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Academic and Professional Career: ± 1978: M.Sc.(Geology & Mining) Azerbaijan State
University (Baku, former USSR) Fields of Research: ] Major interests are in the fields of sedimentology/stratigraphy,
and sedimentation and tectonics. Primary emphasis is on the sedimentary basin
analysis: including interpretation of the palaeoenvironments and basin-fill
history in relation to the structural evolution and tectonic framework of
sedimentary basins. At present working on the sedimentation and basin-fill
history of the Neogene clastic succession within the Bengal Basin,
Bangladesh. ] Other areas of interest include modern fluvial sedimentology and
geomorphology, and clastic sedimentary petrology. Contact addresses: Work: Department of Geology Home:
335,
Research Interests: „ During the past decade the main interest and focus of Dr. Alam's
research has been on the facies and facies sequence analyses of the
predominantly clastic Tertiary sedimentary succession exposed onland as well
as in the subsurface of the Bengal Basin, Bangladesh, in order to interpret
the overall palaeogeographic settings and the depositional environments of
the Neogene Surma Group and Tipam Group sediments within the basin. In recent
years, particular emphasis has been on the onland clastic sedimentary sequences
exposed in the Chittagong-Tripura Fold Belt (CTFB) of the southeastern „ Over the past few years the main line of Dr. Alam's research has
been to focus on understanding the depositional history of the
Tertiary-Holocene sedimentary-fill of the „ Development of lithostratigraphic and allostratigraphic
classifications for the Tertiary succession within the Bengal Basin,
Bangladesh on the basis of detailed facies and facies sequence analyses of
both the exposed onland successions and the subsurface core data, wireline
log data, and seismic sections. „ Development of a tectonic framework for the Bengal Basin,
Bangladesh, in an effort to unveil the depositional history of the
sedimentary basin-fill in relation to the three major tectonic provinces
within the basin, namely – (i) the Stable Shelf in
the northwest; (ii) the Central Deep Basin (including the Sylhet Trough in
the northeast and the Hatia Trough in the south); and (iii) the
Chittagong-Tripura Fold Belt in the east. Selected Publications: 1. Alam, M.M., Crook, K.A.W. and Taylor, G. (1985): Fluvial herring-bone cross-stratification in modern tributary
mouth bar, 2. Alam, M.M. (1991a): Paleoenvironmental
study of the Barail sediments exposed in northeastern 3. Alam, M.M. (1991b): Some distinctive
aspects of braiding and anastomosing with reference to the Jamuna and 4. Alam, M.M. (1991c): Sedimentation on
the channel banks in a multi-channel river system. 5. Alam, M.M. (1992a): Sedimentation in
modern anastomosed-fluvial environment: An example from the semi-arid eastern
6. Alam, M.M. (1992b): Sedimentology of a
large-scale sandy braided-fluvial system: The Jamuna River, Bangladesh. 7. Alam, M.M. (1994): Study of
proximal-distal relationships in a sandy braided-fluvial environment:
Significance in paleofluvial interpretation. 8. Alam, M.M. (1995): Tide-dominated
sedimentation in the upper Tertiary succession of the Sitapahar anticline, 9. Alam, M.M. and Ferdous, M.H.S. (1995): Lithofacies analysis and depositional environments of the Lichubagan
Sandstone Formation in the Sitapahar anticline, southeastern Folded Belt of
Bangladesh. J. Indian Assoc. Sediment., 14, 9-18. 10. Alam, M.M. (1996): Low-sinuosity
braided-fluvial sedimentation model: A comparison of the Lichubagan Sandstone
Formation (LS), Sitapahar anticline, and the Jamuna ( 11. Alam. M.M. and Ferdous, M.H.S. (1996): Neogene clastic succession of the Sitapahar
anticline, southeastern 12. Huq, N.E., Rahman, S.H. and Alam, M.M. (1997): Sedimentology of bar-top sequence in the 13. Alam, M.M. and Karim, S.M.R. (1997): Sedimentology of part of the Neogene succession
in the Mirinja anticline, southeastern folded belt of the Bengal Basin,
Bangladesh. 14. Alam, M.M. and Hoque, N. (1998): Channel pattern and sedimentation style in the
Meghna River, Bangladesh: An example of a large-scale anastomosing system. J.
Remote Sensing & Environment, 2, 71-85. 15. Gani, M.R. and Alam, M.M. (1999):
Trench-slope controlled deep-sea clastics in the exposed lower Surma Group in
southeastern fold belt of the Bengal Basin, Bangladesh. Sediment. Geol.,
127(3-4), 219-236. 16. Sultana D.N. and Alam, M.M. (2000): Facies analysis of the Surma Group succession in the subsurface
of the 17. ALAM, M.M. & CURRAY, J.R.
(2002): Editorial: The curtain goes up a sedimentary basin in
south-central 18. ALAM, M., ALAM, M.M., CURRAY, J.R., CHOWDHURY, M.L.R.
& GANI, M.R. (2002): An overview of the sedimentary
geology of the 19. SIKDER, A.M. & ALAM, M.M. (2002): 2-D modelling of the anticlinal structures and structural
development of the eastern fold belt of the Bengal Basin, Bangladesh. In:
Alam, M.M. & Curray, J.R. (Eds.), Sedimentary geology of the Bengal
Basin, Bangladesh, in relation to the Asia-Greater India collision and the
evolution of the eastern Bay of Bengal. Special Issue, Sediment. Geol.,
(in press). 20. GANI, M.R. & ALAM, M.M. (2002): Sedimentation and basin-fill history of the Neogene clastic
succession exposed in the southeastern fold belt of the Bengal Basin,
Bangladesh: A high-resolution sequence stratigraphic approach. In: Alam,
M.M. & Curray, J.R. (Eds.), Sedimentary geology of the Bengal Basin,
Bangladesh, in relation to the Asia-Greater India collision and the evolution
of the eastern Bay of Bengal. Special Issue, Sediment. Geol., (in
press). |
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