Recognises six zones by modal proportions of heavy minerals. The sediments were mostly derived from the Himalayas. Detritus from the Indian subcontinent is found sporadically in clay-rich sediments that were deposited during periods of slow sedimentation, where the deep-sea channel migrated away from the drilled sites. -from Authors
CITATION STYLE
Yokoyama, K., Amano, K., Taira, A., & Saito, Y. (1990). Mineralogy of silts from the Bengal Fan. Proc., Scientific Results, ODP, Leg 116, Distal Bengal Fan, 59–75. https://doi.org/10.2973/odp.proc.sr.116.116.1990
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