Distribution of grain size and clay minerals in sediments from the INDEX area, central Indian Basin

• Main Authors: Valsangkar, A.B., Ambre, N.V.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Taylor and Francis 2000
• Subjects: sediments; granulometry; grain size; clay minerals; lithology; particle size; mineralogy; Antarctic; Indian; Antarc*
• Online Access: http://drs.nio.org/drs/handle/2264/1649

The granulometry of 21 box core sediments from five selected sites in the Central Indian Basin (CIB) have been studied to understand the sediment size characteristics in the Pioneer area before the benthic disturbance experiment. The sediments are predominantly clayey silt. Statistical parameters were determined to understand the control and variations in the grain size. The mean grain size (M sub(2) phi) ranged from 7.0 to 8.6 for the surface and from 6.6 to 8.6 for the subsurface sediments, indicating deposition of very fine fractions during the Neogene period. The sediments were poorly sorted as revealed from the higher sigma sub(1) values (2.7 to 2.9). Higher and negative values of skewness (SK sub(1)) indicated a winnowing action of prevailing currents in the area. Average kurtosis (K sub(G)) values for the surface (0.4 to 0.8) and subsurface (0.5 to 1.2) showed that sediments were very platykurtic and leptokurtic. Clay mineralogical studies showed that smectite had a wider range (from 6% to 55%) and decreased southward because of its terrigenous origin. The terrigenous influence of the sediments could be documented as far as 12 degrees S. Smectite and kaolinite increased eastward and chlorite decreased southward. This observation positively correlated with the mean current direction in the area. However, the influence of Antarctic Bottom Water (AABW) in the area could be predicted from the southward increase in chlorite content