14.11.2012 Views

SOUVENIR COMMITTEE - Birbal Sahni Institute of Palaeobotany

SOUVENIR COMMITTEE - Birbal Sahni Institute of Palaeobotany

SOUVENIR COMMITTEE - Birbal Sahni Institute of Palaeobotany

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Training Programme on “PALYNOLOGY IN FOSSIL FUEL EXPLORATION”<br />

[ September 10-17, 2012 ]<br />

Name BABEESH. C<br />

Email Address bbshivakripa@gmail.com<br />

Phone/Mobile No. 09566143252<br />

DOB 09/11/1989<br />

Mailing Address Research Scholar, Dept. <strong>of</strong> Geology, Anna<br />

University,Chennai-600025<br />

Name <strong>of</strong> Organization Anna University<br />

Academic Qualifications<br />

M.Sc. in Applied Geology, Anna University, 2012 [First Div]<br />

Pursuing Ph.D. in Geology, Anna University<br />

Title <strong>of</strong> Ph.D. Thesis: Holocene monsoon variability inferred from paleo lake sediments,<br />

Ladakh Himalayas.<br />

Areas <strong>of</strong> research interests:<br />

The study <strong>of</strong> ancient lake deposits has been helped immeasurably by limnologists, sedimentologists, and<br />

geochemists, by making observations on active lakes, Pleistocene lakes and their Holocene residues.<br />

Paleoclimatic information may be contained in the nature <strong>of</strong> the basin itself as well as in the material that filled it.<br />

Every lake deposit is testimony to at least two important environmental changes, one initiating lacustrine<br />

deposition and the other terminating it. Climatic factors may be involved in either or both events. For instance,<br />

glacial lakes <strong>of</strong>ten form during a warming trend, and they can be recognized from the shape <strong>of</strong> the basins and the<br />

fact that many are dammed by moraines. Tectonic events unrelated to overall climatic change may lead to<br />

steepened hydraulic gradients and increased precipitation in the watershed and hence earlier filling <strong>of</strong> the basin.<br />

Filling and choking with sediment probably is the most common death <strong>of</strong> lakes, but lakes can also dry up. In that<br />

case, a clear record is usually left in the sediment in the form <strong>of</strong> an evaporitic terminal stage or by a lake level<br />

marker.<br />

Name BANDANA DIMRI<br />

E-mail Address bandanadimri@gmail.com<br />

Phone/Mobile No. 9456531728<br />

DOB 04/07/1988<br />

Mailing Address <strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong><br />

53 University Road, Lucknow-226007<br />

Name <strong>of</strong> Organisation <strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong>,<br />

Academic Qualifications<br />

M.Sc. in Geology, H.N B Garhwal University Srinagar, 2010 [First Div]<br />

Pursuing Ph.D. BSIP, Lucknow<br />

Title <strong>of</strong> Ph.D. Thesis: Genesis <strong>of</strong> Mesoproterozoic chert facies <strong>of</strong> the Salkhan Limestone, Son<br />

Valley, Vindhyan Supergroup: microbial assemblage and Biostratigraphic implications.<br />

Areas <strong>of</strong> research interests:<br />

The research area <strong>of</strong> interest is the sedimentological and micropaleontological studies backed by a sound<br />

knowledge <strong>of</strong> the various geological processes in relation to the petroleum / fuel industry. Owing to my research<br />

understanding worked on dissertation thesis on the Quaternary deposits during post-graduation studies. An<br />

abstract has published earlier in 2011 entitled “Understanding <strong>of</strong> the Geological Evolution <strong>of</strong> Surat Depression<br />

and Development <strong>of</strong> Hydrocarbon Pools in Contigeous Area”. Presently, engaged in the palaeobiological<br />

investigations and sedimentological studies with special reference to genesis <strong>of</strong> siliceous chert in the Semri Group<br />

<strong>of</strong> rocks in the Son Valley area.<br />

<strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong>, Lucknow<br />

38

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!