五臺(tái)山英文導(dǎo)游詞
【篇一：五臺(tái)山英文導(dǎo)游詞】
mount wutai
世界遺產(chǎn)提名地：五臺(tái)山，由兩部分組成：臺(tái)懷核心區(qū)和佛光寺核心區(qū)，核心區(qū)面積18415公頃，緩沖區(qū)42312公頃。
located in wutai county of xinzhou city the northeastern of shanxi province china.
位于中國山西省東北部忻州市五臺(tái)縣境內(nèi)。
is made of the oldest stratum in the world which is more than 2.5 billion years.
由大于25億年的世界古老地層構(gòu)成
it has 5 peaks in north south east west and center, the peak is 3061 meters above a level which is called as “the ridge of northern china”
有東西南北中五座山峰，最高峰3061米，被譽(yù)為“華北屋脊”
the mountaintops are flat and wide commonly known as platform, so it was called the five flat-top mountains. 五座山峰頂部平坦寬廣，俗稱臺(tái)頂，因此得名五臺(tái)山。
mount wutai has a magnificent natural landscape and a rich geological heritage,
五臺(tái)山自然景觀奇?zhèn)ス妍悾刭|(zhì)遺產(chǎn)豐富
its unique palaeotectonic relics, rare periglacial and glacier land form,
其獨(dú)特的古地質(zhì)構(gòu)造遺跡，稀有的冰原冰川地貌景觀
and valuable species and ecological resources,
珍貴物種和生態(tài)資源
rves as a typical evidence of an important period in the history of earth evolution.
使其成為代表地球演變史重要階段的典型例證
the age of various rock units of granite and greenstone belts in mount wutai is around 2.6 to 2.5 billion years, 五臺(tái)山花崗巖~綠巖帶的年齡在26至25億年
and it’s expod in the great height difference of the new generation of mountains and valleys,
并且出露于高差巨大的新生代山脈和山谷內(nèi)
various levels of rocks expod to surface.
各種層次巖石組成良好出露地表
and it has time continuity and irreplaceability in geological time.
在地質(zhì)時(shí)代上具有時(shí)間的連續(xù)性和不可替代性
the displayed rich geological phenomenon is irreplaceability in the world.
所展示的豐富地質(zhì)現(xiàn)象在世界范圍內(nèi)也具有不可替代性
campared with tho well known mountains around the world its long history of geological evolution is very rare, 其漫長(zhǎng)的地質(zhì)演化史在世界著名山峰中非常罕見
and it became field visit location in many international geological conferences and is the classic geological rearch area in china.
成為多次地質(zhì)會(huì)議的考察地及中國經(jīng)典的地質(zhì)研究地區(qū)
the granite-greenstone belt of mount wutai also led to the formation of typical neoarchean collision orogenic belts,
五臺(tái)山花崗巖~綠巖帶構(gòu)成典型的新太古代碰撞造山帶
it fully revealing the early collision orogen structure ctionand different levels of crustal,
完整展示出早期碰撞造山帶構(gòu)造剖面及不同地殼層次
and has typical geological evolution significance.
具有典型的地質(zhì)演化意義
therefore ,mount wutai is key evidence for studies of the archean plate tectonics and the collision orogenic belts. 是研究太古宙板塊構(gòu)造與碰撞造山帶的關(guān)鍵例證
the geochronological boundary of the archean and proterozoic eons, is considered as the most important geological events in tectonic evolution.
太古宙到遠(yuǎn)古宙界限被認(rèn)為是地殼演化史上最重要的地質(zhì)事件
during this period, the earth has undergone profound changes.
地球在這一時(shí)期發(fā)生了深刻變化
international commission on stratigraphy propos that the line of demarcation be drawn at 2.5 billion years ago. 國際地層委員會(huì)建議這一界限年代應(yīng)劃分在25億年前
mount wutai rerve many unconformities interface before and after 2.5 billion years,
五臺(tái)山保留有多個(gè)25億年前后的不整個(gè)界面
and has clear lines of demarcation between different stages of geological evolution,
具有明顯的地質(zhì)演化階段性
it’s also involving the radical environmental changes of continental extensions after the end of the collision orogeny(2.5billion years).
涉及典型板塊碰撞造山結(jié)束，向板內(nèi)伸展環(huán)境的劇烈變化
they provide sound conditions for tting off the boundaries of the archean and proterozoic eons,
非常有利于劃分太古宙~遠(yuǎn)古宙界限
and is typical area for establishing the archean proterozoic boundary before 2.5 billion years.
是建立太古宙~遠(yuǎn)古宙界限的典型地區(qū)
it’s also bearing comparable value to universal geological studies.
具有全球地質(zhì)對(duì)比價(jià)值
mount wutai keeps a complete records of the paleoproterozoic strata before 2.5-1.9 billion years,
五臺(tái)山保留完整的古元古代地層記錄（2.5~1.9億年）
there are well-prerved early weathering crusts, ancient red bed as well as rich records of stromatolites in the stratigraphic ctions.
地層剖面保留了早期古風(fēng)化殼、古紅層及異常豐富的疊層石記錄
there is a rich rerve of paleofloral fossils in the doucun subgroup of mount wutai,
五臺(tái)山豆村帶群中發(fā)現(xiàn)了豐富的古植物化石
and they are the earliest china’s eukaryotic organisms before 2.4 billion years,
并有中國已知最古老的真殼生物化石（24億年前）
it’s 600-700 million years earlier than the previously acclaimed oldest eukaryotic fossil record.
比先前認(rèn)為的最古老真殼生物化石記錄早6至7億年
in this regard mount wutai is valuable to the understanding of earlier evolution of life.
對(duì)認(rèn)識(shí)早期生命演化具有重要價(jià)值
compared with other ancient planation surfaces of east asia,
與東亞其他古夷體面相比
mount wutai is a typhical example of the cenozoic continental extension and of the fault block orogeny. 五臺(tái)山為早期寒武紀(jì)地殼中新生代伸展、斷塊造山活動(dòng)的典型代表
