Oligocene的意思
Oligocene中文翻譯:
adj.漸漸統的;漸新世的
n.漸漸統;漸新世
Oligocene───n.漸漸統;漸新世;adj.漸漸統的;漸新世的
oligogene───n.少量基因
oligogenes───n.少量基因
Pliocene───adj.上新世的;n.上新世,上新世巖
oligochaete───n.寡毛綱(環節)動物;adj.寡毛綱(環節)動物的
oligoclase───n.[礦物]奧長石,鈉鈣長石
Holocene───adj.全新世的;全新統的
Miocene───adj.第三紀中新世的;n.第三紀中新世;中新世沉積巖
Pleiocene───adj.上新世的
The samples are from Oligocene, Miocene and Pliocene strata.───樣品的地層年代介于漸新世和上新世之間。
Oligocene and the Ulunguhe Fm. Early Eocene to Early Oligocene.───早始新世至早漸新世。
Produced in Asia, Eastern Europe Oligocene .───產于亞洲、歐洲東部漸新統。
any of many extinct cats of the Old and New Worlds having long sword like upper canine teeth; from the Oligocene through the Pleistocene.───東半球許多已經滅絕的貓科動物,其上犬齒形如長劍;生活在從漸新世經由更新世時期。
As in the Oligocene before it, grasslands continued to expand and forests to dwindle in extent.───在先前的漸新世,草地的面積增大,森林的面積減少。
The west side of the lake offers much older fossils from the Miocene, Oligocene and Cretaceous eras (including dinosaur remains).───而盆地西部的化石,年代則更古老,從含有恐龍遺跡的白堊紀,到漸新世與中新世。
Hundred years, Quanzhou experienced many historical changes, the new interactive air-filled history of old customs, culture Oligocene.───百多年來,泉州經歷多次歷史變革,新風舊俗交互遞嬗,風氣漸新。
the Upper Cretaceous was in the higher base level, which developed fan delta- lacustrine facies until late Oligocene.───上白堊統基準面快速抬升,沉積區整體處于湖泊-扇三角洲沉積體系,一直持續到古近系漸新統晚期。
Oligocene erosion had truncated the sediments draped over the dome.───覆蓋于穹丘上的沉積巖為漸新世侵蝕所截削。
Oligocene erosion had truncated the sediments draped over the dome.
In late Eocene - Oligocene, that is red coarse sediment.
The differences between Oligocene series in the east and west are demonstrated.
Venezuela, oil is produced from lenticular sandstone beds of the Oligocene oficina Formation.
The uplifting, right-lateral strike-slip shearing, tilting and southward shearing of the Altai Mountains in Xinjiang have affected, since Oligocene, the drainage systems evolution and development.
There are four hydrocarbon source rocks, Palaeocene, Eocene, Oligocene and Miocene.
Paleogene Oligocene Linhe formation ( E _ 3 J ) and Eocene Wulate formation ( E _ 2 wl ).
It peaked in the Oligocene Epoch around 34 million years ago in Eurasia, and again in the Miocene Epoch about 10 million years ago in Eurasia and Africa.
Eocene through lower Oligocene lacustrine shales and Oligocene through lower Miocene lacustrine and deltaic coaly shales are the mature source rocks.