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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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1

Biswal, T. K., and S. K. Jena. "Large Lateral Ramp in the Fold-Thrust Belts of Mesoproterozoic Eastern Ghats Mobile Belt, Eastern India." Gondwana Research 2, no. 4 (October 1999): 657–60. http://dx.doi.org/10.1016/s1342-937x(05)70232-x.

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2

Chetty, T. R. K. "The Eastern Ghats Mobile Belt, India: A Collage of Juxtaposed Terranes (?)." Gondwana Research 4, no. 3 (July 2001): 319–28. http://dx.doi.org/10.1016/s1342-937x(05)70332-4.

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3

Nanda, J. K., and U. C. Pati. "Geochemistry and original nature of Precambrian khondalites in the Eastern Ghats, Orissa: a discussion." Transactions of the Royal Society of Edinburgh: Earth Sciences 82, no. 1 (1991): 87–88. http://dx.doi.org/10.1017/s0263593300007537.

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Анотація:

While congratulating the authors for the wealth of geochemical data on a very important Precambrian lithological assemblage of India, known commonly as khondalites, which constitute a major part of the Eastern Ghats mobile belt bordering the eastern fringes of the Indian Peninsula, we have a few comments to offer on the hypothesis propounded by the authors (Dash et al. 1987).

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4

Jana, Niptika, Arun Singh, Ashwani Kant Tiwari, Chandrani Singh, and Rahul Biswas. "Mantle deformation patterns and signatures of rift, beneath Eastern Ghats Mobile Belt." Physics of the Earth and Planetary Interiors 289 (April 2019): 20–33. http://dx.doi.org/10.1016/j.pepi.2019.01.009.

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5

Biswal, T. K., and Suspa Sinha. "Deformation history of the NW salient of the Eastern Ghats Mobile Belt, India." Journal of Asian Earth Sciences 22, no. 2 (October 2003): 157–69. http://dx.doi.org/10.1016/s1367-9120(02)00182-7.

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6

Jana, Niptika, Astha Singh, Ashwani Kant Tiwari, Tuna Eken, Arun Singh, Chandrani Singh, and Uma Shankar. "Seismic anisotropy and mantle deformation beneath Eastern Ghats Mobile Belt using direct-S waves." Precambrian Research 360 (July 2021): 106215. http://dx.doi.org/10.1016/j.precamres.2021.106215.

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7

Singh, Saurabh, Rajeev Kumar Pandey, Divya Prakash, and Chandra Kant Singh. "Geochronology of the Polycyclic Granulite Terrain of The Eastern Ghats Mobile Belt: An Overview." JOURNAL OF SCIENTIFIC RESEARCH 66, no. 01 (2022): 33–40. http://dx.doi.org/10.37398/jsr.2022.660104.

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8

SENGUPTA, P., S. DASGUPTA, P. K. BHATTACHARYA, M. FUKUOKA, S. CHAKRABORTI, and S. BHOWMICK. "Petro-tectonic Imprints in the Sapphirine Granulites from Anantagiri, Eastern Ghats Mobile Belt, India." Journal of Petrology 31, no. 5 (October 1, 1990): 971–96. http://dx.doi.org/10.1093/petrology/31.5.971.

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9

Chalapathi Rao, N. V. "Glimmeritic enclave in a lamprophyre from the Settupalle alkaline pluton, Eastern Ghats mobile belt." Journal of the Geological Society of India 75, no. 6 (June 2010): 783–90. http://dx.doi.org/10.1007/s12594-010-0073-1.

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10

Mahapatro, S. N., A. K. Tripathy, J. K. Nanda, and Abhinaba Roy. "Coexisting ultramylonite and pseudotachylyte from the eastern segment of the Mahanadi shear zone, Eastern Ghats Mobile Belt." Journal of the Geological Society of India 74, no. 6 (December 2009): 679–89. http://dx.doi.org/10.1007/s12594-009-0184-8.

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11

Biswal, T. K., D. Seward, and S. K. Jena. "Eastern Ghats Mobile Belt is an Epitome of Mesoproterozoic Fold Thrust Belt: A Study from its NW Margin." Gondwana Research 4, no. 4 (October 2001): 579–81. http://dx.doi.org/10.1016/s1342-937x(05)70383-x.

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12

Chandrasekhar, E., D. Ramesh, and T. K. Biswal. "Magnetotelluric evidence on the southward extension of the Eastern Ghats mobile belt from Ongole, India." Journal of Asian Earth Sciences 164 (September 2018): 23–32. http://dx.doi.org/10.1016/j.jseaes.2018.06.009.

