Palaeocene


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Palaeocene

(ˈpælɪəʊˌsiːn)
adj
(Palaeontology) of, denoting, or formed in the first epoch of the Tertiary period, which lasted for 10 million years
n
(Palaeontology) the Palaeocene the Palaeocene epoch or rock series
[C19: from French from paléo- palaeo- + Greek kainos new, recent]
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014
References in periodicals archive ?
However, unlike the Bara Thrust, the Shin Qamar Thrust carries Palaeocene units as well as the Murree Formation in its hangingwall with the original unconformable contact being the Palaeocene and the Miocene being intact.
We prefer to use the name Pishin Belt, as it also comprises sedimentary successions of shallow marine carbonates, as well as flysch and mollase-type sediments that range from Late Palaeocene to Holocene.
The Samana Block is part of the Outer Lesser Himalayas, and comprises carbonate-dominated Jurassic-Upper Palaeocene lithologies.
The newly-identified species of penguins is believed to have grown this big because they rapidly evolved evolved in the Palaeocene epoch after the dinosaurs vanished on Earth and large marine reptiles disappeared from the southern hemisphere waters.
The earlier 16/1-6 S Verdandi oil and gas discovery, which was made in the same licence in 2003, was in the Heimdal formation in the Palaeocene and in the Grid formation in the Eocene.
There was a widespread volcanic activity at the end of Cretaceous/early Palaeocene time which formed the Deccan Plateau.
A team of geologists from the Jai Narayan Vyas University, Jodhpur discovered a cluster of trace fossils of aquatic insect mayfly in Rajasthan's Barmer believed to be from Palaeocene age, which is from 63 million to 58 million years ago.
Salem et al., "Diagenesis and reservoir quality evolution of palaeocene deep-water, marine sandstones, the shetland-faroes Basin, British continental shelf," Marine & Petroleum Geology, vol.
Named Kumimanu biceae, it lived during the late Palaeocene epoch.
Production commenced in September 2007 from a Tertiary Palaeocene Forties sands reservoir with a structural closure.
It concentrates mainly on the Maastrichtian (latest Cretaceous) Qahlah and Simsima Formations and the overlying Palaeocene Muthaymimah Formation at Jebels Rawdah, Buhays and Faiyah (Figs.