Silurian

音標(biāo)發(fā)音

But as the ecosystem recovered after the freeze, it expanded, with land plants becoming common over the course of the Silurian period.
但在冰封之后，隨著生態(tài)系統(tǒng)的復(fù)原，其范圍也隨之?dāng)U大，其結(jié)果是在Silurian期陸生植物變得更為普遍。
The third largest extinction in Earth's history, the Ordovician-Silurian mass extinction had two peak dying times separated by hundreds of thousands of years.
作為地球史上消亡物種排行第三的大滅絕，奧陶系-志留紀(jì)大滅絕有兩個(gè)死亡高峰期，其中相隔數(shù)十萬(wàn)年時(shí)間。
The earliest of the Big Five, the end-Ordovician or Ordovician-Silurian extinction events some 444 million years ago, are reckoned by many to be the second largest.
五次大滅絕中發(fā)生最早的一次是奧陶紀(jì)末期或者奧陶紀(jì)-志留紀(jì)大滅絕事件，發(fā)生在大約4億4千4百萬(wàn)年前。許多科學(xué)家估計(jì)這次規(guī)模是五次當(dāng)中第二大的。

from or referring to the period of time between about 445 and 420 million years ago, in which fish with jaws (= mouth bones) and some plants and small animals on land first appeared

of, denoting, or formed in the third period of the Palaeozoic era, between the Ordovician and Devonian periods, which lasted for 25 million years, during which fishes first appeared 2500
the Silurian period or rock system

志留系
The Silurian was mainly medium sand, fine sand, siltstone and pelitic siltstone in shallow sea.
志留系沉積以濱淺海的中細(xì)砂巖、粉砂巖及泥質(zhì)粉砂巖為主。
志留紀(jì)

志留系
Acidizing treatments in TaZhong(TZ)12 Silurian sandstone formation had achieved little effect and should be improved for inadequate understanding on the damage and inappropriate acid system.
塔中(TZ)12油田志留系砂巖儲(chǔ)層在以往酸化改造現(xiàn)場(chǎng)實(shí)踐中，由于對(duì)儲(chǔ)層傷害認(rèn)識(shí)不夠深入，酸液類(lèi)型和配方針對(duì)性不強(qiáng)，酸化有效率和增產(chǎn)率有待進(jìn)一步提高。
志留紀(jì)