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13

Biswal, T. K. "Fold-thrust belt geometry of the Eastern Ghats Mobile Belt, a structural study from its western margin, Orissa, India." Journal of African Earth Sciences 31, no. 1 (July 2000): 25–33. http://dx.doi.org/10.1016/s0899-5362(00)00070-1.

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14

BHATTACHARYA, S., RAJIB KAR, S. MISRA, and W. TEIXEIRA. "Early Archaean continental crust in the Eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite." Geological Magazine 138, no. 5 (September 2001): 609–18. http://dx.doi.org/10.1017/s0016756801005702.

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Анотація:

The Eastern Ghats granulite belt of India has traditionally been described as a Proterozoic mobile belt, with probable Archaean protoliths. However, recent findings suggest that synkinematic development of granulites took place in a compressional tectonic regime and that granulite facies metamorphism resulted from crustal thickening. The field, petrological and geochemical studies of a charnockite massif of tonalitic to trondhjemitic composition, and associated rocks, document granulite facies metamorphism and dehydration partial melting of basic rocks at lower crustal depths, with garnet granulite residues exposed as cognate xenoliths within the charnockite massif. The melting and generation of the charnockite suite under granulite facies conditions have been dated c. 3.0 Ga by Sm–Nd and Rb–Sr whole rock systematics and Pb–Pb zircon dating. Sm–Nd model dates between 3.4 and 3.5 Ga and negative epsilon values provide evidence of early Archaean continental crust in this high-grade terrain.

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15

Biswal, T. K., and S. Sinha. "Fold-Thrust-Belt Structure of the Proterozoic Eastern Ghats Mobile Belt: A Proposed Correlation Between India and Antarctica in Gondwana." Gondwana Research 7, no. 1 (January 2004): 43–56. http://dx.doi.org/10.1016/s1342-937x(05)70305-1.

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16

Chetty, T. R. K., and D. S. N. Murthy. "Collision tectonics in the late Precambrian Eastern Ghats Mobile Belt: mesoscopic to satellite-scale structural observations." Terra Nova 6, no. 1 (January 1994): 72–81. http://dx.doi.org/10.1111/j.1365-3121.1994.tb00635.x.

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17

Mandal, Animesh, Saibal Gupta, William K. Mohanty, and Surajit Misra. "Sub-surface structure of a craton–mobile belt interface: Evidence from geological and gravity studies across the Rengali Province–Eastern Ghats Belt boundary, eastern India." Tectonophysics 662 (November 2015): 140–52. http://dx.doi.org/10.1016/j.tecto.2015.01.016.

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18

Chetty, T. R. K., P. Vijay, B. L. Narayana, and G. V. Giridhar. "Structure of the Nagavali Shear Zone, Eastern Ghats Mobile Belt, India: Correlation in the East Gondwana Reconstruction." Gondwana Research 6, no. 2 (April 2003): 215–29. http://dx.doi.org/10.1016/s1342-937x(05)70971-0.

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19

Chetty, T. R. K. "Structural architecture of the northern composite terrane, the Eastern Ghats Mobile Belt, India: Implications for Gondwana tectonics." Gondwana Research 18, no. 4 (November 2010): 565–82. http://dx.doi.org/10.1016/j.gr.2010.02.006.

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20

Singh, Saurabh, Divya Prakash, Chandra Kant Singh, Vedika Srivastava, Manoj Kumar Yadav, Pradip Kumar Singh, and Manish Kumar. "Occurrence of sapphirine-bearing granulites from Kothuru, Eastern Ghats Mobile Belt: implications on ultra-high temperature metamorphism." Current Science 122, no. 11 (June 10, 2022): 1298. http://dx.doi.org/10.18520/cs/v122/i11/1298-1304.

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21

B., Swapna. "An ethnobotanical survey of plants used by Yanadi tribe of Kavali, Nellore district, Andhra Pradesh, India." Journal of Scientific and Innovative Research 4, no. 1 (February 25, 2015): 22–26. http://dx.doi.org/10.31254/jsir.2015.4106.

