The peninsular malaysian granites are distributed into three parallel belts i e.
A type granites geochemical characteristics.
Geochemical and petrological data indicates that it is a type granite which formed in within plate granite tectonic set up.
New analyses of 131 samples of a type alkaline or anorogenic granites substantiate previously recognized chemical features namely high sio 2 na 2 o k 2 o fe mg ga al zr nb ga y and ce and low cao and sr.
Good discrimination can be obtained between a type granites and most orogenic granites m i and s types on plots employing ga al various major element ratios and y ce nb and zr.
On the basis of the major trace element characteristics the initial nd isotope compositions and relict zircon u pb ages of the triassic granites and their spatial overlap with the.
Example from peninsular malaysia granites azman a ghani department of geology university of malaya 50603 kuala lumpur abstract.
S type granites are a category of granites first proposed by chappell white.
Geochemical characteristics of s and i type granites.
Geochemical characteristics discrimination and petrogenesis.
There are lower levels of calcium and strontium.
Hf and nd isotopes.
The sarudik a type granites are further assigned.
Petrographic characteristics of the barabazar granite under cross nicol a granite with interlocking crystals and perthite t exture.
They are recognized by a specific set of mineralogical geochemical textural and isotopic characteristics.
S type granites are over saturated in aluminium with an asi index greater than 1 1 where asi al 2 o 3 cao na 2 o k 2 o in mol percent.
By using ga al ratio fractionated felsic i or s type granites can overlap in apparent.
Geochemical and isotopic data suggest that the source of these a type granites is the mesoproterozoic continental crust without significant incorporation of mantle derived component and their formation is controlled by subsequent fractional crystallization.
Chemical characteristics of a type granites include high silica alkalis zirconium niobium gallium yttrium and cerium.
A type granites are mostly peraluminous and many of them have metasedimentary sources that previously underwent significant extraction of hydrous felsic melts.
Petrographic features are representative of the chemical.
The barabazar granite was emplaced at.
Good discrimination can be obtained between a type granites and most orogenic granites m i and s types on plots employing ga al various major element ratios and y ce nb and zr.
Western central and eastern belts.
Y yb ta and nb similar to the typical continent continent syn collisional granite.
Pdf on jan 1 1987 j b.
Whalen and others published a type granites.