Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Verdine-Bearing Oolitic Sand from Cores, off Ganges-Brahmaputra Mouth, Bay of Bengal


Affiliations
1 Geological Survey of India, 29, Jawaharlal Nehru Road, Kolkata - 700 016, India
 

   Subscribe/Renew Journal


Three sediment cores (116 to 125 cm long) collected from outer continental shelf from water depths of 120 to 150 m off Ganges-Brahmaputra mouth in the Bay of Bengal show oolitic sand horizons at subsurface levels around 25, 50 and 100 cm, alternating with highly assorted terrigenous clayey silt. Sediment texture, mineral and biogenic assemblage indicate near shore reefal environment for the oolitic sands. Green grains in oolitic sediments have been identified as phyllite V of verdine facies. It is inferred that the verdine-bearing oolitic sands are deposited during early Holocene transgressive phase.
Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 244

PDF Views: 146




  • Verdine-Bearing Oolitic Sand from Cores, off Ganges-Brahmaputra Mouth, Bay of Bengal

Abstract Views: 244  |  PDF Views: 146

Authors

Amitava Bandyopadhyay
Geological Survey of India, 29, Jawaharlal Nehru Road, Kolkata - 700 016, India

Abstract


Three sediment cores (116 to 125 cm long) collected from outer continental shelf from water depths of 120 to 150 m off Ganges-Brahmaputra mouth in the Bay of Bengal show oolitic sand horizons at subsurface levels around 25, 50 and 100 cm, alternating with highly assorted terrigenous clayey silt. Sediment texture, mineral and biogenic assemblage indicate near shore reefal environment for the oolitic sands. Green grains in oolitic sediments have been identified as phyllite V of verdine facies. It is inferred that the verdine-bearing oolitic sands are deposited during early Holocene transgressive phase.