「Cenozoic」の共起表現一覧(1語右で並び替え)
該当件数 : 31件
Cenozoic activity was mainly in the form of isolated b | |
esozoic, the age of reptiles, and the current | Cenozoic age of mammals. |
en displaced about 600 km northward since the | Cenozoic along the Queen Charlotte-Fairweather fault s |
umber of times in different groups during the | Cenozoic, and in each instance was immediately followe |
He has also worked extensively on | Cenozoic bryozoans in England and southern Scandinavia |
matics and morphometrics of late Mesozoic and | Cenozoic bryozoans found in deposits located in the Ca |
Early | Cenozoic Carnivora ("Miacoidea"). |
ize each island in turn, a process aided by a | Cenozoic climate allowing it to live at lower altitude |
nd was therefore a major causal factor in the | Cenozoic Cooling trend that eventually led to our most |
Upper Rhine Plain was formed during the Early | Cenozoic era, during the Late Eocene epoch. |
The last period of the | Cenozoic era, known as the Pleistocene period, is some |
contributed greatly to the coal swamps of the | Cenozoic era. |
untains and the Diablo Range during the later | Cenozoic era. |
he smallest mammals of either the Mesozoic or | Cenozoic eras. |
hys Ocean during the middle Mesozoic to early | Cenozoic eras. |
the middle portion of the Cretaceous and the | Cenozoic, especially with respect to terrestrial ecosy |
Late Cretaceous and | Cenozoic Mammals of North America: Biostratigraphy and |
lly the Paleocene-Eocene transition and early | Cenozoic mammals. |
On the Mesozoic and | Cenozoic Paleontology of California. |
Cenozoic Plants and Climates of the Arctic (Nato a S I | |
titution, located in Beijing, grew out of the | Cenozoic Research Laboratory in 1929 and is its own in |
Davidson Black founds the | Cenozoic Research Laboratory for the research and appr |
They jointly produced a schema of New Zealand | Cenozoic rocks that survives to the present almost wit |
alaeozoic meta-sedimentary rocks, Mesozoic to | Cenozoic sedimentary rocks and superficial deposits. |
veld complex) they may be any age such as the | Cenozoic Skaergaard intrusion of east Greenland. |
The | Cenozoic uplift and earthquake belt of mainland Britai |
In the | Cenozoic, uplifting and westward tilting of the Sierra |
vers an area of 5000 km² with nearly 700 late | Cenozoic vents. |
The | Cenozoic was studied and further determined by, among |
e mountains themselves did not form until the | Cenozoic, when immense forces between the colliding Af |
the Permian and Triassic and again during the | Cenozoic with a sinistral strike-slip sense. |
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