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Анотація:

An ethno botanical survey was undertaken to collect information from Yanadi tribe of Cheruvukattasangham, Kavali, Nellore district, Andhra Pradesh, India. Kavali is a part of Eastern Ghats Mobile Belt which is a Precambrian fold belt extending over 600 km along the east coast of India from the North of Cuttack in Orissa to Nellore in Andhra Pradesh. Yanadi tribe is most prevalent in this region. Besides other usages of plants the practice of oral tradition for healthcare management of human and domesticated animals using herbal medicines is still prevalent among the inhabitants of the area. The study revealed that, the Yanadi tribe used 30 plant species belonging to 20 families to treat scorpion sting, snake bite, cold, helminthic diseases, body pains after delivery in women, dysentery etc. This paper reports the uses of medicinal plants used by tribal people in the form of juices, extracts, decoctions, pastes and powders. The information requires validation for clinical usage.

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22

Gupta, S., A. Bhattacharya, M. Raith, and J. K. Nanda. "Contrasting pressure-temperature-deformation history across a vestigial craton-mobile belt boundary: the western margin of the Eastern Ghats Belt at Deobhog, India." Journal of Metamorphic Geology 18, no. 6 (November 2000): 683–97. http://dx.doi.org/10.1046/j.1525-1314.2000.00288.x.

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23

Baranwal, V. C., S. P. Sharma, D. Sengupta, M. K. Sandilya, B. K. Bhaumik, R. Guin, and S. K. Saha. "A new high background radiation area in the Geothermal region of Eastern Ghats Mobile Belt (EGMB) of Orissa, India." Radiation Measurements 41, no. 5 (May 2006): 602–10. http://dx.doi.org/10.1016/j.radmeas.2006.03.002.

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24

Singh, A. P., and D. C. Mishra. "Tectonosedimentary evolution of Cuddapah basin and Eastern Ghats mobile belt (India) as Proterozoic collision: gravity, seismic and geodynamic constraints." Journal of Geodynamics 33, no. 3 (April 2002): 249–67. http://dx.doi.org/10.1016/s0264-3707(01)00066-7.

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25

Sanyal, Prasanta, B. C. Acharya, S. K. Bhattacharya, A. Sarkar, S. Agrawal, and M. K. Bera. "Origin of graphite, and temperature of metamorphism in Precambrian Eastern Ghats Mobile Belt, Orissa, India: A carbon isotope approach." Journal of Asian Earth Sciences 36, no. 2-3 (September 2009): 252–60. http://dx.doi.org/10.1016/j.jseaes.2009.06.008.

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26

Chetty, T. R. K., B. L. Narayana, P. Vijay, and G. V. Giridhar. "Shear Zones in the Central Part of the Eastern Ghats Mobile Belt, India and Their Continuity Through East Antarctica." Gondwana Research 4, no. 4 (October 2001): 596–97. http://dx.doi.org/10.1016/s1342-937x(05)70399-3.

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27

Mahapatro, S. N. "Geology of the northern contact zone between the Eastern Ghats Mobile Belt and the Singhbhum craton in Odisha sector." Journal of the Geological Society of India 82, no. 6 (December 2013): 724–25. http://dx.doi.org/10.1007/s12594-013-0214-4.

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28

Mahapatro, S. N., N. C. Pant, S. K. Bhowmik, A. K. Tripathy, and J. K. Nanda. "Archaean granulite facies metamorphism at the Singhbhum Craton-Eastern Ghats Mobile Belt interface: implication for the Ur supercontinent assembly." Geological Journal 47, no. 2-3 (July 4, 2011): 312–33. http://dx.doi.org/10.1002/gj.1311.

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29

Chaudhuri, Kuntal, Kajaljyoti Borah, and Sandeep Gupta. "Seismic evidence of crustal low velocity beneath Eastern Ghat Mobile Belt, India." Physics of the Earth and Planetary Interiors 261 (December 2016): 207–16. http://dx.doi.org/10.1016/j.pepi.2016.10.004.

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30

PRAKASH, DIVYA, DEEPAK, PRAVEEN CHANDRA SINGH, CHANDRA KANT SINGH, SUPARNA TEWARI, MAKOTO ARIMA, and HARTWIG E. FRIMMEL. "Reaction textures and metamorphic evolution of sapphirine–spinel-bearing and associated granulites from Diguva Sonaba, Eastern Ghats Mobile Belt, India." Geological Magazine 152, no. 2 (August 14, 2014): 316–40. http://dx.doi.org/10.1017/s0016756814000399.

