Готові списки джерел за темами / Dharwar Craton

Добірка наукової літератури з теми "Dharwar Craton"

Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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Статті в журналах з теми "Dharwar Craton"

Sunder Raju, P. V., P. G. Eriksson, O. Catuneanu, S. Sarkar, and S. Banerjee. "A review of the inferred geodynamic evolution of the Dharwar craton over the ca. 3.5–2.5 Ga period, and possible implications for global tectonics." Canadian Journal of Earth Sciences 51, no. 3 (March 2014): 312–25. http://dx.doi.org/10.1139/cjes-2013-0145.

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The geological history and evolution of the Dharwar craton from ca. 3.5–2.5 Ga is reviewed and briefly compared with a second craton, Kaapvaal, to allow some speculation on the nature of global tectonic regimes in this period. The Dharwar craton is divided into western (WDC) and eastern (EDC) parts (separated possibly by the Closepet Granite Batholith), based on lithological differences and inferred metamorphic and magmatic genetic events. A tentative evolution of the WDC encompasses an early, ca. 3.5 Ga protocrust possibly forming the basement to the ca. 3.35–3.2 Ga Sargur Group greenstone belts. The latter are interpreted as having formed through accretion of plume-related ocean plateaux. The approximately coeval Peninsular Gneiss Complex (PGC) was possibly sourced from beneath plateau remnants, and resulted in high-grade metamorphism of Sargur Group belts at ca. 3.13–2.96 Ga. At about 2.9–2.6 Ga, the Dharwar Supergroup formed, comprising lower Bababudan (largely braided fluvial and subaerial volcanic deposits) and upper Chitradurga (marine mixed clastic and chemical sedimentary rocks and subaqueous volcanics) groups. This supergroup is preserved in younger greenstone belts with two distinct magmatic events, at 2.7–2.6 and 2.58–2.54 Ga, the latter approximately coincident with ca. 2.6–2.5 Ga granitic magmatism which essentially completed cratonization in the WDC. The EDC comprises 2.7–2.55 Ga tonalite–trondhjemite–granodiorite (TTG) gneisses and migmatites, approximately coeval greenstone belts (dominated by volcanic lithologies), with minor inferred remnants of ca. 3.38–3.0 Ga crust, and voluminous 2.56–2.5 Ga granitoid intrusions (including the Closepet Batholith). An east-to-west accretion of EDC island arcs (or of an assembled arc – granitic terrane) onto the WDC is debated, with a postulate that the Closepet Granite accreted earlier onto the WDC as part of a “central Dharwar” terrane. A final voluminous granitic cratonization event is envisaged to have affected the entire, assembled Dharwar craton at ca. 2.5 Ga. When Dharwar evolution is compared with that of Kaapvaal, while possibly global magmatic events and freeboard–eustatic changes at ca. 2.7–2.5 Ga may be identified on both, the much earlier cratonization (by ca. 3.1 Ga) of Kaapvaal contrasts strongly with the ca. 2.5 Ga stabilization of Dharwar. From comparing only two cratons, it appears that genetic and chronologic relationships between mantle thermal and plate tectonic processes were complex on the Archaean Earth. The sizes of the Kaapvaal and Dharwar cratons might have been too limited yet to support effective thermal blanketing and thus accommodate Wilson Cycle onset. However, tectonically driven accretion and amalgamation appear to have predominated on both evolving cratons.

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Mukhopadhyay, Dhruba. "Structural Pattern in the Dharwar Craton." Journal of Geology 94, no. 2 (March 1986): 167–86. http://dx.doi.org/10.1086/629021.

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OKUDAIRA, T., T. HAMAMOTO, B. HARI PRASAD, and RAJNEESH KUMAR. "Sm–Nd and Rb–Sr dating of amphibolite from the Nellore–Khammam schist belt, SE India: constraints on the collision of the Eastern Ghats terrane and Dharwar–Bastar craton." Geological Magazine 138, no. 4 (July 2001): 495–98. http://dx.doi.org/10.1017/s001675680100543x.

