早第三纪

Thereafter, due to a large number of ancient human fossils found in the material, some people think that the human and ape in the new Middle and Late Miocene Tertiary (180-600 million years ago) started to divide the community a few years Dryopithecus health of various species are the ancestors of monkeys, a species which evolved into the first person Branch representatives - Ramapithecus later evolved from the Ramapithecus dating back 200 million years ago, Australopithecus, and then through the Homo erectus, early Homo sapiens, late Homo sapiens (M. Krume farmer) and evolved into modern man.

此后，由于大量古人类化石材料的发现，部分人认为人和猿是在新第三纪的中新世中晚期（距今180—600万年间）开始分化的，森林古猿里的几个种是各种现生猿的祖先，其中有一个种进化成最早的人科代表——腊玛古猿，以后由腊玛古猿进化成距今200万年前的南方古猿，再经过直立人、早期智人、晚期智人而进化成现代人。

Influenced by tectonic movement, there were no sediments in the area from Oligocene to Miocene. Appearance of marlite in the Pliocene, especially in Yaqueling region, proved localized depositing environment forming, for which there had only few amount of terrigenous matters to supply. Sedimentary facies association of alluvial fan, fan delta and inland lake appeared at the early and middle stage of lower Pleistocene, and association of fan delta and inland lake appeared at the later stage of lower Pleistocene and the early stage of middle Pleistocene. Net-veined laterite appeared at the top of lacustrine deposit, which reflected pedogenesis taking place after the end of deposition. Such evolution history proves that there had no lager river system traversing this area before the early stage of middle Pleistocene.

对于江汉盆地西缘宜昌地区来说，其沉积及古地理演化表现为：早白垩世为受天阳坪断裂控制的内陆湖泊沉积环境，沉积中心在天阳坪断裂的北侧，此时几乎不存在来自黄陵地区的水系；晚白垩世同样为受断裂控制的内陆湖盆环境，但湖盆面积扩大、断裂活动减弱，且后期出现成化湖相沉积；第三纪早期盆地由断陷盆地转变为坳陷盆地，同时石膏的出现代表了局限咸化湖盆的存在；渐新世—中新世，受构造影响，缺失该时期的沉积；上新世时在鸦鹊岭一带出现的泥灰岩沉积反映了陆源物质供应不足的局限沉积环境的存在；早更新世早中期为冲积扇—扇三角洲—内陆湖泊沉积，早更新世晚期—中更新世早期为扇三角洲—湖相沉积，后期出现沉积结束以后的网纹红土化作用。

In view of the mapping relationship between expulsion time and formation time of structure traps, the expulsion time of Niuerduan may be too early because basin structure figured in Neogene Period.

由于盆地的构造格局定型于新第三纪以后，因此从排烃期与构造圈闭形成期之间的匹配关系考虑，牛二段的排油偏早。

In this article the research of pinaceous fossil cones from the Creaceous to the Oligocene in the Tertiary is reviewed and summarized systematically.

本文主要对早白垩世到老第三纪渐新世这段时间的松科化石球果的研究作了系统回顾和总结。

These stages can be generalized into four cycles: 1 lower Cretaceous to lower Eocene; 2 middle Eocene to Oligocene; 3 Oligocene to Neocene; 4 Quaternary.

从而可以划分出四个构造旋回：1早白垩世—早始新世；2中始新世—渐新世；3渐新世—晚第三纪；4第四纪。

Little of the soil composition of planet Earth is older than Tertiary and most no older than Pleistocene.

地球上只有很少的土壤成分的生成年代早于第三纪（直译：很少的土壤成分的年龄超过第三纪），大多数不会早于更新世

The water depth had increased since Late Te r tiary and reached to high stand in Early and Middle Pliocene (outer neritic to b athyal environment), and then decreased.

研究认为崖19-1-1井晚第三纪以来古水深变化的总趋势为逐渐增大，至上新世早中期出现外浅海至半深海环境，为古水深最大时期，随后水深则逐渐减小。

Petroleum systems in half-grabens extend along the slope, while petroleum systems in grabens are basically restricted between two boundary faults or extend slightly.

盆地早第三纪经历了3个裂陷期，均发育有烃源岩、储层和局部盖层，形成的含油气系统存在着依次改造相互叠加组合的关系。

According to geologists' textual research,the volcanic eruption in Qiongbei started from early Tertiary period of Kainozoic era ,and ended in the Holocene of Quaternary period,about 13 thousand years ago.

据地质学家考证，琼北火山喷发于新生代早第三纪，最后一次喷发是第四纪全新世，距今约1万3千年前。

By means of the principle,method and technology of sequence stratigraphy,The dynamic characteristics of filling and evolution of Huangxian Eogene fault basin are studied,based on the classification of high frequency sequences.

运用层序地层学原理和方法，在黄县盆地进行高频层序地层划分的基础上，对黄县早第三纪断陷盆地充填演化的动力学特征进行研究。

But we don't care about Battlegrounds.

但我们并不在乎沙场中的显露。

Ah! don't mention it, the butcher's shop is a horror.

啊！不用提了。提到肉，真是糟透了。