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Анотація:

AbstractThe Diguva Sonaba area (Vishakhapatnam district, Andhra Pradesh, South India) represents part of the granulite-facies terrain of the Eastern Ghats Mobile Belt. The Precambrian metamorphic rocks of the area predominantly consist of mafic granulite (±garnet), khondalite, leptynite (±garnet, biotite), charnockite, enderbite, calc-granulite, migmatic gneisses and sapphirine–spinel-bearing granulite. The latter rock type occurs as lenticular bodies in khondalite, leptynite and calc-granulite. Textural relations, such as corroded inclusions of biotite within garnet and orthopyroxene, resorbed hornblende within pyroxenes, and coarse-grained laths of sillimanite, presumably pseudomorphs after kyanite, provide evidence of either an earlier episode of upper-amphibolite-facies metamorphism or they represent relics of the prograde path that led to granulite-facies metamorphism. In the sapphirine–spinel-bearing granulite, osumilite was stable in addition to sapphirine, spinel and quartz during the thermal peak of granulite-facies metamorphism but the assemblage was later replaced by Crd–Opx–Qtz–Kfs-symplectite and a variety of reaction coronas during retrograde overprint. Variable amounts of biotite or biotite+quartz symplectite replaced orthopyroxene, cordierite and Opx–Crd–Kfs–Qtz-symplectite at an even later retrograde stage. Peak metamorphic conditions of c. 1000°C and c. 12 kbar were computed by isopleths of XMg in garnet and XAl in orthopyroxene. The sequence of reactions as deduced from the corona and symplectite assemblages, together with petrogenetic grid and pseudosection modelling, records a clockwise P–T evolution. The P–T path is characteristically T-convex suggesting an isothermal decompression path and reflects rapid uplift followed by cooling of a tectonically thickened crust.

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31

Bhattacharya, S., Rajib Kar, and S. Moitra. "Petrogenesis of granitoid rocks at the northern margin of the Eastern Ghats Mobile Belt and evidence of syn-collisional magmatism." Journal of Earth System Science 113, no. 4 (December 2004): 543–63. http://dx.doi.org/10.1007/bf02704022.

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32

Biswal, T. K., Bimal Biswal, Supriyo Mitra, and Maitry Roy Moulik. "Deformation Pattern of the NW Terrane Boundary of the Eastern Ghats Mobile Belt, India: A Tectonic Model and Correlation with Antarctica." Gondwana Research 5, no. 1 (January 2002): 45–52. http://dx.doi.org/10.1016/s1342-937x(05)70887-x.

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33

Bhadra, S., S. Gupta, and M. Banerjee. "Structural evolution across the Eastern Ghats Mobile Belt–Bastar craton boundary, India: hot over cold thrusting in an ancient collision zone." Journal of Structural Geology 26, no. 2 (February 2004): 233–45. http://dx.doi.org/10.1016/s0191-8141(03)00112-3.

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34

Ghosh, Arya, Tapas Bhattacharyya, Rajib Kar, and Tapan Moharana. "Structural framework of the transpressive Mahanadi Shear Zone and reevaluation of the regional geology in the northern sector of the Eastern Ghats Mobile Belt, Eastern India." International Journal of Earth Sciences 110, no. 5 (May 11, 2021): 1631–52. http://dx.doi.org/10.1007/s00531-021-02034-8.

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35

ANAND, S. "Study of Aeromagnetic Data Over Part of Eastern Ghat Mobile Belt and Bastar Craton." Gondwana Research 6, no. 4 (October 2003): 859–65. http://dx.doi.org/10.1016/s1342-937x(05)71030-3.

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36

Sinha, Suspa, G. Ian Alsop, and T. K. Biswal. "The evolution and significance of microfracturing within feldspars in low-grade granitic mylonites: A case study from the Eastern Ghats Mobile Belt, India." Journal of Structural Geology 32, no. 10 (October 2010): 1417–29. http://dx.doi.org/10.1016/j.jsg.2010.07.006.

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37

Katz, Michael B. "Sri Lanka-Indian Eastern Ghats-East Antarctica and the Australian Albany Fraser Mobile Belt: Gross Geometry, Age Relationships, and Tectonics in Precambrian Gondwanaland." Journal of Geology 97, no. 5 (September 1989): 646–48. http://dx.doi.org/10.1086/629342.

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38

Subba Rao, M. V., and V. Divakara Rao. "Chemical constraints on the origin of the charnockites in the Eastern Ghat mobile belt, India." Chemical Geology 69, no. 1-2 (June 1988): 37–48. http://dx.doi.org/10.1016/0009-2541(88)90156-8.

