Coarse fraction components in a red-clay sedimemt core, Central Indian Ocean Basin: Their occurrence and significance

dc.contributor.author	Iyer, S.D.
dc.contributor.author	Fernandes, G.Q.
dc.contributor.author	Mahender, K.
dc.date.accessioned	2016-10-04T10:57:24Z
dc.date.available	2016-10-04T10:57:24Z
dc.date.issued	2012
dc.identifier.citation	Journal of the Indian Association of Sedimentologists. 31(1-2); 2012; 123-135.	en_US
dc.identifier.uri	http://irgu.unigoa.ac.in/drs/handle/unigoa/4583
dc.description.abstract	Coarse Fractions Components of a sediment core (268 cm from a water depth of 5120 m) collected at 18 degrees S and 80 degrees E from the red clay domain in the Central Indian Ocean Basin (CIOB), comprises mineral grains, basaltic fragments, phillipsite, ferromanganese micronodules, glass shards, small pumices, microtektites and biogenic material. This paper describes the provenance of these coarse fraction components that have resulted from multiple sources- both in situ and derived products.	en_US
dc.publisher	Indian Association of Sedimentologists	en_US
dc.subject	Earth Science	en_US
dc.title	Coarse fraction components in a red-clay sedimemt core, Central Indian Ocean Basin: Their occurrence and significance	en_US
dc.type	Journal article	en_US