A group led by British sedimentologist Paul Wignall of the University of Leeds writes about
examining rocks cored from basin sediments 600 miles south of Bedout.
Not exact matches
As each cylinder of
rock comes up from the deep, onboard specialists rush to record its density, resistivity, temperature and any other data that might change before the
cores are
examined at a main lab in Bremen, Germany.
Initially, they hoped to generate interest in geology and acquire some
rock cores for students to
examine in class.
Then he
examined layers of sediment in these deep
cores, using a suite of techniques to calculate the age of the sand, other
rocks, and organic matter in each layer.