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39

Kaur, Gurmeet, Roger H. Mitchell, and Suhel Ahmed. "Mineralogy of the Vattikod lamproite dykes, Ramadugu lamproite field, Nalgonda District, Telangana: A possible expression of ancient subduction-related alkaline magmatism along Eastern Ghats Mobile Belt, India." Mineralogical Magazine 82, no. 1 (February 2018): 35–58. http://dx.doi.org/10.1180/minmag.2017.081.045.

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Анотація:

ABSTRACTThe mineralogy of nine recently discovered dykes (VL1:VL8 and VL10) in the vicinity of Vattikod village, Nalgonda district in Telangana State is described. The mineral assemblage present and their compositions are comparable to those of bona fide lamproites in terms of the presence of phlogopite (Ti-rich, Al-poor phlogopite and tetraferriphlogopite); amphiboles (potassic-arfvedsonite, potassic-richterite, potassic-ferro-richterite, potassic-katophorite, Ti-rich potassic-katophorite, Ti-rich potassic-magnesio-katophorite); Al-poor clinopyroxenes; feldspars (K-feldspar, Ba-K-feldspar and Na-feldspar) and spinels (chromite-magnetite and qandilite-ulvöspinel-franklinite). These dykes have undergone diverse and significant degrees of deuteric alteration as shown by the formation of secondary phases such as: titanite, allanite, hydro-zircon, calcite, chlorite, quartz and cryptocrystalline SiO2. On the basis of their respective mineralogy: the VL4 and VL5 dykes are classified as pseudoleucite-phlogopite lamproite; VL2 and VL3 dykes as pseudoleucite-amphibole-lamproite; and VL6, VL7 and VL8 as pseudoleucite-phlogopite-amphibole-lamproite. VL10 is extensively altered but contains fresh euhedral apatite microphenocrysts together with pseudomorphs after leucite and is classified as a pseudoleucite-apatite-(phlogopite?) lamproite. The mineralogy of the Vattikod lamproite dykes is compared with that of the Ramadugu, Somavarigudem and Yacharam lamproite dykes which also occur in the Ramadugu lamproite field. The lamproites from the Eastern Dharwar Craton are considered as being possible expressions of ancient subduction-related alkaline magmatism along the Eastern Ghats mobile belt.

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40

LEELANANDAM, C., K. BURKE, L. D. ASHWAL, and S. J. WEBB. "Proterozoic mountain building in Peninsular India: an analysis based primarily on alkaline rock distribution." Geological Magazine 143, no. 2 (March 2006): 195–212. http://dx.doi.org/10.1017/s0016756805001664.

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Анотація:

Peninsular India was assembled into a continental block c. 3 million km2 in area as a result of collisions throughout the length of a 4000 km long S-shaped mountain belt that was first recognized from the continuity of strike of highly deformed Proterozoic granulites and gneisses. More recently the recognition of a variety of tectonic indicators, including occurrences of ophiolitic slivers, Andean-margin type rocks, a collisional rift and a foreland basin, as well as many structural and isotopic age studies have helped to clarify the history of this Great Indian Proterozoic Fold Belt. We here complement those studies by considering the occurrence of deformed alkaline rocks and carbonatites (DARCs) in the Great Indian Proterozoic Fold Belt. One aim of this study is to test the recently published idea that DARCs result from the deformation of alkaline rocks and carbonatites (ARCs) originally intruded into intra-continental rifts and preserved on rifted continental margins. The suggestion is that ARCs from those margins are transformed into DARCs during continental, or arc–continental, collisions. If that idea is valid, DARCs lie on rifted continental margins and on coincident younger suture zones; they occur in places where ancient oceans have both opened and closed. Locating sutures within mountain belts has often proved difficult and has sometimes been controversial. If the new idea is valid, DARC distributions may help to reduce controversy. This paper concentrates on the Eastern Ghats Mobile Belt of Andhra Pradesh and Orissa, where alkaline rock occurrences are best known. Less complete information from Kerala, Tamil Nadu, Karnataka, West Bengal, Bihar and Rajasthan has enabled us to define a line of 47 unevenly distributed DARCs with individual outcrop lengths of between 30 m and 30 km that extends along the full 4000 km length of the Great Indian Proterozoic Fold Belt. Ocean opening along the rifted margins of the Archaean cratons of Peninsular India may have begun by c. 2.0 Ga and convergent plate margin phenomena have left records within the Great Indian Proterozoic Fold Belt and on the neighbouring cratons starting at c. 1.8 Ga. Final continental collisions were over by 0.55 Ga, perhaps having been completed at c. 0.75 Ga or at c. 1 Ga. Opening of an ocean at the Himalayan margin of India by c. 0.55 Ga removed an unknown length of the Great Indian Proterozoic Fold Belt. In the southernmost part of the Indian peninsula, a line of DARCs, interpreted here as marking a Great Indian Proterozoic Fold Belt suture, can be traced within the Southern Granulite Terrain almost to the Achankovil-Tenmala shear zone, which is interpreted as a strike-slip fault that also formed at c. 0.55 Ga.

