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Malapur, M. A.
- Petrography and Geochemistry of the Neoarchaean Greywackes from Central Part of the Dharwar-Shimoga Greenstone Belt, Western Dharwar Craton
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Authors
Affiliations
1 Department of Studies in Geology, Karnatak University, Dharwad-580003, IN
2 Department of Geology, Central University of Kerala, Kasaragod-671123, IN
1 Department of Studies in Geology, Karnatak University, Dharwad-580003, IN
2 Department of Geology, Central University of Kerala, Kasaragod-671123, IN
Source
International Journal of Earth Sciences and Engineering, Vol 10, No 4 (2017), Pagination: 898-902Abstract
Greywackes are the most dominant of litho units in the central part of the Dharwar-Shimoga greenstone belt of the Western Dharwar Craton. They are texturally immature with angular to subangular detrital sand grains with 25 to 60% matrix. Quartz forms the main detrital component and is mostly monocrystalline with distinct undulatory extinction. Amongst feldspars, plagioclase feldspar exceeds K-feldspar. Micas occur as large and small flakes that are oriented. Biotite is the main mica mineral. The phyllite, chert, quartzite and felsic volcanic rock fragments are common. The matrix is generally made up of chlorite, sericite, clay to silt-sized quartz and feldspar. In Q-F-L classification diagram, these rocks plot in the fields of quartz wackes and quartzose wackes. The silica content varies between 60.93 and 68.07 wt% and alkalies between 3.69 and 5.21 (Table 2), and compositionally they are comparable to andesite and dacite. Moderately higher values of Fe2O3 (av. 8.16 wt%), MgO (av. 7.89 wt%) and K2O/Na2O (av. 1.65) indicate a matrix with an abundance of chlorite, biotite, clays and iron oxides. The petrographic and geochemical evidence suggests that these greywackes were derived from the source which had felsic to intermediate composition, with a moderate relief exposed to arid and dry palaeoclimatic conditions. As compared to greywackes of the northern part of the Dharwar-Shimoga greenstone belt, the greywackes of the present study area (central part) have higher values of MgO, Fe2O3+MgO, K2O/Na2O, Al2O3/Na2O and lower values of Al2O3, Na2O, and SiO2/MgO.Keywords
Greywacke, Petrography, Geochemistry, Provenance, Dharwar-Shimoga Greenstone Belt.Full Text
References
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- Basalt-Andesite-Dacite-Rhyolite (BADR) Metavolcanic Sequence from the Central Part of Dharwar-Shimoga Greenstone Belt, Western Dharwar Craton
Abstract Views :157 |
PDF Views:119
Authors
Affiliations
1 Department of Studies in Geology, Karnatak University, Dharwad-580003, IN
2 Department of Geology, Central University of Kerala, Kasaragod-671123, IN
1 Department of Studies in Geology, Karnatak University, Dharwad-580003, IN
2 Department of Geology, Central University of Kerala, Kasaragod-671123, IN
Source
International Journal of Earth Sciences and Engineering, Vol 10, No 1 (2017), Pagination: 106-110Abstract
The petrographic and major element geochemical characteristics clearly suggest that the metavolcanic rocks of Medur Formation in the central part of the Dharwar-Shimoga greenstone belt comprise basalt, andesite, dacite and rhyolite (BADR) sequence. These metavolcanic rocks are metamorphosed to greenschist-amphibolite facies. The basalts show mixed tholeiitic and komatiitic composition. The andesites are mainly tholeiitic, while dacite and rhyolites are calc alkaline nature. Good correlation exists between SiO2 and major oxides, which suggests that these metavolcanic series (BADR) compositions are genetically inter-related and were derived probably from differentiation of magma at different depths.Keywords
Metavolcanics, Petrography, Geochemistry, Dharwar-Shimoga Greenstone Belt, Dharwar Craton.Full Text