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Bhattacharyya, T. K.
- The Behaviour of Trace Elements in the Magmatic Members of the Singhbhum Granitic Complex
Authors
1 Department of Geology, Presidency College, Calcutta, IN
2 Department of Atomic Energy, Atomic Minerals Division, Petrology Laboratory, New Delhi, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 9, No 2 (1968), Pagination: 178-196Abstract
Seventeen trace elements in 37 total rock samples belonging to six magmatic units of Singhbhum Granite, and nearly as many trace elements in II individual minerals separated from these rocks were estimated by quantitative and semi-quantitative spectrographic analysis respectively. Uranium was determined fluorimetrically in all the 37 samples. The trace element distributions in these samples have been studied in relation to those of the major elements as computed from the modal analyses on the basis of optical and chemical data on the constituent minerals.The trends of variation of the trace elements and of the diadochic element ratios in these rocks conform broadly to those expected under conditions of fractional crystallisation of volatile-rich granitic melts. Distinctive trends of variation of several trace elements and diadochic element ratios with increasing differentiation were found for the three distinct but closely related phases into which these intrusive units may be classified on structural and petrologic grounds. Multivariate analyses and t-tests on 12 trace elements in samples belonging to the three phases indicate that the three phases of granites have significantly different trace element compositions.
- Rare-Earths and Other Trace Elements in Uraninites
Authors
1 Atomic Minerals Division, Department of Atomic Energy, New Delhi, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 11, No 3 (1970), Pagination: 205-216Abstract
Abundances of the lanthanides, yttrium, scandium and 12 other elements in pegmatitic and hydrothermal uraninites from India and Massif Central, France, are presented and compared with those available in literature. The pegmatitic uraninites exhibit a selective, and the hydrothermal types a complete rare-earth assemblage with Gd markedly high in both. The La-Nd: Sm-Ho: Er-Lu ratio may serve as an index of fractionation. Pegmatitic uraninites show an abnormal distribution of La in excess of Ce. An explanation is offered for this.- Petrology and Geochemistry of the Ultramafic Intrusion of Keshargaria, Singhbhum, Bihar
Authors
1 Department of Geology, Presidency College, Calcutta, IN
2 Petrology Laboratory, Department of Atomic Energy, New Delhi, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 13, No 2 (1972), Pagination: 113-121Abstract
An ultramafic body flanked on either side by tholeiitic dolerite occurs as a minor intrusion in the Singhbhum granite, southwest of Keshargaria (22°36' : 85°56'). The ultramafic body varies from pyroxene-rich harzburgite to olivine-rich poikilitic harzburgite, the latter being conspicuous in the central part of the intrusion. A crude planar structure defined by enstatite crystals is developed towards the contact walls. The constituent mafic silicates, arranged in paragenetic order, are: forsteritic olivine, enstatite, diopsidic augite (malacolite), phlogopite and plagioclase, the last three phases appear to represent intracummulus crystallisation.
The central part of the intrusion is relatively enriched in olivine whereas the marginal parts are in an advanced stage of differentiation relative to the central zone, indicated by lower Mg/Fe and Ba/Rb ratios in the former. This spatial variation in degree of differentiation is considered to have been induced during flowage of the crystal-iquid mush. The ultramafic intrusion is non-uniform in chemical and mineralogical compositions and does not represent unaltered mantle material. The significant deviation from the mantle composition is in higher aluminium and ferric iron and lower magnesium in the investigated peridotite. The Keshargaria ultramafic body which is one of several such bodies associated with the Newer Dolerite intrusions, represents a stage of fractionation of mantle derived magma.
