Paleocene信息详情
n.古新世
cageling palette───笼式调色板
pale moon───苍白的月亮
paleolithic cave painting───旧石器岩画
palea kameni───棕榈石
trowel palette knife───泥刀
alarmingly pale───苍白得吓人
paleontologist costume───古生物学家服装
pale skin───苍白的皮肤
pale faced───面色苍白；白人
palestra───n.(Palestra)人名；(意、塞)帕莱斯特拉；n.摔角场，角力场；体育学校
During Late Paleocene there were two greater transgressions in the sag.───晚古新世丽水凹陷经历了两次较大规模的海侵。
There he developed the experience and expertise that led to parallel exploration of the Paleocene in China.───在那里，他积累了专业知识和经验，并促成了对中国古新统进行的类似考察。
Their ages may be early Late Cretaceous and Late Cretaceous-Paleocene.───它们分属于晚白垩世早期、晚白垩世—古新世。
The Paleocene epoch was a time of dense forests and evolutionary experiments.───古新世可以说是一个丛林茂密演化不断的时代。
During the Paleocene the island continent of India moved north and collided with Asia.───在古新世，印度这个大陆岛继续向北移动与亚洲版块相撞。
The Paleocene epoch, 63 millions ago, is a crucial time in the history of mammals, it was a world without dinosaurs.───古新的世纪，63成千上万前，是关键的时光在哺乳动物的历史上，它是一个世界没有恐。
Petroleum Prospects of Mesozoic and Paleocene in the Western Depression of the East China Sea Shelf Basin───东海陆架盆地西部坳陷带的中生界和古新统油气远景
Paleocene depositional environment and coal bearing characteristics of Jidong basin, Heilongjiang───黑龙江省鸡东盆地下第三系沉积环境及聚煤特征
A study on characteristics of the Late Cretaceous-Paleocene structures in Jiuquan Basin───酒泉盆地晚白垩世-古新世构造特征
Paleocene - Eocene terrigenous deposits, deposited in grabens and half-grabens, constituted the lower tectonic layer of the sedimentary basins of South China Sea.
From late Cretaceous to Paleocene, it is the time of basin extruding, uplifting and denudation, therefore a larger angular unconformity formed between Mesozoic and Cenozoic.
From Cretaceous Period to Paleocene Eocene, subsidence and sedimentation area migrated gradually towards inside basin because the major thrust belts were piggyback and developed towards inside basin.
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Paleocene The oldest epoch of the Tertiary, 65 - 55 million yesrs ago.
During the Paleocene there was a great deal of coevolution of plants and animals , the plants evolving adaptations to animal pollination and fruit and seed dispersal.
The boundaries between the Upper Cretaceous and Paleogene, Paleocene and Eocene, and Eocene and Oligocene in China nearly accord with corresponding ones elsewhere in the world.
The Paleocene epoch was a time of dense forests and evolutionary experiments.
The middle Jurassic Yeba formation volcanics, Paleocene biotite granite porphyry, Miocene quartz monzonite and Oligocene granite porphyry could be found in the ore field.