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    Seafloor and sediment characteristics in INDEX AREA 

    Sharma, R.; Nath, B.N.; Valsangkar, A.B.; Khadge, N.H.; Gupta, S.M.; Parthiban, G. (Metal Mining Agency of Japan, 1997)
    Seafloor surveys and sediment sampling during the INDEX (Indian Deep-Sea Environmental Experiment) studies in the Central Indian Basin, resulted in identification of Test and Reference Areas, as well of establishment of ...
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    A note on geochemistry of surface sediments from Krishna-Godavari basin, East Coast of India 

    Pattan, J.N.; Parthiban, G.; PrakashBabu, C.; Khadge, N.H.; Paropkari, A.L.; Kodagali, V.N. (The Geological Society of India, 2008)
    A closely spaced 75 surface sediments drawn from ‘Gas Hydrate` Project taken up by National Institute of Oceanography on a regional scale from the Krishna-Godavari Basin (Latitude I5 degrees 35 minutes to 16 degrees 20 ...
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    Himalayan sedimentary pulses recorded by silicate detritus within a ferromanganese crust from the Central Indian Ocean 

    Banakar, V.K.; Galy, A.; Sukumaran, N.P.; Parthiban, G.; Volvaiker, A.Y. (Elsevier, 2003)
    A Central Indian Ocean deep-water seamount hydrogenous ferromanganese crust (SS663-Crust) contains variable (7-23%) amounts of detrital material (silicate-detritus). Taking into account the growth rate of the authigenic ...
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    Coupling between suboxic condition in sediments of the western Bay of Bengal and southwest monsoon intensification: A geochemical study 

    Pattan, J.N.; Mir, I.A.; Parthiban, G.; Karapurkar, S.G.; Matta, V.M.; Naidu, P.D.; Naqvi, S.W.A. (Elsevier, 2013)
    Reconstruction of paleo-redox conditions in a radiocarbon (14C) dated sediment core (SK-218/1), covering the past 45 ka (thousand calendar years), collected from the western Bay of Bengal (Lat: 14 degrees 02′N; Long: 82 ...
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    Geochemistry of deep-sea sediment cores from the Central Indian Ocean Basin 

    Mudholkar, A.V.; Pattan, J.N.; Parthiban, G. (NISCAIR, New Delhi, 1993)
    Four sediment cores from the Central Indian Ocean Basin (CIOB) were studied to characterise the coarse fraction (less than 63 mu), transition metal and major oxide contents. Transition metals (Mn, Cu, Ni, Zn) show enrichment ...
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    Evidence of Himalayan erosional event at approx. 0.5 Ma from a sediment core from the equatorial Indian Ocean in the vicinityof ODP Leg 116 sites 

    Nath, B.N.; Gupta, S.M.; Mislankar, P.G.; Rao, B.R.; Parthiban, G.; Roelandts, I.; Patil, S.K. (Elsevier, 2005)
    A sediment core collected from an area _100 miles south of the ODP Leg 116 (distal Bengal Fan) in the equatorial Indian Ocean was investigated for microfossils, mineralogy, mineral chemistry, magnetic susceptibility, grain ...
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    Productivity fluctuations in the southeastern Arabian Sea during the last 140 ka 

    Pattan, J.N.; Toshiyuki Masuzawab; Naidu, P.D.; Parthiban, G.; Mineko Yamamoto (Elsevier, 2003)
    Detailed analyses of multiple geochemical productivity proxies such as calcium carbonate, biogenic opal, biogenic Ba, organic carbon and total nitrogen have been carried out on a sediment core from the southeastern Arabian ...
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    Fe speciation and Fe/Al ratio in the sediments of southeastern Arabian Sea as an indicator of climate change 

    Pattan, J.N.; Parthiban, G.; Gupta, S.M.; Mir, I.A. (Elsevier, 2012)
    Aluminium, titanium and iron are the major lithogeneous contributors to the marine sediment and their abundance varies strikingly with the intensity of monsoonal precipitation. Al and Ti concentrations in a sediment core ...
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    Chemistry of surface sediment along a north-south transect across the equator in the Central Indian Basin: An assessment of biogenic and detrital influences on elemental burial on the seafloor 

    Banakar, V.K.; Parthiban, G.; Pattan, J.N.; Jauhari, P. (Elsevier, 1998)
    The detailed chemistry of the surface sediment collected along a north-south transect across the equator in the Central Indian Ocean suggest that: biogenic sedimentation north of equator is dominated by carbonate ooze and ...
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    Impacts on surface productivity during sediment dispersal experiment in Central Indian Basin 

    LokaBharathi, P.A.; Nath, B.N.; Ingole, B.S.; Parthiban, G.; Matondkar, S.G.P.; Raghukumar, C.; Khadge, N.H.; Valsangkar, A.B.; Suryanarayana, A.; Jaisankar, S.; Sharma, R. (Taylor and Francis, 2005)
    It is anticipated that in the case of mining of marine minerals, sea floor sediments will be brought up along with the mineral ores and discharged on the surface. These nutrient rich sediments would create a set of different ...
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    Parthiban, G. (12)
    Pattan, J.N. (6)Nath, B.N. (5)Khadge, N.H. (4)Gupta, S.M. (3)Sharma, R. (3)Valsangkar, A.B. (3)Banakar, V.K. (2)Ingole, B.S. (2)LokaBharathi, P.A. (2)... View MoreSubject
    sediments (12)
    deep-sea mining (3)environmental impact (3)geochemistry (3)mineralogy (3)organic carbon (3)benthos (2)deep water (2)detritus (2)ecosystem disturbance (2)... View MoreDate Issued2010 - 2013 (2)2000 - 2009 (7)1993 - 1999 (3)Has File(s)Yes (12)

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