Archeologist Richard Hansen has worked for more than 20 years to solve the enigma of the early Maya.

My father was an archeologist and so we were...

我的父亲是一位考古学家，因此我们…

On graduation from Oxford, he went to the Middle East as an archeologist and to learn Arabic.

从牛津大学毕业后，他到了中东，作为一个考古学家，并在那学习阿拉伯文。

Pretend you are a detective or archeologist, tell us what you can reconstruct about the culture from the object.

假设你是个侦探或是考古学家，告诉我们你将怎样通过这些物品重建当时的文化？

big hole back here and a little patch of hair, and my, son ofthe archeologist immediately went WOW.

后面有个大洞，这里有一小块头发，而我，身为考古学家的儿子，开始大喊大叫。

The archeologist said that the pyramids are the remnants of an alien civilization.

里边的考古学家说这些金字塔是一种地域外文明的遗迹。

I don't see how. I'm an archeologist.

我不知道怎么帮，我是个考古学家。

A local archeologist called the pyramid's destruction an incredible display of ignorance.

一位当地的考古学家称金字塔的毁灭令人无知的难以置信。

A British archeologist who has spent many years trying to convince people that Atlantis could have existed.

他是一位英国考古学家，他已经花费了很多年时间试图让人们相信亚特兰蒂斯很可能是存在的。

He was, in many ways, a music archeologist.

他在很多方面，是一个音乐考古学家。

The crustal evolution in Liaoning Province has undergone multiple stages, in which the basement was formed in Archeozoic-Paleoproterozoic Era, platform cover was developed in Mesoproterozoic-Middle Triassic, and platform was mobiled of after Middle Triassic. The Nos.

辽宁省地壳演化经历了太古宙古元古代基底形成、中元古代中三叠世地台盖层发展、中三叠世以后地台活化等发展阶段。

Based on a study of six garnet samples from Archeozoic metamorphic rocks in Inner Mongolia, this paper discusses the relationship of crystal shape, physical properties, chemical composition of garnets and components of the rocks to spectroscopy as well as the formation condition of garnets.

本文对内蒙古南部太古宙集宁群变质岩系中6个石榴石样品进行了研究，讨论了晶体形态、物理性质、化学成分与岩石成分和波谱学之间的关系。

From Paleoproterozoic Era to late Archeozoic Erathem, it was formed metamorphic complex after deformation and metamorphism from solid liquid facies to soft liquid facies, and it was formed epimetamorphic clastic rock and carbonate rock at Mesoproterozoic-Neoproterozoic Erathem.

古元古晚太古界经历了固流相柔流相变形变质作用后形成变质杂岩（包括表壳岩和变质侵入岩），中新元古界为浅变质碎屑岩和碳酸盐岩。

From the New Archeozoic era to the Cenozoic era, the structural framework in Qinling significantly changed many times. The total evolution can be distinguished to five dominant stages: 1. The forming period of crystalline basement ( Ars-Pt1);

自新太古代以来，秦岭基本构造格局发生过多次重大变革，其演化可划分为5个重要阶段，即：（1）结晶基底形成阶段（Ar3－Pt1）；

Long geological evaluation and Cenozoic structural and fault activities led to the formation of multiple types of oil and gas pools from Neogene to Archeozoic Era and resulted in a great deal of oil and gas accumulations in uplifts and sags.

漫长的地质演化和新生代构造断裂活动形成了上第三系至太古界多层系多类型的油气藏，在凹陷、凸起的各部位，分布着大型油气聚集带。

The recent geologic data show that it is the Archeozoic high-grade metamorphic terrain formed by the supracrustal rock-TTG rock series, that is different with the southern Longgang landmass.

新近调查资料表明，它是由表壳岩-TTG岩系组成的一太古宙高级变质地体，并有别于南侧之龙岗陆块。

There is obviously fault contact between the cap rock and Archeozoic rock basement, associated with basic magma intrusion and with the characteristics of the back margin tensile of d é collement structure.

盖层与太古代基底之间存在明显的断层接触，并伴随基性岩浆侵入活动，具有滑脱构造后缘拉伸带的特征。

The great majority of gold deposits in North China platform are hosted by the Archeozoic strata or emplaced in the Yanshanian magmatic intrusives of the Archeozoic strata.

华北地台中绝大多数金矿赋存于太古宙地层或侵入于太古宙地层中之燕山期岩浆岩体内。

China's Archeozoic Terrane, mainly a granite-greenstone belt, a small part of which been metamorphosed at a high grade, is basically located in North China Platform distributive area.

中国太古宙地体基本上分布在华北地台范围内，主要为花岗岩绿岩带.少部分为高级变质带。

Massive sulfide Cu-Zn deposit of Hongtoushan type which occurs in Archeozoic granitic greenstone terrain in Qinyuan area of Liaoning possesses unique geochemical characteristics.

产于辽宁省清原地区太古宙花岗-绿岩地体中的红透山式块状硫化物铜锌矿床，具有独特的地球化学特征。

On such a basis, the shape and depth of the magnetic body below the Junggar basin were modeled by using the magnetization intensity of Archeozoic rocks from North China.

利用小波变换技术对航磁异常进行了分离，并在此基础上利用华北地台太古代陆壳的磁化强度值模拟了位于地壳深部的古老结晶基底的形态与产状。