A B C D E F G H I J K L M N O P Q R S T U V W X Y Z All
Mohan, A.
- Colour-coded Compositional Mapping of Orthopyroxene-Plagioclase -: Symplectites in Mafic Granulites from Panrimalai, South India
Authors
1 Departmeont of Geology, Banaras Hindu University, Varanasi-221005, IN
2 Geological Institute Yokohama National university, 79-7 Tokiwadai, Hodogaya-ku, Yokohama 240-8501, JP
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 69, No 2 (2007), Pagination: 285-290Abstract
Orthopyroxene-plagioclase symplecti tes have been observed in garnet-bearing mafic granulites from Panrirnalai, South India. Symplectites are arrested textures from which one can study diffusional processes. We have used colour-coded compositional mapping for reaction textures from mafic granulites to understand the element mobility pattern. The variable.composition of anorthite in plagioclase supports the interpretation that the orthopyroxene-plagioclase symplectites adjoining embayed garnet blast were formed by open-system diffusion - controlled reaction in the NCFMAS model system.Keywords
Mafic granulites, Symplectites, Diffusion, South India.- Internally Consistent Geothermobarometers in the System FeO-MgO-Al2O3-SiO2-H2O Involving Garnet, Cordierite, Aluminosilicate and Quartz and their Application to Metapeiites
Authors
1 Department of Geology, Banaras Hindu University, Varanasi-221 005, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 49, No 6 (1997), Pagination: 647-660Abstract
Reactions involving garnet, cordierite, aluminosilicate and quartz in FMASH system are calibrated as geothermobarometers, namely 1/2 Fe-crd + 1/3 Pyrope = 1/2 Mg-crd + 1/3 Almandine (1); 2 Almandine + 4 sillimanite/andalusite + 5 quartz = 3 Fe-crd (2 and 4); and 2 Pyrope + 4 sillimanite/andalusite + 5 quartz = 3 Mg-crd (3 and 5).
T = [6170+O.031(P-1)-400(XFe-XMg)Crd-A]/(RlnKD+2.812+B) (1)
A= 166 X2Mg-506 X2Fe+680 XFeXMg+336 (XCa+XMa) (XMg-XFe)-
XCa - 358 XMn and B = 1.5 XCa
For Fe and Mg end-member reactions involving sillimanite, the following geobarometric formulation is obtained:
PFe=1+[{(24.02-6RlnKFe)T-17369}/4.003] (2)
PMg=1+[{(7.238-6RlnKMg)T+19640}/3.82] (3)
Similarly for reactions involving and alusite, PFe and PMg expressions are : PFe=1+[{(26.04-6RlnKFe)T-19471}/3.86] (4)
PMg = 1+[{(9.25-6RlnKMg)T+17536}/3.68) (5)