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The Nellore–Khammam schist belt, SE India, is sandwiched in between the Proterozoic Eastern Ghats terrane and the Archaean Dharwar–Bastar craton. We report Sm–Nd and Rb–Sr mineral isochron ages of amphibolite from the schist belt. The Sm–Nd and Rb–Sr ages are 824±43 Ma and 481±16 Ma, respectively. The Sm–Nd age indicates the timing of peak metamorphism, whereas the Rb–Sr age indicates the Pan-African thermal overprint. The peak metamorphism was related to collision of the Eastern Ghats terrane with the Dharwar-Bastar craton, which occurred during early Neoproterozoic time.

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Rama Rao, J. V., B. Ravi Kumar, Manish Kumar, R. B. Singh, and B. Veeraiah. "Gravity of Dharwar Craton, Southern Indian Shield." Journal of the Geological Society of India 96, no. 3 (September 2020): 239–49. http://dx.doi.org/10.1007/s12594-020-1543-8.

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Roy, Sunil Kumar, D. Srinagesh, Dipankar Saikia, Arun Singh, and M. Ravi Kumar. "Seismic anisotropy beneath the Eastern Dharwar craton." Lithosphere 4, no. 4 (August 2012): 259–68. http://dx.doi.org/10.1130/l198.1.

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Mamtani, Manish A., Sandeep Bhatt, Virendra Rana, Koushik Sen, and Tridib K. Mondal. "Application of anisotropy of magnetic susceptibility (AMS) in understanding regional deformation, fabric development and granite emplacement: examples from Indian cratons." Geological Society, London, Special Publications 489, no. 1 (January 9, 2019): 275–92. http://dx.doi.org/10.1144/sp489-2019-292.

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AbstractIn this paper the authors review various applications of analysing fabric in granites from Indian cratons using anisotropy of magnetic susceptibility (AMS). First the general importance of AMS in identifying the internal fabric in massive granitoids devoid of visible foliations/lineations is highlighted. Subsequently, three important applications of AMS in granitoids are discussed. (a) The case of Godhra Granite (southern parts of the Aravalli Mountain Belt) is presented as an example of the robustness of AMS in working out the time relationship between emplacement/fabric development and regional deformation by integrating field, microstructural and magnetic data. (b) AMS orientation data from Chakradharpur Granitoid (eastern India) are compared with field-based information from the vicinity of the Singhbhum Shear Zone to highlight the use of AMS in kinematic analysis and vorticity quantification of syntectonic granitoids. (c) Magnetic fabric orientations from the Mulgund Granite (Dharwar Craton) are presented to document the application of AMS in recognizing superposed deformation in granitoids. Moreover, AMS data from Mulgund Granite are also compared with data from another pluton of similar age (c. 2.5 Ga) from the Dharwar Craton (Koppal Granitoid; syenitic composition). This highlights the use of AMS from granitoids of similar absolute ages in constraining the age of regional superposed deformation.

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MANUVACHARI, T. B., A. G. UGARKAR, B. CHANDAN KUMAR, and M. A. MALAPUR. "Basalt-Andesite-Dacite-Rhyolite (BADR) Metavolcanic Sequence from the Central Part of Dharwar-Shimoga Greenstone Belt, Western Dharwar Craton." International Journal of Earth Sciences and Engineering 10, no. 01 (March 6, 2017): 106–10. http://dx.doi.org/10.21276/ijee.2017.10.0116.

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Kumar, Anil, Y. J. Bhaskar Rao, V. M. Padma Kumari, A. M. Dayal, and K. Gopalan. "Late Cretaceous mafic dykes in the Dharwar craton." Journal of Earth System Science 97, no. 1 (July 1988): 107–14. http://dx.doi.org/10.1007/bf02861631.

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Venkatachala, B. S., Manoj Shukla, Mukund Sharma, S. M. Naqvi, R. Srinivasan, and B. Udairaj. "Palaeobiologic activity in the archaean Dharwar craton, India." Origins of Life and Evolution of the Biosphere 19, no. 3-5 (May 1989): 448–49. http://dx.doi.org/10.1007/bf02388944.

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Chinnaiah, Chinnaiah. "Characterisation of Manganese Ores of Shimoga Schist Belt, Dharwar Craton, Southern India." Global Journal For Research Analysis 3, no. 3 (June 15, 2012): 184–89. http://dx.doi.org/10.15373/22778160/mar2014/70.

