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Статті в журналах з теми "Eastern Ghats Belt"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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1

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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2

Simmat, Ralf, and Karen Rickers. "Wagnerite in high-MgAl granulites of Anakapalle, Eastern Ghats Belt, India." European Journal of Mineralogy 12, no. 3 (May 31, 2000): 661–66. http://dx.doi.org/10.1127/0935-1221/2000/0012-0661.

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3

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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4

Mukhopadhyay, Dhruba, and Krishnapriya Basak. "The Eastern Ghats Belt … A polycyclic granulite terrain." Journal of the Geological Society of India 73, no. 4 (April 2009): 489–518. http://dx.doi.org/10.1007/s12594-009-0034-8.

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5

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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Анотація:

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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6

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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7

Kumar, K. Vijaya, C. Leelanandam, and W. G. Ernst. "Evolution of the Eastern Ghats Belt, India: A Magmatic Perspective." Journal of the Geological Society of India 97, no. 2 (February 2021): 217. http://dx.doi.org/10.1007/s12594-021-1657-7.

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8

Mahapatro, S. N., A. K. Tripathy, J. K. Nanda, and S. C. Rath. "Petrology of the Udayagiri anorthosite complex, Eastern Ghats Belt, India." Journal of the Geological Society of India 82, no. 4 (October 2013): 319–29. http://dx.doi.org/10.1007/s12594-013-0159-7.

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9

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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10

Bhowmik, Santanu Kumar. "Multiple episodes of tectonothermal processes in the Eastern Ghats granulite belt." Journal of Earth System Science 106, no. 3 (September 1997): 131–46. http://dx.doi.org/10.1007/bf02839285.

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11

Dasgupta, Somnath, Sankar Bose, Santanu Kumar Bhowmik, and Pulak Sengupta. "The Eastern Ghats Belt, India, in the context of supercontinent assembly." Geological Society, London, Special Publications 457, no. 1 (2017): 87–104. http://dx.doi.org/10.1144/sp457.5.

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12

Lal, S. N. "Sapphirine Granulites of Eastern Ghats Belt, India: Evidence of Proterozoic Decompression." Gondwana Research 4, no. 4 (October 2001): 674. http://dx.doi.org/10.1016/s1342-937x(05)70470-6.

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13

Rao, A. T., V. I. Fonarev, A. N. Konilov, and M. Romanenko. "Cheralite from Visakhapatnam Area in the Eastern Ghats Granulite Belt, India." Gondwana Research 1, no. 1 (October 1997): 137–41. http://dx.doi.org/10.1016/s1342-937x(05)70012-5.

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14

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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15

Arima, M., N. Takano, P. Saradhi, and H. Kagami. "Crustal and Mantle Evolution of the Proterozoic Eastern Ghats Belt, India." Gondwana Research 4, no. 4 (October 2001): 564–65. http://dx.doi.org/10.1016/s1342-937x(05)70368-3.

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16

PREMAVANI, D., M. TARAKESWARA NAIDU, O. ANIEL KUMAR, and M. VENKAIAH. "Diversity and distribution of tree species in tropical forests of Northcentral Eastern Ghats, India." Asian Journal of Forestry 1, no. 1 (June 18, 2017): 27–32. http://dx.doi.org/10.13057/asianjfor/r010104.

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Анотація:

Premavani D, Naidu MT, Kumar OA, Venkaiah M. 2017. Diversity and distribution of tree species in tropical forests ofNorthcentral Eastern Ghats, India. Asian J For 1: 27-32. The diversity and distribution of tree species were studied in three 1 ha sites oftropical forests in the northcentral Eastern Ghats of India. The phytosociological data from forest sites were analyzed quantitatively todetermine the basal area, species diversity, richness and stand density. A total of 1,507 individuals of 104 plant taxa, pertaining to 82genera under 41 families were enumerated at â‰¥15 cm gbh using belt transects (5 m Ã— 1000 m). Tree stand density varied from 371-660individuals per ha while average basal area ranged from 14.54 â€“ 46.51 m2 ha-1. Shannon-Weiner Index (H') ranged from 0.97-0.98,Equitability or evenness index ranged from 0.70-0.79 and Margalef richness index ranged from 10.54 â€“ 10.82. The most dominantfamilies were Rubiaceae, Euphorbiaceae, Fabaceae, Moraceae, and Verbenaceae. Our results suggest further development of forestmanagement and biodiversity conservation in Eastern Ghats region.

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17

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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18

Maji, A. K., and S. S. Sarkar. "Quantitative genetic modelling of the Turkel anorthosite, Eastern Ghats Belt, Orissa, India." Journal of Asian Earth Sciences 24, no. 2 (November 2004): 199–211. http://dx.doi.org/10.1016/j.jseaes.2003.10.009.

