Browsing by Title
Now showing items 5272-5291 of 9167
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Morphology and evolution of the central west coast of India
(Indian Association for Limnology and Oceanography, 1989) -
Morphology and grain-size characteristics of a log-spiral beach at Nagwa (Diu), west coast of India
(CSIR-NISCAIR, 1985)Sediment samples collected along 6 beach profiles of a log-spiral shaped beach and nearby dunes have been studied for particle size distribution in relation to wave refraction patterns. The results reveal that the foreshore ... -
Morphology and petrography of pumice from the Central Indian Ocean Basin
(CSIR-NISCAIR, 1988)Majority of pumice are equant with high Corey's shape factor values. Petrographic studies indicate flow bands of isotropic nature, with varied vesicle shape and size, and the diffractograms show them to be mainly composed ... -
Morphology and physiology of the marine straminipilan fungi, the aplanochytrids isolated from the equatorial Indian Ocean
(NISCAIR, CSIR, 2006)While thraustochytrids, a group of unicellular marine straminipilan protists, have been found to be abundant in the water column, little is known of aplanochytrids. These constitute one of the 3 groups belonging to the ... -
Morphology and tectonics of Mahanadi Basin, northeastern continental margin of India from geophysical studies
(Elsevier, 2008)The bathymetry, total intensity magnetic and satellite free-air gravity data over the eastern continental margin of India between the latitudes 18 degrees 30 minutes N and 20 degrees N within the water depths of 25-2300 m ... -
Morphology of a coral bank, western continental shelf of India: A multibeam study
(Geological Society of India, 1993)Morphology of a living coral bank (Gaveshani Bank) is described using multibeam swath bathymetric survey system Hydrosweep. The bank has a height of 42 m, length of 2 km and a maximum width of 1.66 km, with steep flanks ... -
Morphology of an uncharted seamount from Central Indian Basin
(Elsevier, 1989)The morphology of a seamount at 12 degrees 35'S and 76 degrees 16'E is studied. This conical seamount has a maximum height of 1275 m (water depth 4135 m) and covers an area of about 189 sq km. The maximum basal extension ... -
Morphology of pockmarks along the western continental margin of India: Employing multibeam bathymetry and backscatter data
(Elsevier, 2010)This study addresses the morphology of pockmarks along the western continental margin of India using multibeam bathymetry and backscatter data. Here, for the first time we have utilized the application of ArcGIS (Geographical ... -
Morphology, taxonomy and ecology of Thraustochytrids and Labyrinthulids, the marine counterparts of zoosporic fungi
(M D Publications, New Delhi, India, 1996)The most common zoosporic fungi, or to use a compromising, term which seems right according to the current perspective, the fungi-like protists, in the marine environment are the thraustochytrids and labyrinthulids. According ... -
Morphometric analyses of the river basins in Goa
(Geographical Society of India, 1987)Morphometric analyses of seven river basins in Goa, India have been carried out. The linear and areal aspects of these basins are reported here. The plots of stream order versus stream numbers and stream orders versus mean ... -
Morphometric characteristics in the horseshoe crab Tachypleus gigas (Arthropoda: Merostomata)
(NISCAIR, CSIR, 2000)The relationships observed between total carapace length with carapace width, carapace weight, telson length, body weight were found statistically significant (p < 0.05) in the male and female horseshoe crab, Tachypleus ... -
Morphometric studies in Penaeus merguiensis from Ratnagiri waters for selection of the brood stock in genetic improvement programmes
(Indian Fisheries Association, 1990) -
Morphometric studies on a part of Central Indian Ocean
(Geological Society of India, 1989)Morphometric and slope angle studies carried out on a part of Indian Ocean Basin have shown that gentle slope angle ranges dominate, 92% of the area represented by 0-3 degrees slopes. Young's hypothesis of log-normal ... -
Morphometry and cell volumes of diatoms from a tropical estuary of India
(NISCAIR, India, 2009)Cell volumes and per cell carbon contents of different diatoms (10 centric, 14 pennate and 1 dinoflagellate) collected from Dona Paula Bay in the central west coast of India have been analyzed. Morphometric information on ... -
Morphometry and electrophoretic studies of Cynoglossus bilineatus (Lac.) from Bombay waters
(Indian Fisheries Association, 1972) -
Morphotectonic and petrological variations along the southern Central Indian Ridge
(Springer, 2016)In order to ascertain the effect of geomorphic and tectonic domains on the formation, enrichment, and ascension of the ridge axis melt, structural and petrological data from a nearly 300-km-long axial stretch along the ... -
Morphotectonic architecture of an India–Madagascar breakup related anomalous submarine terrace complex on the southwest continental margin of India
(Elsevier, 2013)An anomalous lateral bathymetric protrusion [Alleppey–Trivandrum Terrace Complex (ATTC)] in the form of two contiguous terrace-like features exists in the mid-continental slope off southwest coast of India. This bathymetric ... -
Morphotectonic characteristics, distribution and probable genesis of bathymetric highs off southwest coast of India
(Elsevier, 2018)The western continental margin of India and the adjacent deep ocean basins were formed by break-up and separation among India, Seychelles and Madagascar since the Late Cretaceous. The initial India-Madagascar separation ... -
Morphotectonic signatures and revised timing of opening of the Andaman Backarc Basin, Northeast Indian Ocean
(Elsevier, 2021)The Andaman Backarc Basin is believed to have been formed by the present episode of seafloor spreading in the Andaman Sea, separating the Alcock Rise in the north (Burmese Plate) and the Sewell Rise in the south (Sunda ... -
Morphotectonics of the Carlsberg Ridge between 62 degrees 20 minutes and 66 degrees 20 minutes E, northwest Indian Ocean
(Elsevier, 2008)The segmentation pattern of 440 km long section of the Carlsberg Ridge between 62 degrees 20 minutes E and 66 degrees 20 minutes E, in the northwest Indian Ocean, has been studied using multibeam bathymetry and magnetic ...