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Дисертації з теми "Dharwar Craton"

Osborne, Ian. "Age and origin of proterozoic kimberlites and lamproites from the Dharwar Craton, southern India." Thesis, Open University, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.551615.

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This is a study of kimberlite and lamproite intrusions located in southern India within the Eastern Dharwar craton (EDC). Bulk-rock major-element, trace-element, REE- and Nd- isotopic data support previous studies that have classified the ultramafic magrnatism located in the EDC as either Group I kimberlite or lamproite. This study reports new high-precision Ar-Ar age data for southern Indian ultrapotassic 'rocks (kimberlites and lamproites). Previously, the Chelima lamproite (ca. 1400 Ma) was considered to be one of the oldest lamproites in the world. However, our age data suggest that at least one lamproite (Pochampalle from Krishna lamproite field) was generated in the same region 100 Ma before the Chelima event. The Pochampalle lamproite was emplaced around ~ 1500 Ma as shown by the Ar-Ar data in this study, roughly 250 Ma before the other Krishna lamproites. It would seem that the Pochampalle lamproite was also derived from an isotopically distinct source region with a lower 143Ndl144Nd ratio than other Krishna lamproites. These findings not only have implications for regional ultramafic/ultrapotassic magrnatism, but also demonstrate that the mantle processes for producing lamproitic melts existed earlier than previously thought. This study also presents the first Hf isotopic analyses of perovskites from Indian kimberlites. Perovskites fall into two distinct groups in Hf isotope space, suggesting a degree of heterogeneity in the source of the kimberlites in the EDC. The kimberlites are all found in such close proximity that lateral variations in the source are unlikely, but this does not preclude vertical heterogeneity in the source region(s). I propose a model of kimberlite generation with a vertically heterogeneous source that has undergone separate periods of enrichment and depletion before kimberlite melt generation and emplacement at ~ 11 00 Ma.

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Chalapathi, Rao Nittala Venkata. "Petrogenesis of Proterozoic kimberlites and lamproites from the Cuddapah Basin and Dharwar craton, southern India." Thesis, University of Cambridge, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.627224.

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Bouhallier, Hugues. "Evolution structurale et métamorphique de la croûte continentale archéenne (craton de Dharwar, Inde du sud)." Rennes 1, 1994. https://tel.archives-ouvertes.fr/tel-00619323.

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Bouhallier, Hugues. "Evolution structurale et métamorphique de la croûte continentale archéenne : craton de Dharwar, Inde du Sud /." Rennes : Géosciences, Université de Rennes I, 1995. http://catalogue.bnf.fr/ark:/12148/cb35771450m.

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Moyen, Jean-François. "Le magmatisme granitique a la transition archeen-proterozoique : l'exemple du craton de dharwar, inde du sud (granite de closepet et intrusions associees)." Clermont-Ferrand 2, 2000. http://www.theses.fr/2000CLF22189.

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La fin de l'archeen est generalement marquee par une periode d'intense activite magmatique (mise en place de granitoides). Ces granites different a la fois des ttg archeennes, et des granites calco-alcalins modernes. Le craton de dharwar, en inde du sud, presente a l'affleurement de nombreux massifs granitiques tardi-archeens. De plus, il offre une coupe naturelle de la croute continentale, depuis des niveaux profonds (facies granulite), jusqu'a des niveaux superficiels (facies schiste vert). L'un de ces granites, le massif de closepet, affleure a tout les niveaux structuraux. Une etude multi-methodologique (terrain, spot, asm) du champ de deformation dans et aux alentours de ce massif a permis de proposer un modele de mise en place de ces magmas au sein de zones de cisaillement actives. La modelisation geochimique a permis de demontrer que ce granite est le produit du melange de deux magmas, l'un issu de la fusion partielle d'un manteau metasomatise par des magmas issus de la fusion d'une plaque subductee ; l'autre issu de la fusion partielle du socle gneissique, rechauffe par l'arrivee des magmas mantelliques. Dans le craton, on trouve plusieurs types de granites tardi-archeens. Des magmas de type ttg (fusion d'une plaque basaltique subductee) cohabitent avec des magmas de type sanukitoide (interaction de magmas ttg avec les peridotites du manteau), des granites anatectiques, et de granites du type closepet. Les memes types de granites existent dans tout les cratons archeens. Ceci amene a proposer un modele d'evolution geodynamique pour l'archeen : chaque craton aurait connu une succession de cycles d'activites commencant par un collage d'arc insulaires (ttg et sanukitoides, et chevauchements), puis un remaniement ht-bp du continent neoforme, avec refusion du manteau enrichi (granites type closepet et structures en domes et bassins). Le refroidissement progressif de la terre au cours de l'archeen a rendu les interactions entre les magmas ttg et le manteau de plus en plus importantes, ce qui se traduit par une abondance croissante des sanukitoides et des granites type closepet. Finalement, au proterozoique, la terre est devenue assez froide pour empecher la fusion de la plaque plongeante, causant donc une transition vers des mecanismes petrogenetiques radicalement differents.