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19

NARAYANA, B. "Geochemistry and Origin of Megacrystic Granitoid Rocks from Eastern Ghats Granulite Belt." Gondwana Research 2, no. 1 (January 1999): 105–15. http://dx.doi.org/10.1016/s1342-937x(05)70131-3.

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20

Dasgupta, Somnath, and Pulak Sengupta. "Indo-Antarctic Correlation: a perspective from the Eastern Ghats Granulite Belt, India." Geological Society, London, Special Publications 206, no. 1 (2003): 131–43. http://dx.doi.org/10.1144/gsl.sp.2003.206.01.08.

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21

Dasgupta, Somnath. "Petrological evolution of the Eastern Ghats Belt- Current status and future directions." Episodes 43, no. 1 (March 1, 2020): 124–31. http://dx.doi.org/10.18814/epiiugs/2020/020007.

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22

Bose, Sankar, Nilanjana Sorcar, Kaushik Das, Proloy Ganguly, and Sneha Mukherjee. "Pulsed tectonic evolution in long-lived orogenic belts: An example from the Eastern Ghats Belt, India." Precambrian Research 369 (February 2022): 106522. http://dx.doi.org/10.1016/j.precamres.2021.106522.

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23

Bhattacharya, S., A. K. Chaudhary, A. K. Saw, P. Das, and D. Chatterjee. "Mafic granulite xenoliths in the Chilka Lake suite, Eastern Ghats Belt, India: evidence of deep-subduction of residual oceanic crust." Solid Earth Discussions 4, no. 2 (November 5, 2012): 1379–410. http://dx.doi.org/10.5194/sed-4-1379-2012.

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Анотація:

Abstract. Granulite xenoliths preserve key geochemical and isotopic signatures of their mantle source regions. Mafic granulite and pyroxinite xenoliths within massif-type charnockitic rocks from the Eastern Ghats Belt have recently been reported by us. The mafic granulite xenoliths from the Chilka Lake granulite suite with abundant prograde biotite are geochemically akin to Oceanic Island Basalt (OIB). They can be distinguished from the hornblende-mafic granulite xenoliths with signatures of Arc-derived basalt occurring in the other suites of the Eastern Ghats Belt. These two groups of xenoliths in the Paleoproterozoic Eastern Ghats Province have quite distinct Nd-model ages- 1.9 Ga and 2.5 Ga respectively, which may be interpreted as their crustal residence ages. Strong positive Nb anomalies, indicating subducted oceanic crust in the source, LREE enrichment and strongly fractionated REE pattern are key geochemical signatures attesting to their origin as OIB-type magma. Also low Yb and Sc contents and high (La / Yb)N ratios can be attributed to melting in the presence of residual garnet and hence at great depths (> 80 km). The variable enrichment in radiogenic 87Sr, between 0.70052 and 0.71092 at 1.9 Ga and less radiogenic 143Nd between ε-1.54 and 7.46 are similar to those of the OIBs compared to MORBs. As OIBs commonly contain some recycled oceanic crust in their sources, we suggest that the residue of the oceanic crust from a previous melting event (~ 2.5 Ga) that produced the Arc-derived basalts (protoliths of hornblende-mafic granulite xenoliths) could have subducted to great depths and mechanically mixed with the mantle peridotite. A subsequent re-melting event of this mixed source might have occurred at ca. 1.9 Ga as testified by the crustal residence ages of the biotite-mafic granulite xenoliths of the Chilka Lake granulite suite.

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24

Bhattacharya, S., R. Kar, A. K. Saw, and P. Das. "Relative chronology in high-grade crystalline terrain of the Eastern Ghats, India: new insights." Solid Earth Discussions 3, no. 1 (January 17, 2011): 1–17. http://dx.doi.org/10.5194/sed-3-1-2011.

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Abstract. The two major lithology or gneiss components in the polycyclic granulite terrain of the Eastern Ghats, India, are the supracrustal rocks, commonly described as khondalites, and the charnockite-gneiss. Many of the workers considered the khondalites as the oldest component with unknown basement and the charnockite-protoliths as intrusive into the khondalites. However, geochronological data do not corroborate the aforesaid relations. The field relations of the hornblende- mafic granulite with the two gneiss components together with geocronological data indicate that khondalite sediments were deposited on older mafic crustal rocks. We propose a different scenario: Mafic basement and supracrustal rocks were subsequently deformed and metamorphosed together at high to ultra-high temperatures – partial melting of mafic rocks producing the charnockitic melt; and partial melting of pelitic sediments producing the peraluminous granitoids. This is compatible with all the geochronological data as well as the petrogenetic model of partial melting for the charnockitic rocks in the Eastern Ghats Belt.

