Monsoon rainfall and contrasting source rocks influenced sediment composition of peninsular basins along the east coast of India (western Bay of Bengal)

Author:

Peketi A.,Mazumdar A.,Pillutla S.P.K.,Rai V.K.,Sawant B.,Chaitanya A.V.S.,krishna Rama

Funder

Council of Scientific and Industrial Research, India

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference124 articles.

1. Sr, Nd isotopic evidence of terrigenous flux variations in the Bay of Bengal: implications of monsoons during the last ~34,000 years;Ahmad;Geophys. Res. Lett.,2005

2. Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera;Ahmad;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2008

3. Strontium and neodymium isotopic compositions in sediments from Godavari, Krishna and Pennar rivers;Ahmad;Curr. Sci.,2009

4. South Asian monsoon history over the past 60 kyr recorded by radiogenic isotopes and clay mineral assemblages in the Andaman Sea;Ali;G-cubed,2015

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