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Katuru, Venkata Pavan. "Tectonic and Isotopic evolution of the Dharwar Craton, India." Thesis, 2021. https://hdl.handle.net/2440/133494.

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The crustal evolution of a craton could be studied from analysing its zircon U-Pb record and associated isotopic and elemental composition. The Dharwar Craton in southern India is one such craton on which several independent studies have been conducted on isolated domains within the craton. In this thesis, we have attempted to create a robust tectonic and isotopic evolution model of the Dharwar Craton which also includes previously published data. This thesis is divided into four chapters spanning from the Archean origins of the craton to the latest thermal events affecting various domains within the craton. Chapter 1 deals with zircon U-Pb dating, rare earth element (REE) composition and Lu-Hf isotopic analysis from granitoids sampled across the various domains within the Dharwar Craton to evaluate the crustal evolution episodes from individual domains and compare them to build a robust crustal architecture model for the Dharwar Craton including previously published data. Chapter 2 deals with the detrital record of the Dharwar Craton deposited within the various volcano-sedimentary greenstone belts that unconformably overly the basement granitoid gneisses and igneous batholiths through detrital zircon U-Pb dating, REE compositions. The detrital sequences sampled from the Western Dharwar Craton have been analysed for detrital zircon Lu-Hf isotopes to further constrain the crustal evolution processes within the Western Dharwar Craton. Chapter 3 deals with the detrital record of the Kaladgi-Badami basin, an east-west trending intracratonic Paleoproterozoic basin that unconformably overlies the northern part of Dharwar Craton, which formed as part of the widespread Proterozoic sedimentation across India termed as Purana basins. The detrital zircon U-Pb dating, REE compositional data from various stratigraphic units has been used to infer potential source regions and to compare with sedimentary records across other Paleoproterozoic basins across India and Madagascar to understand the post-assembly tectonic process within the Dharwar Craton which led to the formation of the Kaladgi-Badami basin. Chapter 4 deals with the thermal record of the Western Dharwar Craton by magmatic and meta-igneous zircon, apatite and monazite: U-Pb dating, REE composition sampled along the western margin along the Dharwar Craton including the adjacent Coorg block and Karwar block. The difference between ages obtained using high-temperature zircon (>800° C) U-Pb dating and medium temperature (450—550° C) apatite U-Pb dating was used to infer the timing and spatial extent of the last thermal event experienced across the Dharwar Craton and correlate with contemporaneous tectonic events.
Thesis (Ph.D.) -- University of Adelaide, School of Physical Sciences, 2021

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Marokane, Manoko Maggie. "Petrology and (U-Th)/He Thermochronology of Mesoproterozoic Kimberlites from the eastern Dharwar Craton, southern India." Thesis, 2017. https://hdl.handle.net/10539/25041.

