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alumni reception - Syracuse Universe Department of Earth Sciences ...

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ealize they do not know as much as they thought<br />

they did, and I was no different. After was all said<br />

and done, I passed, and came away with a much more<br />

focused idea <strong>of</strong> what I need to do to accomplish my<br />

research goals.<br />

Once my exam was over I traveled to the<br />

University <strong>of</strong> Arizona to analyze U-Pb in detrital<br />

zircons as part <strong>of</strong> a collaboration between SU and the<br />

USGS. The rock samples were collected from Vermont<br />

to Virginia. The trip was a huge success, and has<br />

started to give my collaborators and me much insight<br />

into where Cambrian sedimentary rocks along this<br />

part <strong>of</strong> eastern North America originated. This project<br />

is still ongoing, as I hope to analyze several thousand<br />

more zircons, this time from Virginia to Missouri.<br />

Combined with the previous data, the new study will<br />

give us a picture <strong>of</strong> how the entire eastern part <strong>of</strong><br />

North America formed in the early Cambrian.<br />

Finally, I would like to thank the department for<br />

recognizing my efforts with several awards: a Student<br />

Publication award for my paper in the Journal <strong>of</strong><br />

was a very busy year for me. In addition to serving as<br />

Head ta for the department, I also made considerable<br />

My exploration and field work in Iceland.<br />

Sampling ancient gneiss in the Minnesota River Valley.<br />

Geology and the Newton C. Chute award for my<br />

service to the department and pr<strong>of</strong>essional promise. I<br />

would also like to thank donors to the John J. Prucha<br />

field fund for awarding me money to collect ~1 billion<br />

year old rock samples along the eastern US. By<br />

collecting and analyzing these rocks I hope to learn<br />

more about potential sources to the Cambrian rocks<br />

mentioned above, and gain a better understanding <strong>of</strong><br />

how the eastern US might have looked approximately<br />

500 million years ago.<br />

Drew Siler<br />

I’m starting the fifth year <strong>of</strong> my dissertation<br />

research at <strong>Syracuse</strong> in the Fall <strong>of</strong> 2010. Last year<br />

progress on my research. In addition to presenting a<br />

poster at AGU in December, I published my first, firstauthored<br />

publication with my advisor Jeff Karson.<br />

I also went to the SIMS lab at UCLA and collected<br />

the last <strong>of</strong> my data, U/Pb in zircon geochronology<br />

data from Icelandic rhyolites. In May, I attended the<br />

ExxonMobil Big Horn Basin Field Trip, where we<br />

learned the basics <strong>of</strong> petroleum geology and play<br />

elements. This summer I am an intern at Chevron in<br />

Houston, TX, working in a reservoir management<br />

team on an oil field <strong>of</strong>f the coast <strong>of</strong> Angola. I plan to<br />

finish my research and defend my dissertation in the<br />

Spring <strong>of</strong> 2011.<br />

Tonny Sserubiri<br />

It has been a great first year for me at the<br />

Heroy Geology Laboratory with lots <strong>of</strong> new things to<br />

marvel at. I’m thankful to the various Pr<strong>of</strong>essors at<br />

the <strong>Department</strong>, especially my advisor Chris Scholz<br />

and graduate students who have made my stay here<br />

memorable.<br />

Having completed my first year <strong>of</strong> Graduate<br />

School, my current focus is my Master’s thesis, which<br />

will comprise various sedimentological aspects,<br />

ranging from seismic data analysis and interpretation,

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