OH)
4
+ 2SiO
2
+2.67 KCl(
aq
)+ 6H
2
O reaction which occurs in the presence of neutral to acidic solutions to form dravite in the
studied pegmatites.
Biography
Akramosadat Mirlohi did her Ph.D. in Petrology at the age of 31 years in University of Isfahan, Isfahan, Iran. She has published 5 papers in journals
(1 ISI and 4 Iranian Scientific Journals).
Relevant Topics
Peer Reviewed Journals
Make the best use of Scientific Research and information from our 700 + peer reviewed, Open Access Journals