早寒武世 的英文怎麼說
中文拼音 [zǎohánwǔshì]
早寒武世
英文
lower cambrian-
Early cambrian anoxic event sedimentation in guizhou province
貴州早寒武世的缺氧事件沉積2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation
塔中隆起源於早古生代拉張背景下的正斷層，寒武-奧陶紀為其烴源巖形成的重要時期；早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期，同時也為志留系形成地層及復合圈閉提供了古地理背景；志留?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆紀末塔中鼻狀隆起基本定型，古油藏遭受破壞，形成了瀝青砂巖；早二疊世晚期的構造變形使古油藏遭受進一步的破壞；二疊紀后構造變動主要以調節為主。Early cambrian sponge spicule fossils from zhenba county, southern shaanxi province
陜西鎮巴早寒武世海綿骨針化石Helcionelloid mollusk from the lower cambrian heilinpu formation, chengjiang, yunnan
雲南澄江早寒武世黑林鋪組軟體動物太陽女神螺From the cambrian to the early middle ordovician, the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm, and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province, while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province
在寒武紀至中奧陶世早期，東秦嶺北部二郎坪海槽的寒武紀放射蟲和早奧陶世牙形石與東秦嶺南部浙川陸棚北部的寒武紀三葉蟲、早奧陶世牙形石和頭足類屬華南生物省，而浙川陸棚南部的寒武紀三葉蟲和早奧陶世牙形石屬于華南生物省，兼有華北生物省分子。All these ductile shear zones are characterized by northward thrusting. the u - pb dating on zircons from the bedded gabbro of the qimanyuter ophiolite melange gives an age of 526 ? 1 ma ( early cambrian )
在其曼于特蛇綠巖的層狀細粒輝長巖中獲得了鋯石u - pb年齡值為526 1ma （早寒武世） ，它被晚奧陶世花崗巖侵入。Of which 4 new genera and 4 new species are established. discovery of a lot of fossil worms with their traces provide direct clues to study on the locomotion style of the worm and indirect evidences for trace fossils to find their producer
在以上屬種中發現大量的蟲、跡同在的化石，為研究早寒武世的翻吻動物的運動方式以及遺跡化石提供了直接依據。In fact, over 300 million years earlier than the world of dinosaur ( dated back to 500 million years ), earth had witnessed the first era of colorful life world ? cambrian period
《侏羅紀公園》重現了1億多年前的侏羅紀夢幻般的恐龍世界，其實，早在恐龍世界之前3億多年（距今約5億多年） ，地球生命就已經開辟了多彩多姿的生命世界第一個紀元? ?寒武紀。Restudy on the eodiscoids from the shuijingtuo formation early cambrian in eastern yangtze gorge area, western hubei
峽東地區早寒武世水井沱組古盤蟲類三葉蟲的再研究5 ) the lophophores at trocholophe stage in heliomedusa orienta are tentatively interpreted here. 6 ) the mineralization of the animal took place gradually from outside to inside during their preservation before the fresh carcass were broken down, which could have given access to the preservation of the softy anatomy of organisms in chengjiang fauna
第五章基於澄江動物群中的腕足動物化石，對腕足動物的演化做了初步的探討，認為腕足動物在早寒武世己經出現了大量的分異，其形態己經相當進化。The middle cambrian early devonian ( 513 - 397ma ) tectonic stage was characterized by a series of tectonic events with different features, which are completely different from the caledonian event that occurred in the appalachian orogen and in scotland
摘要中國大陸早古生代（中寒武世早泥盆世）構造期以發生系列各具特徵、分佈局限、準同時的構造事件為特徵。Now it is thought that two formations were formed in the same period from early cambrian to early ordovician and were deposited in different parts of sea basin on the northern edge of the north china platform, based on the acritarchs contained in these formations
通過對以上兩個組中疑源類化石進行研究，認為阿牙登組應從白雲鄂博群中分出，與腮林忽洞組一同劃歸早寒武世至早奧陶世的地層中，阿牙登組與腮林忽洞組為同一時期不同局限海盆的沉積，是早古生代華北地臺最北部邊緣的沉積產物。Geochemical characteristics and petrogenesis of neoproterozoic - early cambrian volcanic rocks in tianshan area
早寒武世火山巖地球化學和巖石成因Geochemical research on tectonic environment of early cambrian granites in the huzhong area of heilongjiang province
黑龍江省呼中地區早寒武世花崗巖構造環境的地球化學研究Geochemical constraint on the origin and sources of early - middle cambrain acidic volcanic rocks from baiyin ore deposit
甘肅白銀廠礦田早中寒武世酸性火山巖成因及源區特徵的地球化學制約The major lithofacies palaeogeographic characteristics of the qiongzhusi age and early canglangpu age ( early cambrian ) are a land in middle hubei, the carbonate tidal flat surrounding the land, shelf and a basin in the south
早寒武世早中期巖相古地理格局由鄂中古陸、圍繞古陸的碳酸鹽潮坪、陸棚及南邊的陸棚邊緣盆地組成。The geological setting of chengjiang biota firstly, the pattern of chinese tectonic has been cited, which can help us to understand the place of china in the world clearly and easily. secondly, the lower cambrian of china and the early cambrian geomorph of eastern yunnan have been included
澄江生物群的地質構造背景首先介紹了中國區域大地構造格局，其次是關于中國的寒武系和滇東地區早寒武世古地理概貌的論述，緊接著是澄江化石庫的古地理概貌。This paper is a continuation of the papers on lithofacies palaeogeography of the early, middle and late cambrian and the early and middle ordovician
摘要本文是筆者等的中國早、中、晚寒武世和早、中奧陶世巖相古地理諸文的繼續。The land disappeared during the late canglangpu age and longwangmiao age ( early cambrian ) and the framework of palaeogeography consisted of tidal flat, open carbonate platform, platform - margin slopes and basin in the south
早寒蟬寒武世中晚期巖相古地理格局由碳酸鹽潮坪、開闊臺地、臺緣斜坡和臺緣盆地組成，該地區主體進入碳酸鹽臺地演化階段。Phosphate deposits are distributed along the margin, platform and basin in the west yangtze area. the analysis methods include the paleogeography, petrology, organic geochemistry, geochemistry. the conclusions are drawn that the source of phosphate deposits distributed along the margin originate from the weathering production of continent, while phosphate deposits along the platform and basin gain phosphorus through hot spring on the buttom of the sea floor, which is brought to the sedimentary environment by rising sea - fluid, then accumulated by the organism and microorganism, meanwhile, basin phosphorite keep relatively higher organic carbon content
認為早寒武世早期古陸遭受風化，被剝蝕下來的產物成為潮坪型磷塊巖的主要磷質來源，在碳酸鹽巖臺地發生的熱點活動和上升洋流從盆底深部帶來的磷質，共同作為臺地型磷塊巖的磷源，盆地型磷塊巖的磷質同樣是由熱點活動和上升流攜帶至缺氧的沉積環境中，通過藻類或微生物的富集作用成巖，並保留了較高的有機碳含量。分享友人