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25

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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26

Mahapatro, S. N., J. K. Nanda, and A. K. Tripathy. "The Jugsaipatna Anorthosite Complex, Eastern Ghats Belt, India: Magmatic lineage and petrogenetic implications." Journal of Asian Earth Sciences 38, no. 3-4 (April 2010): 147–61. http://dx.doi.org/10.1016/j.jseaes.2009.10.008.

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27

BHOWMIK, S. "Ultrapotassic Rocks along Late Ductile Shear Zones from the Eastern Ghats Belt, India." Gondwana Research 3, no. 1 (January 2000): 55–63. http://dx.doi.org/10.1016/s1342-937x(05)70057-5.

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28

Nagaraju, J., and T. R. K. Chetty. "Emplacement History of Pasupugallu Gabbro Pluton, Eastern Ghats Belt, India: a Structural Study." Gondwana Research 8, no. 1 (January 2005): 87–100. http://dx.doi.org/10.1016/s1342-937x(05)70265-3.

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29

Dobmeier, Christoph, Ralf Simmat, and Michael Raith. "New Constraints on the Proterozoic Crustal Evolution of the Eastern Ghats Belt, India." Gondwana Research 4, no. 4 (October 2001): 609–10. http://dx.doi.org/10.1016/s1342-937x(05)70412-3.

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30

Das, Suman, Abhijit Bhattacharya, Michael M. Raith, Subhadip Bhadra, and Manua Banerjee. "Aluminous sapphirine granulites from the Eastern Ghats Belt (India): Phase relations and relevance to counterclockwise P-T history." European Journal of Mineralogy 18, no. 1 (March 6, 2006): 35–48. http://dx.doi.org/10.1127/0935-1221/2006/0018-0035.

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31

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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32

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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33

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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34

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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35

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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36

Mohan, Anand. "High Grade Metamorphic Rocks: Khondalites and Charnockites from Visakhapatnam, Eastern Ghats Granulite Belt, India." Journal of the Geological Society of India 95, no. 3 (March 2020): 322. http://dx.doi.org/10.1007/s12594-020-1433-0.

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37

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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38

Dobmeier, Christoph J., and Michael M. Raith. "Crustal architecture and evolution of the Eastern Ghats Belt and adjacent regions of India." Geological Society, London, Special Publications 206, no. 1 (2003): 145–68. http://dx.doi.org/10.1144/gsl.sp.2003.206.01.09.

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39

Bhattacharya, S., and M. Basei. "Contrasting magmatic signatures in the Rairakhol and Koraput alkaline complexes, Eastern Ghats belt, India." Journal of Earth System Science 119, no. 2 (April 2010): 175–81. http://dx.doi.org/10.1007/s12040-010-0010-0.

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40

Dasgupta, Somnath, Jürgen Ehl, Michael M. Raith, Pulak Sengupta, and Pranesh Sengupta. "Mid-crustal contact metamorphism around the Chimakurthy mafic-ultramafic complex, Eastern Ghats Belt, India." Contributions to Mineralogy and Petrology 129, no. 2-3 (October 28, 1997): 182–97. http://dx.doi.org/10.1007/s004100050331.

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41

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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42

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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43

Mukhopadhyay, Subir, Supriya Roy, Masato Fukuoka, and Somnath Dasgupta. "Controls of evolution of mineral assemblages in ultrahigh-temperature metamorphosed Mn-carbonate-silicate rocks from the Eastern Ghats Belt, India." European Journal of Mineralogy 14, no. 1 (January 28, 2002): 73–83. http://dx.doi.org/10.1127/0935-1221/2002/0014-0073.

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44

Bhattacharya, Samarendra, and Ashwini Kumar Chaudhary. "Secular evolution of continental crust: recorded from massif-type charnockites of Eastern Ghats belt, India." Natural Science 02, no. 10 (2010): 1079–84. http://dx.doi.org/10.4236/ns.2010.210134.

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45

Rao, B. Veeranarayana. "Petrochemistry and Genesis of Magnetite Ores from Addatigala and Devipatnam, Eastern Ghats Belt, South India." Gondwana Research 4, no. 4 (October 2001): 749. http://dx.doi.org/10.1016/s1342-937x(05)70540-2.

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46

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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47

Kar, Rajib. "Generation of granitic plutons during Crustal orogenesis: An example from the Eastern Ghats granulite belt." Journal of the Geological Society of India 80, no. 5 (November 2012): 653–66. http://dx.doi.org/10.1007/s12594-012-0191-z.

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48

Bhattacharya, S., A. K. Chaudhary, and W. Teixeira. "Mafic dykes at the southwestern margin of Eastern Ghats belt: Evidence of rifting and collision." Journal of Earth System Science 119, no. 6 (December 2010): 815–23. http://dx.doi.org/10.1007/s12040-010-0058-x.

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