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Mesozoic相关的网络例句

查询词典 Mesozoic

与 Mesozoic 相关的网络例句 [注:此内容来源于网络,仅供参考]

Geothermal gradients of the basins in the eastern of Algin Rift were higher than those of the basins in western of Algin Rift in Late Mesozoic,and tectonic activities were stronger,indicating a strong regional tectonic thermal event.The basins on the western of Algin Rift were all compressive depressions,their geothermal gradients were lower.

中生代晚期阿尔金断裂以东沉积盆地地温梯度普遍高于阿尔金断裂以西沉积盆地,构造活动性强,强烈的构造运动引发了岩浆活动及地壳深部热活动,表明存在一期强烈的具有区域规模的构造热事件;阿尔金断裂以西为挤压坳陷型盆地,地温梯度普遍较低。

Photo Gallery: Jurassic Period An Allosaurus tramps through a Mesozoic-era forest in this artist's depiction.

一只古生异龙践踏通过一个中生代时期的森林在这方面艺术家的写照。

We also analyzed the leg bone proportions of 14 species of Mesozoic birds from the Early Cretaceous of China by using ternary diagrams and comparison with 21 specimens of Cenozoic birds, and concluded that the Early Cretaceous enantiornithines are typical arboreal birds, more basal birds from the Mesozoic are mainly arboreal with some adapted for scansorial life, and the ornithurines are characterized by both arboreal and terrestrial adaptations.

在此基础上,对中国中生代14例鸟类的栖息习性进行了分析,利用三元投影的统计方法,并以国内外新生代21例鸟类标本作为对比参考,得出辽西中生代不同类型鸟类的栖息行为特征:基干鸟类以树栖为主要习性,其中个别鸟类还具有攀援的习性,而反鸟类则是典型的树栖鸟类,今鸟类兼有树、地栖的习性。

The Mesozoic strata outcropped in the central-east part of Guangdong Province may divided into 15 of Ⅲ rank sedimentary sequences, while there are 12 of Ⅲ rank sequences of Mesozoic identified in the seismic profiles and well LF35-1-1 in offshore Chaoshan depression in the north margin of South China Sea.

南海北部陆缘陆上粤中-粤东地区出露一系列的中生界,可以划分为15个Ⅲ级沉积层序。在毗邻海区的潮汕坳陷的地震剖面和LF35-1-1井也可以识别出12个Ⅲ级沉积层序。

Early Mesozoic: The accretion of thickness of continental lithosphere in eastern part of North China block took place because Yangzi block subducted beneath North China block in NW direction in early Mesozoic.

中生代早期:因扬子地块向北西方向俯冲,造成了华北地块东部大陆岩石圈曾存在一次重要的加厚过程,随之而来的是俯冲板片的断离和岩石圈根的拆沉。

In existing ich-nofacies model trace-making courses with ulti-stages and ulti-tiering are not stressed. Existing ichno-tiering models are based mainly on the Mesozoic-Cenozoic data. The reported data show that tiering distributions of Chondrites are different in Palaeozoic and Mesozoic-Cenozoic.

流行的遗迹相和遗迹阶层模式的不足是:前者在操作上,简单地将遗迹化石及其组合处理为同沉积或准同沉积的物理沉积构造,忽略了造迹活动的多阶段和多阶层的特点;后者的资料基础仅依据中生代以来的地层记录,对重大生物-环境事件和造迹生物生态习性演化对遗迹阶层形成和分布的影响注重不够。

Using many geoscientific methods, the formation mechanism and u ranium mmeralization of the Mesozoic-Cenozoic fossil hydrothermal sys tems, Southeast China, have been discussed for the first time through comprehensive studies of the two typical Mesozoic-Cenozoic uranium ore forming fossil hydrothermal systems—Xiangshan Volcanic Rock Type U ranium Ore-field and Xiazhuang Granite Type Urani um Ore-field by integration of "Three sources: Uranium and its Mineralizer Source, Water Source and Heat Source".

本文综合运用多种地质手段,通过解剖华东南地区二个典型的中新生代铀成矿古水热系统,即江西相山火山岩型铀成矿古水热系统和广东下庄花岗岩型铀成矿古水热系统,将&铀源、水源和热源&三者结合起来,首次探讨了华东南地区中新生代古水热系统的形成条件及其铀成矿作用。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究,精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现,把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带;初步确定该区的变质作用属于中温-低压型,变质作用发生的时代为290Ma左右,是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原&居里得能组&岩屑砂岩的碎屑锆石SHRIMP U-Pb定年,确认这套地层的沉积不早于晚泥盆世,很可能是石炭纪,而不是前人所说的前寒武纪;结合对其区域地质背景、源区位置和沉积环境分析,推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料,结合该区已有相关资料的综合研究,确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪,不存在泥盆纪的岩浆岩,进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料,把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%,相应的地壳缩短量分别为4.3km、9km和11.3km。

The authors discuss some major geological issues in Pre-Cambrian and Mesozoic ear in the South -East China in the light of recent geological mapping and re-expound the geological texture of Mesozoic ear in the South-East China.

作者根据近期一系列地质编图所取得的认识,就中国东南部前寒武纪和中生代地质的一些主要问题进行了讨论。

Taking Jiyang Depression as the study object, many kinds of disciplines were applied synthetically in this thesis, such as, stratigraphy, structural geology, sedimentology, historical geology, geophysics, etc. On the basis of the reconstruction of the denuded thickness and the original thickness, and the study of the developing characteristics of the basin-controlled faults, combined with the study of space-time distribution of the sedimentary facies and the analysis of basin - transfer mechanism and the geodynamics, the prototype basins of each structural stage in Mesozoic were studied and analyzed in detail, moreover, the superimposed relationship of the Mesozoic basin and Cenozoic basin was discussed.

本论文选择济阳坳陷作为研究对象,开展地层学、构造地质学、沉积学、地史学以及地球物理学等多学科综合研究,以地层剥蚀厚度、原始厚度的恢复以及控盆断层发育演化特征的研究为切入点,辅以沉积相的时空展布研究,并结合盆地转型机制、地球动力学背景分析,对济阳坳陷中生代各构造期的盆地原型进行详细解剖和分析,探讨其与新生代盆地的叠合关系。

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