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dc.contributor.authorGuptha, M.V.S.
dc.date.accessioned1997-11-27T09:57:05Z
dc.date.accessioned2017-09-29T13:46:48Z
dc.date.available1997-11-27T09:57:05Z
dc.date.available2017-09-29T13:46:48Z
dc.date.issued1979
dc.identifier.citationJournal of the Geological Society of India, vol.20(3); 1979; 107-113
dc.identifier.issn0016-7622
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/5251
dc.description.abstractThe degree of fragmentation and colour of the skeletal fragments, colouration in benthic foraminifers have been studied in surficial sediment samples collected from forty stations from the continental shelf region between Ratnagiri in the south and Indus canyon in the north. The abundance peaks of fragmented shells correspond to the terrace depths of -65, -75, -85 and -92 m in the outer shelf region off Ratnagir which indicate the different phases of eustatic sea levels. It is inferred from the occurrence of abundance peaks at similar depths in the other regions of the continental shelf that they must correspond to the presence of lowered strands. The disposition of the black shells in a linear fashion parallel to the coast line at the depths mentioned above also supports the proposition
dc.languageen
dc.publisherGeological Society of India
dc.relation.ispartofJ Geol Soc India
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.othercontinental shelves
dc.subject.otherforaminifera
dc.subject.otherbenthos
dc.subject.othersediments
dc.subject.othereustatic changes
dc.subject.othersea level changes
dc.subject.othersedimentary environments
dc.subject.otherISW, India, West Coast
dc.titleSediments of the western continental shelf of India - Environmental significance
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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