Special Program for International Students

GRADUATE COURSE IN EARTH SCIENCE
  & GEOENVIRONMENTAL SCIENCE
Current MEXT students


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Fig.1 Large scale trough cross stratification in the basal part of a channel in the lower part of the Tipam Sandstone formation on the right bank of the Hari River, south-west of the Lalakhal tea garden, Jaintiapur, North-eastern Sylhet, Bangladesh

Hossain H. M. Zakir (Bangladesh)

Email: zakir_kln @yahoo.com,
s049220 @matsu.shimane-u.ac.jp

Thesis title:  Petrographic and geochemical characterization of the Tertiary succession in the Sylhet Basin, Bangladesh.
Supervisor:  Dr. Barry Roser (2004-2006).

The Bengal basin is situated in the eastern part of the Indian sub-continent, occupying all of Bangladesh, and West Bengal, Myanmar, and Tripura, as well as part of the Bay of Bengal. The basin had its origin during the collision of India with Eurasia and Myanmar, building the extensive Himalayan and Indo-Burman Ranges. The Bengal Basin constitutes one of the thickest Tertiary sedimentary sequences in the world.

The Sylhet Basin is a rapidly subsiding sub-basin of the Bengal Basin, and is a tectonically complex province in northeastern Bangladesh. The basin contains hydrocarbon reserves which are the only natural energy resource discovered in Bangladesh to date. Topographically it is characterized by low rounded hillocks with cliffs and scarps. My thesis research will examine the petrography and geochemistry of Tertiary sediments in the Sylhet basin within the age range of Mid Eocene to Mio-Pliocene. The results of this study may contribute to solving problems associated with the development and production of hydrocarbon resources, and also characterize the nature of strata in this region.

Aim and Objectives:


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