- Ore Genetic Significance of Geochemical Trends During Progressive Migmatisation Within Part of the Singhbhum Shear Zone, Bihar
Authors
1 Geology Department, Presidency College, Calcutta, IN
2 Geological Survey of India, Patna, IN
3 Petrology Laboratory, Atomic Minerals Division, New Delhi, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 13, No 1 (1972), Pagination: 39-50Abstract
Study of the trends of geochemical migration of some major and minor elements during progressive migmatisation within part of the Singhbhum shear zone supports the view that apatite-magnetite, uraninite and copper sulphide deposits and the associated wall rock alterations are related to processes of migmatisation therein. During migmatisation extensive mobilisation of elements took place when Si, Al, Na and small quantities of Ga, U and Zr were introduced into the pre-existing basic metavolcanics within the shear zone, and Fe, Mg, Ca, K, Ti, Mn, P, Ba, Rb, Sr, Li, Ni, Co, Cr, V, Cu, and Y were expelled from these rocks. The addition of the former group of elements brought about transformation of these rocks, into felspathic schists and gneisses (the soda-granites) while the expulsion of the latter group of elements from these rocks and their addition to the migmatising fluids caused progressive changes in the chemical composition of these fluids. At the closing stages of the process these fluids were transformed into mineralising solutions that gave rise to apatite-magnetite, uraninite and copper sulphide deposits and to extensive sericitisation, chloritisation, biotitisation and silicification within the shear zone. The various elements, present in traces, entered the crystal lattices of these minerals, in accordance with their geochemical preferences and in proportion to their concentration in the mineralising solutions. The resulting deposits should be regarded as 'metasomatic hydrothermal'.- Geochemistry of the Newer Dolerite Suite of Intrusions within the Singhbhum Granite-A Preliminary Study
Authors
1 Department of Geology, Presidency College, Calcutta, IN
2 Atomic Minerals Division, Department of Atomic Energy, New Delhi, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 14, No 4 (1973), Pagination: 329-346Abstract
Three petrogenetic groups are recognised from petrologic and geochemical data on the Precambrian Newer Dolerite dyke swarm. They are (a) accumulates (peridotites, norites and lamprophyres), (b) products of direct magmatic crystallization (two generations of dole rites and associated micropegmatitic dolerites and micro-granites, each with distinctive trends of major-and minor-element variations), and (c) products of partial melting (leuco-granophyre and xenolithic granophyre), Geochemically, the entire suite has abnormally high K/Rb, Ni, Co and abnormally low Rb, Ba and Sr. Linear discriminant function indicates that the dolerites are typically sub-alkaline. Source magma is inferred to have been picritic and derived by partial melting of the upper mantle.- Geochemistry and Tectonic Significance of Late Archaean-Early Proterozoic Metabasalts from Bacheli, Bastar District, Madhya Pradesh
Authors
1 School of Studies in Geology, Pt. Ravishankar Shukla University, Raipur - 492 010, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 43, No 4 (1994), Pagination: 360-369Abstract
The fine grained, massive metabasalts of Bacheli-Kirandul areas, Bastar district, M.P., characterized by a greenschist facies mineral assemblage have been studied for their major, trace and REE geochemical distribution pattern. On Jensen's AFM Plot and diagrams of relatively immobile elements; these metabasalts fall in the tholeiitic basalts to basaltic andesite field.
Large scatter in Na2O/K2O, K/Rb and RblSr ratios suggest to alteration effects, while high MgO content ascribes to the oxidative diagenesis. Relatively immobile and HFSE element discriminant diagrams point to an island arc/convergent plate setting. The depletion in Nb and Ta relative to Th and LREE in these samples may be relict from a previous tectonic event.
Inferences drawn from geochemical tectonic discriminant diagrams have been evaluated in the light of additional geological data, and an ensialic rift setting for these volcanics is envisaged.
Keywords
Geochemistry, Tectonics, Metabasalts, Bastar District, Madhya Pradesh.- A Reappraisal of the Stratigraphy of Bailadila Group, Bacheli, Bastar District, M.P.
Authors
1 School of Studies in Geology, Pt. Ravishankar Shukla University, Raipur - 492 010, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 42, No 6 (1993), Pagination: 549-562Abstract
The metasedimentary sequence of Bailadila Group exposed in Bacheli area, south Bastar is studied in detail. Based on field relations, structural disposition, conglomerate ocurrence and petrographic characters, Bailadila Group is divided into three Subgroups, which in turn comprise five formations. Formal stratigraphic formationidentified are namely, Bhansi metabasalt-metapelite, Bacheti metasiliclastic, East Ridge Shale, Loa Conglomerate and shale Kailash Nagar Iron Formation. Based on the Stratigraphic continuity, the metabasalt-metapelite association (Bengpal) underlying the feldapathic quartzite (Bacheli metasiliciclastic-Bailadila) is proposed to be included as basal formation of Balladila Group.
Further, high LaN/YbN(10.41-15.89(ratio and Eu/Eu* (0.56-0.64) negative anamolies suggest a sialic continental crust.
It is also proposed that metavolcania-clastic association at chandenar and Tulsi Dongar being similar in lithoassociation to the proposed Bhansi Formation should also be considered of Bailadila Group.