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A dissertation submitted in fulfilment of the requirements for the degree of Master of Science, in the Department of Geosciences, University of the Witwatersrand, Johannesburg, South Africa, 2017.
Apatite (U-Th)/He thermochronometry data from two different kimberlite clusters of the Dharwar Craton is used, together with geologic constraints, to develop a model for the burial, uplift, and unroofing history of southern India (i.e. Peninsular India). The apatite helium (AHe) dates for the CC-5 kimberlite at a present-day elevation of 398 m range between 128-235 Ma, with a mean age of 164.9 ± 21.2 Ma (1 S.D.). The AHe dates for the SK-2 kimberlites at a present-day elevation of 289 m range from 121.1-170.7 Ma, with a mean age of 166.3 ± 25.2 Ma (1 sigma standard deviation). The mean AHe ages for the CC-5 and SK-2 kimberlites from the approximately 150 km apart Wajrakarur and Raichur kimberlite fields, respectively, are indistinguishable within their uncertainties. This suggests a similar uplift and erosion history of the two areas on the eastern Dharwar craton. All these dates are younger than kimberlite pipe emplacement (ca. 1100 Ma) signalling a major post-emplacement erosion during the Mesozoic (Middle Jurassic). We use the data to link not only uplift and erosion to elevation gain, but to show how this corresponds to deep mantle processes and continental formation or breakup. Our HeFTy time-temperature modelling results indicate heating to temperatures of ~175 °C suggesting burial, which was followed by an unroofing (cooling) event. Plate tectonic modelling using GPlates software package is also consistent with t-T models, in that the signals observed are also recorded by plate movements (e.g. the 175 Ma). Burial is restricted to a depth of 3 km after pipe emplacement. Erosion estimates show that the Dharwar Craton underwent ≥ 1.5-4 km of erosion during the Jurassic, most likely related to Gondwana break-up that commenced at ~180 Ma. The fast drift of the Indian plate (18 cm/a) towards the northern hemisphere during the Cretaceous is related to the removal of the once thick cratonic keel beneath the Indian Craton. Whether parts of the mantle lithosphere were delaminated/removed during or post Gondwana is controversially debated. Herein, we propose a model for cratonic root delamination, related to deep mantle processes (i.e., dynamic topography) that may have played a role or aided in lithospheric thinning of the Indian tectonic plate.
LG2018

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Gore, R. J. "Geochronological and sedimentological constraints of the Srisailam Formation, S.E. India." Thesis, 2011. http://hdl.handle.net/2440/96125.

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This item is only available electronically.
The Proterozoic Cuddapah Basin contains the poorly constrained Srisailam Formation, which presumably lies unconformably over the Nallamalai Group. The Cuddapah Basin is thought to have initiated as a rift basin > 1900 Ma before developing into a foreland basin due to uplift of the Eastern Ghats Belt (EGB) at ~1600 Ma. U-Pb geochronology indicates deposition of the Srisailam Formation commenced after 1660 Ma and ceased prior to the deposition of the Kurnool Group which was deposited < 1090 Ma. The Srisailam Formation was deposited in a tidal flat/shallow marine environment as it contains tidal and storms influences, glauconitic sandstones, along with bimodal east-west paleocurrents, which suggest links with an open seaway. Detrital zircon Hf isotope data combined with detrital zircon U-Pb data suggest the Dharwar Craton as a dominant source region with a mixed crustal evolution (ɛHf -11 to +8). Detrital zircon age peaks at ~3200 Ma, ~2700-2400 Ma and ~2300 Ma imply that sediments are dominantly sourced from 3400-3000 Ma tonalite-trondhjemite-granodiorite (TTG), 3000-2500 Ma volcanosedimentary greenstone belts and 2600-2500 Ma calc-alkaline to K-rich granitic intrusions. Trace element data suggests zircon grains are sourced from granitoids with zircon crystallisation at ~860˚C. This study reveals that the Srisailam Formation is quite possibly a lateral equivalent of the Nallamalai Group.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011

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Книги з теми "Dharwar Craton"

Rao, A. T. A crustal section of eastern Dharwar craton-Godavari rift-Eastern Ghats mobile belt, India: Field excursion guide book. Bangalore: Geological Society of India, 1997.

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Частини книг з теми "Dharwar Craton"

Moyen, Jean-François. "Dharwar Craton." In Encyclopedia of Astrobiology, 631–34. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_5149.

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Pandey, Om Prakash. "Dharwar Craton." In Society of Earth Scientists Series, 41–88. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40597-7_2.

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Moyen, Jean-François. "Dharwar Craton." In Encyclopedia of Astrobiology, 1–4. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-642-27833-4_5149-2.

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Moyen, Jean-François. "Dharwar Craton." In Encyclopedia of Astrobiology, 1–4. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_5149-1.