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Singh, Arun, and Chandrani Singh. "Seismic imaging of the deep crustal structure beneath Eastern Ghats Mobile Belt (India): Crustal growth in the context of assembly of Rodinia and Gondwana supercontinents." Precambrian Research 331 (September 2019): 105343. http://dx.doi.org/10.1016/j.precamres.2019.105343.

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Bhattacharya, S. "Nature of Crustal Tri-Junction Between the Eastern Ghats Mobile belt, Singhbhum Craton and Bastar Craton Around Paikmal, Western Orissa: Structural Evidence of Oblique Collision." Gondwana Research 5, no. 1 (January 2002): 53–62. http://dx.doi.org/10.1016/s1342-937x(05)70888-1.

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Raju, D. C. L., and V. Divakara Rao. "Geochemistry and Evolution of Charnockite-Khondalite-Anorthosite Association of Eastern Ghat Mobile Belt - A Fragment of Gondwana." Gondwana Research 4, no. 4 (October 2001): 745–46. http://dx.doi.org/10.1016/s1342-937x(05)70536-0.

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Biswall, T. K., and D. Seward. "Tectonic Implication of the Apatite Fission-track Analysis of the Mylonites from the Terrane Boundary Shear Zone of the Eastern Ghats Mobile Belt Around Lakhna, Orissa." Gondwana Research 6, no. 2 (April 2003): 321–25. http://dx.doi.org/10.1016/s1342-937x(05)70981-3.

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Biswal, T. K. "The Lithotectonic Setting of the Eastern Ghat Mobile Belt and Adjoining Craton in Western Orissa, India: An Example of Mesoproterozoic Fold-Thrust Belt." Gondwana Research 1, no. 3-4 (October 1998): 410–12. http://dx.doi.org/10.1016/s1342-937x(05)70858-3.

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Jana, Niptika, Chandrani Singh, Rahul Biswas, Nitin Grewal, and Arun Singh. "Seismic noise analysis of broadband stations in the Eastern Ghat Mobile Belt of India using power spectral density." Geomatics, Natural Hazards and Risk 8, no. 2 (August 29, 2017): 1622–30. http://dx.doi.org/10.1080/19475705.2017.1365777.

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Biswal, T. K., Harish Ahuja, and Himansu Sekhar Sahu. "Emplacement kinematics of nepheline syenites from the Terrane Boundary Shear Zone of the Eastern Ghats Mobile Belt, west of Khariar, NW Orissa: Evidence from meso- and microstructures." Journal of Earth System Science 113, no. 4 (December 2004): 785–93. http://dx.doi.org/10.1007/bf02704037.

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Biswal, Tapas Kumar, Bert De Waele, and Harish Ahuja. "Timing and dynamics of the juxtaposition of the Eastern Ghats Mobile Belt against the Bhandara Craton, India: A structural and zircon U-Pb SHRIMP study of the fold-thrust belt and associated nepheline syenite plutons." Tectonics 26, no. 4 (July 18, 2007): n/a. http://dx.doi.org/10.1029/2006tc002005.

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Rao, V. Divakara, B. L. Narayana, M. V. Subba Rao, P. Rama Rao, J. Mallikharjuna Rao, N. N. Murthy, and G. L. N. Reddy. "Evolution of the Eastern Ghats Granulite Belt." Gondwana Research 1, no. 3-4 (October 1998): 416–19. http://dx.doi.org/10.1016/s1342-937x(05)70862-5.

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Dasgupta, Somnath, Sankar Bose, and Kaushik Das. "Tectonic evolution of the Eastern Ghats Belt, India." Precambrian Research 227 (April 2013): 247–58. http://dx.doi.org/10.1016/j.precamres.2012.04.005.

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