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Piispa, E. J., A. V. Smirnov, L. J. Pesonen, M. Lingadevaru, K. S. Anantha Murthy, and T. C. Devaraju. "An Integrated Study of Proterozoic Dykes, Dharwar Craton, Southern India." In Dyke Swarms:Keys for Geodynamic Interpretation, 33–45. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-12496-9_3.

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Das, J. N., M. M. Korakoppa, Fareeduddin, S. Shivanna, J. K. Srivastava, and N. L. Gera. "Tuffisitic Kimberlite from Eastern Dharwar Craton, Undraldoddi Area, Raichur District, Karnataka, India." In Proceedings of 10th International Kimberlite Conference, 109–28. New Delhi: Springer India, 2013. http://dx.doi.org/10.1007/978-81-322-1173-0_8.

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Patil Pillai, Shilpa, and Vivek S. Kale. "Interplay Between Tectonics & Eustacy in a Proterozoic Epicratonic, Polyhistory Basin, North Dharwar Craton." In Tectonics and Structural Geology: Indian Context, 75–114. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99341-6_4.

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Newton, R. C. "The Late Archean High-Grade Terrain of South India and the Deep Structure of the Dharwar Craton." In Exposed Cross-Sections of the Continental Crust, 305–26. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0675-4_12.

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Sunder Raju, P. V., and R. K. W. Merkle. "Högbomite Associated with Vanadiferous–Titaniferous Magnetite Bands at Bhaktarhalli, Nuggihalli Schist Belt, Western Dharwar Craton, Karnataka, India." In Proceedings of the 10th International Congress for Applied Mineralogy (ICAM), 657–64. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-27682-8_79.

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Pahari, Arijit, and C. Manikyamba. "Arc–Back Arc Cohabitation and Associated Bimodal Volcanism: Evidence from Neoarchean Raichur Greenstone Belt, Eastern Dharwar Craton, India." In Geochemical Treasures and Petrogenetic Processes, 3–29. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-4782-7_1.

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Тези доповідей конференцій з теми "Dharwar Craton"

Miller, Scott R., Joseph G. Meert, Anthony F. Pivarunas, Anup K. Sinha, and M. K. Pandit. "PALEOMAGNETISM AND GEOCHRONOLOGY IN THE EASTERN DHARWAR CRATON." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303387.

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Raju, Perumala, and Rajat Mazumder. "THE GEOLOGICAL EVOLUTION OF THE ARCHEAN DHARWAR-CRATON." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-364281.

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Devaraju, T. C., and T. T. Alapieti. "Exploration for PGE Mineralization in the Western Dharwar Craton." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63389.

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Pal, S. K., and S. Kumar. "Kimberlite mapping using Electrical Resistivity Tomography in Wajrakarur kimberlite field, Eastern Dharwar craton." In 1st Indian Near Surface Geophysics Conference & Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201979029.

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Manikyamba, C., and Abhishek Saha. "PGE Geochemistry of Komatiites from Neoarchean Sigegudda Greenstone Terrane, Western Dharwar Craton, India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63398.

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Ravindran, Arathy, Klaus Mezger, and Balakrishnan Srinivasan. "Composition of the Archaean Mantle and Continental Crust in the Western Dharwar Craton, India." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2175.

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Sebastian, Sibin, Rajneesh Bhutani, and Srinivasan Balakrishnan. "Crustal Reworking in the Archaean: Geochemical Evidences from Granitoid of the Western Dharwar Craton." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2330.

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Kumar, S., and S. K. Pal. "Interpretation of VLF-EM data over Wajrakarur kimberlite pipe 2, Eastern Dharwar craton, India." In 1st Indian Near Surface Geophysics Conference & Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201979053.

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Velarde, Landon D., Scott R. Miller, George D. Kamenov, Paul A. Mueller, Joseph G. Meert, Anup K. Sinha, and M. K. Pandit. "MAJOR AND TRACE ELEMENT GEOCHEMISTRY AND PB-ND ISOTOPES OF MAFIC DYKES, DHARWAR CRATON, INDIA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-340235.

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Chakravadhanula, Manikyamba. "Archean Biogeochemical Processes, Dharwar Craton, India: Isotopic and Geochemical Evidences for the Early Record of Life." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.354.

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